Open access peer-reviewed chapter

Solubility Products and Solubility Concepts

By Anna Maria Michałowska-Kaczmarczyk, Aneta Spórna-Kucab and Tadeusz Michałowski

Submitted: October 20th 2016Reviewed: February 10th 2017Published: August 23rd 2017

DOI: 10.5772/67840

Downloaded: 740

Abstract

The chapter refers to a general concept of solubility product Ksp of sparingly soluble hydroxides and different salts and calculation of solubility of some hydroxides, oxides, and different salts in aqueous media. A (criticized) conventional approach, based on stoichiometry of a reaction notation and the solubility product of a precipitate, is compared with the unconventional/correct approach based on charge and concentration balances and a detailed physicochemical knowledge on the system considered, and calculations realized according to generalized approach to electrolytic systems (GATES) principles. An indisputable advantage of the latter approach is proved in simulation of static or dynamic, two-phase nonredox or redox systems.

Keywords

  • electrolytic two-phase systems
  • solubility
  • dissolution
  • static systems
  • dynamic systems
  • computer simulation
  • GATES
  • GEB

1. Introduction

The problem of solubility of various chemical compounds occupies a prominent place in the scientific literature. This stems from the fact that among various properties determining the use of these compounds, the solubility is of the paramount importance. Among others, this issue has been the subject of intense activities initiated in 1979 by the Solubility Data Commission V.8 of the IUPAC Analytical Chemistry Division established and headed by S. Kertes [1], who conceived the IUPAC-NIST Solubility Data Series (SDS) project [2, 3]. Within 1979–2009, the series of 87 volumes, concerning the solubility of gases, liquids, and solids in liquids or solids, were issued [3]; one of the volumes concerns the solubility of various oxides and hydroxides [4]. An extensive compilation of aqueous solubility data provides the Handbook of Aqueous Solubility Data [5].

A remark. Precipitates are marked in bold letters; soluble species/complexes are marked in normal letters.

The distinguishing feature of a chemical compound sparingly soluble in a particular medium is the solubility product Ksp value. In practice, the known Ksp values are referred only to aqueous media. One should note, however, that the expression for the solubility product and then the Ksp value of a precipitate depend on the notation of a reaction in which this precipitate is involved. From this it follows the apparent multiplicity of Ksp’s values referred to a particular precipitate. Moreover, as will be stated below, the expression for Ksp must not necessarily contain ionic species. On the other hand, factual or seeming lack of Ksp’s value for some precipitates is perceived; the latter issue be addressed here to MnO2, taken as an example.

Solubility products refer to a large group of sparingly soluble salts and hydroxides and some oxides, e.g., Ag2O, considered overall as hydroxides. Incidentally, other oxides, such as MnO2, ZrO2, do not belong to this group, in principle. For ZrO2, the solubility measurements showed quite low values even under a strongly acidic condition [6]. The solubility depends on the prior history of these oxides, e.g., prior roasting virtually eliminates the solubility of some oxides. Moderately soluble iodine (I2) dissolves due to reduction or oxidation, or disproportionation in alkaline media [712]; for I2, minimal solubility in water is a reference state. For 8-hydroxyquinoline, the solubility of the neutral molecule HL is a reference state; a growth in solubility is caused here by the formation of ionic species: H2L+1 in acidic and L−1 in alkaline media.

The Ksp is the main but not the only parameter used for calculation of solubility s of a precipitate. The simplifications [13] practiced in this respect are unacceptable and lead to incorrect/false results, as stated in [1418]; more equilibrium constants are also involved with two-phase systems. These objections, formulated in the light of the generalized approach to electrolytic systems (GATES) [8], where s is the “weighed” sum of concentrations of all soluble species formed by the precipitate, are presented also in this chapter, related to nonredox and redox systems.

Calculation of s gives an information of great importance, e.g., from the viewpoint of gravimetry, where the primary step of the analysis is the quantitative transformation of a proper analyte into a sparingly soluble precipitate (salt, hydroxide). Although the precipitation and further analytical operations are usually carried out at temperatures far greater than the room temperature, at which the equilibrium constants were determined, the values of s obtained from the calculations made on the basis of equilibrium data related to room temperature are helpful in the choice of optimal a priori conditions of the analysis, ensuring the minimal, summary concentration of all soluble forms of the analyte, remaining in the solution, in equilibrium with the precipitate obtained after addition of an excess of the precipitating agent; this excess is referred to as relative to the stoichiometric composition of the precipitate. The ability to perform appropriate calculations, based on all available physicochemical knowledge, in accordance with the basic laws of matter conservation, deepens our knowledge of the relevant systems. At the same time, it produces the ability to acquire relevant knowledge in an organized manner—not just imitative, but focused on heuristics. This viewpoint is in accordance with constructivist teaching, based on the belief that learning occurs, as learners are actively involved in a process of meaning and knowledge construction, as opposed to passively receiving information [19].

2. Definitions and formulation of solubility products

The Ksp value refers to a two-phase system where the equilibrium solid phase is a sparingly soluble precipitate, whose Ksp value is measured/calculated according to defined expression for the solubility product. This assumption means that the solution with defined species is saturated against this precipitate, at given temperature and composition of the solution. However, often a precipitate, when introduced into aqueous media, is not the equilibrium solid phase, and then this fundamental requirement is not complied, as indicated in examples of the physicochemical analyses of the systems with struvite MgNH4PO4 [20, 21], dolomite CaMg(CO3)2 [22, 23], and Ag2Cr2O7.

The values of solubility products Ksp (usually represented by solubility constant pKsp = −logKsp value) are known for stoichiometric precipitates of AaBb or AaBbCc type, related to dissociation reactions:

Ksp=[A]a[B]bforAaBb=aA+bB,orE1
Ksp=[A]a[B]b[C]cforAaBbCc=aA+bB+cCE2

where A and B or A, B, and C are the species forming the related precipitate; charges are omitted here, for simplicity of notation. The solubility products for more complex precipitates are unknown in the literature. The precipitates AaBbCc are known as ternary salts [24], e.g., struvite, dolomite, and hydroxyapatite Ca5(PO4)3OH.

The solubility products for precipitates of AaBb type are most frequently met in the literature. In these cases, for A are usually put simple cations of metals, or oxycations [25]; e.g., BiO+1 and UO2+2 form the precipitates: BiOCl and (UO2)2(OH)2. As B, simple or more complex anions are considered, e.g., Cl−1, S−2, PO4−3, Fe(CN)6−4, in AgCl, HgS, Zn3(PO4)2, and Zn2Fe(CN)6.

In different textbooks, the solubility products are usually formulated for dissociation reactions, with ions as products, also for HgS

HgS=Hg+2+S2(Ksp=[Hg+2][S2])E3

although polar covalent bond exists between its constituent atoms [26]. Very low solubility product value (pKsp = 52.4) for HgS makes the dissociation according to the scheme presented by Eq. (3) impossible, and even verbal formulation of the solubility product is unreasonable. Namely, the ionic product x = [Hg+2][S–2] calculated at [Hg+2] = [S–2] = 1/NA exceeds Ksp, 1/NA2 > Ksp (NA – Avogadro’s number); the concentration 1/NA = 1.66∙10–23 mol/L corresponds to 1 ion in 1 L of the solution. The scheme of dissociation into elemental species [14]

HgS=Hg+S (Ksp1=[Hg][S])E4

is far more favored from thermodynamic viewpoint; nonetheless, the solubility product (Ksp) for HgS is commonly formulated on the basis of reaction (3). We obtain pKsp1 = pKsp – 2A(E01E02), where E01 = 0.850 V for Hg+2 + 2e–1 = Hg, E02 = –0.48 V for S + 2e–1 = S–2, 1/A = RT/F⋅ln10, A = 16.92 for 298 K; then pKsp1 = 7.4.

Equilibrium constants are usually formulated for the simplest reaction notations. However, in this respect, Eq. (4) is simpler than Eq. (3). Moreover, we are “accustomed” to apply solubility products with ions (cations and anions) involved, but this custom can easily be overthrown. A similar remark may concern the notation referred to elementary dissociation of mercuric iodide precipitate

HgI2=Hg+I2(Ksp1=[Hg][I2]) E5

where I2 denotes a soluble form of iodine in a system. From

HgI2=Hg+2+2I1(Ksp=[Hg+2][I1]2,pKsp=28.55) E6

we obtain pKsp1 = pKsp – 2A(E01E03), where

E01=0.850Vfor Hg+2+2e1=Hg,E03=0.621V for I2+2e1=2I1;thenpKsp1=20.80.

The species in the expression for solubility products do not predominate in real chemical systems, as a rule. However, the precipitation of HgS from acidified (HCl) solution of mercury salt with H2S solution can be presented in terms of predominating species; we have

HgCl42+H2S=HgS+4Cl1+2H+1E7

Eq. (7) can be applied to formulate the related solubility product, Ksp2, for HgS. To be online with customary requirements put on the solubility product formulation, Eq. (7) should be rewritten into the form

HgS+4Cl1+2H+1=HgCl42+H2SE7a

Applying the law of mass action to Eq. (7a), we have

Ksp2=[HgCl42][H2S][Cl1]4[H+1]2,(pKsp2=17.33)E8

where [HgCl4–2] = 1015.07[Hg+2][Cl–1]4, [H2S] = 1020.0[H+1]2[S–2], Ksp (Eq. (3)).

The solubility product for MgNH4PO4 can be formulated on the basis of reactions:

MgNH4PO4=Mg+2+NH4+1+PO43(Ksp=[Mg+2][NH4+1][PO43])E9
MgNH4PO4=Mg+2+NH3+HPO42(Ksp1=[Mg+2][NH3][HPO42]=KspK1N/K3P)E10
MgNH4PO4+H2O=MgOH+1+NH3+H2PO41(Ksp2=[MgOH+1][NH3][H2PO41]=KspK1OHK1NKW/(K2PK3P)E11

where K1N = [H+1][NH3]/[NH4+1], K2P = [H+1][HPO4–2]/[H2PO4–1], K3P = [H+1][PO4–3]/[HPO4–2], [MgOH+1] = K1OH[Mg+2][OH–1], KW = [H+1][OH–1].

Note that only uncharged (elemental) species are involved in Eqs. (4) and (5); H2S enters Eq. (8), and NH3 enters Eqs. (10) and (11). This is an extension of the definition/formulation commonly met in the literature, where only charged species were involved in expression for the solubility product. Note also that small/dispersed mercury drops are neutralized with powdered sulfur, according to thermodynamically favored reaction [27]

Hg+S=HgSE8422

reverse to Eq. (4). Some precipitates can be optionally considered as the species of AaBb or AaBbCc type. For example, the solubility product for MgHPO4 can be written as Ksp = [Mg+2][HPO4–2] or Ksp1 = [Mg+2][H+1][PO4–3] = KspK3P.

The ferrocyanide ion Fe(CN)6–4 (with evaluated stability constant K6 ca. 1037) can be considered as practically undissociated, i.e., Fe(CN)6–4 is kinetically inert [28], and then it does not give Fe+2 and CN–1 ions. The solubility product of Zn2Fe(CN)6 is Ksp = [Zn+2]2[Fe(CN)6–4]. Therefore, consideration of Zn2Fe(CN)6 as a ternary salt with Ksp1 = [Zn+2]2[Fe2+][CN–1]6 = Ksp/K6 is not acceptable.

In principle, the solubility product values are formulated for stoichiometric compounds, and specified as such in the related tables. However, some precipitates obtained in laboratory have nonstoichiometric composition, e.g., dolomite Ca1+xMg1-x(CO3)2 [22, 23], FexS [29]. In particular, FexS can be rewritten as Fe+2pFe+3qS; from the relations: 2p + 3q − 2 = 0 and p + q = x, we get q/p = 2(1 − x)/(3x − 2).

In this context, some remark needs a formulation of Ksp for some hydroxyoxides (e.g., FeOOH) and oxides (e.g., Ag2O). The related solubility products are formulated after completion of the corresponding reactions with water, e.g., FeOOH + H2O = Fe(OH)3, Fe2O3∙xH2O + (3 − x)H2O = 2Fe(OH)3Fe(OH)3 = Fe+3 + 3OH–1Ksp = [Fe+3][OH–1]3; Ag2O + H2O = 2AgOHAgOH = Ag+1 + OH–1Ksp = [Ag+1][OH–1], see it in the context with gcd(a,b) = 1.

The solubility product can be involved not only with dissociation reaction. For example, the dissolution reaction Ca(OH)2 + 2H+1 = Ca+2 + 2H2O [30], characterized by Ksp1 = [Ca+2]/[H+1]2, is involved with Ksp = [Ca+2][OH–1]2 in the relation Ksp1 = Ksp/Kw2. In Ref. [31], the solubility product is associated with formation (not dissociation) of a precipitate.

3. Solubility product(s) for MnO2

The scheme presented above cannot be extended to all oxides. For example, one cannot recommend the formulation of this sequence for MnO2, i.e., MnO2 + 2H2O = Mn(OH)4Mn(OH)4 = Mn+4 + 4OH–1Ksp0 = [Mn+4][OH–1]4; Mn+4 ions do not exist in aqueous media, and MnO2 is the sole Mn(+4) species present in such systems. In effect, Ksp0 for MnO2 is not known in the literature, compare with Ref. [32]. However, the Ksp for MnO2 can be formally calculated according to an unconventional approach, based on the disproportionation reaction

5MnO2+4H+1=2MnO41+3Mn+2+H2OE12

reverse to the symproportionation reaction 2MnO4−1 + 3Mn+2 + H2O = 5MnO2 + 4H+1. The Ksp = Ksp1 value can be found there on the basis of E01 and E02 values [33], specified for reactions:

MnO41+4H+1+3e1=MnO2+2H2O(E01=1.692V)E13
MnO2+4H+1+2e1=Mn+2+2H2O(E02=1.228V)E14

Eqs. (13) and (14) are characterized by the equilibrium constants:

Ke1=[MnO2][H2O]2[MnO41][H+1]4[e1]3,Ke2=[Mn+2][H2O]2[MnO2][H+1]4[e1]2E15

defined on the basis of mass action law (MAL) [14], where logKe1 = 3⋅AE01, logKe2 = 2⋅AE02, A = 16.92. From Eqs. (13) and (14), we get

2MnO2+4H2O+3MnO2+12H+1+6e1=2MnO41+ 8H+1+6e1+3Mn+2+6H2OE16

Assuming [MnO2] = 1 and [H2O] = 1 on the stage of the Ksp1 formulation for reaction (16), equivalent to reaction (12), we have

Ksp1=[MnO41]2[Mn+2]3[H+1]4E17

and then

Ksp1=(Ke2)3(Ke1)2E18
pKsp1=3logKe22logKe1=6A(E01E02)=616.92(1.6921.228)=47.11E19

The solubility products with MnO2 involved can be formulated on the basis of other reactions. For example, addition of

Mn+2=Mn+3+e1E20

to Eq. (14) gives

MnO2+4H+1+2e1+Mn+2=Mn+2+2H2O+Mn+3+e1E21

Multiplication of Eq. (21) by 3, and then addition to Eq. (13a)

MnO2+2H2O=MnO41+4H+1+3e1E8423

(reverse to Eq. (13)) gives the equation

3MnO2+12H+1+6e1+3Mn+2+MnO2+2H2O=3Mn+2+6H2O+3Mn+3+3e1+MnO41+4H+1+3e1E22

and its equivalent form, obtained after simplifications,

4MnO2+8H+1=3Mn+3+MnO41+4H2OE22a

Eq. (22) and then Eq. (22a) is characterized by the solubility product

Ksp2=[MnO41][Mn+3]3[H+1]8=(Ke2)3(Ke3)3(Ke1)1E23

where

Ke3=[Mn+2][Mn+3][e1]E24

for Mn+3 + e−1 = Mn+2 (E03 = 1.509 V) (reverse to Eq. (20)), logKe3 = AE03. Then

pKsp2=3A(E012E02+E03)+37.82E25

Formulation of Kspi for other combinations of redox and/or nonredox reactions is also possible. This way, some derivative solubility products are obtained. The choice between the “output” and derivative solubility product values is a matter of choice. Nevertheless, one can choose the Ksp3 value related to the simplest expression for the solubility product Ksp3 = [Mn+2][MnO4−2] involved with reaction 2MnO2 = Mn+2 + MnO4−2.

As results from calculations, the low Kspi (i = 1,2,3) values obtained from the calculations should be crossed, even in acidified solution with the related manganese species presented in Figure 1. In the real conditions of analysis, at Ca = 1.0 mol/L, the system is homogeneous during the titration, also after crossing the equivalence point, at Φ = Φeq > 0.2; this indicates that the corresponding manganese species form a metastable system [34], unable for the symproportionation reactions.

Figure 1.

The log[Xi] versus Φ relationships for different manganese species Xi, plotted for titration of V0 = 100 mL solution of FeSO4 (C0 = 0.01 mol/L) + H2SO4 (Ca = 1.0 mol/L) with V mL of C = 0.02 mol/L KMnO4; Φ = C·V/(C0·V0). The species Xi are indicated at the corresponding lines.

4. Calculation of solubility

In this section, we compare two options applied to the subject in question. The first/criticized option, met commonly in different textbooks, is based on the stoichiometric considerations, resulting from dissociation of a precipitate, characterized by the solubility product Ksp value, and considered a priori as an equilibrium solid phase in the system in question; the solubility value obtained this way will be denoted by s* [mol/L]. The second option, considered as a correct resolution of the problem, is based on full physicochemical knowledge of the system, not limited only to Ksp value (as in the option 1); the solubility value thus obtained is denoted as s [mol/L]. The second option fulfills all requirements expressed in GATES and involved with basic laws of conservation in the systems considered. Within this option, we check, among others, whether the precipitate is really the equilibrium solid phase. The results (s*, s) obtained according to both options (1 and 2) are compared for the systems of different degree of complexity. The unquestionable advantages of GATES will be stressed this way.

4.1. Formulation of the solubility s*

The solubility s* will be calculated for a pure precipitate of: (1o) AaBb or (2o) AaBbCc type, when introduced into pure water. Assuming [A] = a∙s* and [B] = b∙s*, from Eq. (1), we have

s=(Kspaabb)1/(a+b)E26

and assuming [A] = a∙s*, [B] = b∙s*, [C] = c∙s*, from Eq. (2), we have

s=(Kspaabbcc)1/(a+b+c)E27

As a rule, the formulas (26) and (27) are invalid for different reasons, indicated in this chapter. This invalidity results, among others, from inclusion of the simplest/minor species in Eq. (26) or (27) and omission of hydroxo-complexes + other soluble complexes formed by A, and proto-complexes + other soluble complexes, formed by B. In other words, not only the species entering the expression for the related solubility product are present in the solution considered. Then the concentrations: [A], [B] or [A], [B], and [C] are usually minor species relative to the other species included in the respective balances, considered from the viewpoint of GATES [8].

4.2. Dissolution of hydroxides

We refer first to the simplest two-phase systems, with insoluble hydroxides as the solid phases. In all instances, s* denotes the solubility obtained from stoichiometric considerations, whereas s relates to the solubility calculated on the basis of full/attainable physicochemical knowledge related to the system in question where, except the solubility product (Ksp), other physicochemical data are also involved.

Applying formula (26) to hydroxides (B = OH1): Ca(OH)2 (pKsp1 = 5.03) and Fe(OH)3 (pKsp2 = 38.6), we have [35]

Ca(OH)2=Ca+2+2OH1(Ksp1=[Ca+2][OH1]2,s*=(Ksp1/4)1/3=0.0133mol/L)E28
Fe(OH)3=Fe+3+3OH1(Ksp2=[Fe+3][OH1]3,s*=(Ksp2/27)1/4=0.98×1010mol/L)E29

respectively. However, Ca+2 and Fe+3 form the related hydroxo-complexes: [CaOH+1] = 101.3·[Ca+2][OH−1] and: [FeOH+2] = 1011.0·[Fe+3][OH−1], [Fe(OH)2+1] = 1021.7·[Fe+3][OH−1]2; [Fe2(OH)2+4] = 1025.1·[Fe+3]2[OH−1]2 [31]. The corrected expression for the solubility of Ca(OH)2 is as follows

s=[Ca+2]+[CaOH+1]E30

Inserting [Ca+2] = Ksp1/[OH−1]2 and [OH−1] = KW/[H+1], [H+1] = 10−pH (pKW = 14.0 for ionic product of water, KW) into the charge balance

2[Ca+2]+[CaOH+1]+[H+1][OH1]=0E31

we get, by turns,

2105.03/[OH1]2+101.3105.03/[OH1][H+1][OH1]=02105.03+282pH+101.3105.03+14pH+10pH10pH14=0E9000
y(pH)=21022.972pH+1010,17pH+10pH10pH14=0E32

where pH=log[H+1]. Applying the zeroing procedure to Eq. (30), we get pH0 = 12.453 (Table 1), where: [Ca+2] = 0.0116, [CaOH+1] = 0.00656, s = 0.0182 mol/L (Eq. (28)). As we see, [CaOH+1] is comparable with [Ca+2], and there are none reasons to omit [CaOH+1] in Eq. (28).

pHy(pH)[OH−1][Ca+2][CaOH+1]
12.4510.0003770.028250.011690.006592
12.4520.0001930.028310.011640.006577
12.4538.30E-060.028380.011590.006561
12.454−0.0001760.028440.011530.006546
12.455−0.0003590.028510.011480.006531

Table 1.

Zeroing the function (30) for the system with Ca(OH)2 precipitate introduced into pure water (copy of a fragment of display).

The alkaline reaction in the system with Ca(OH)2 results immediately from Eq. (29): [OH−1] – [H+1] = 2[Ca+2]+[CaOH+1]>0.

Analogously, for the system with Fe(OH)3, we have the charge balance

3[Fe+3]+2[FeOH+2]+[Fe(OH)2+1]+4[Fe2(OH)2+4]+[H+1][OH1]=0E33

and then

y(pH)=3103.43pH+2100.42pH+102.9pH+4103.94pH+10pH10pH14=0E34

Eq. (32) zeroes at pH0 = 7.0003 (Table 2), where the value

pHy(pH)[Fe+3][FeOH+2][Fe(OH)2+1][Fe2(OH)2+4]
7.00017.99E-112.510E-182.511E-141.259E-107.936E-25
7.00023.38E-112.508E-182.510E-141.258E-107.929E-25
7.0003−1.23E-112.507E-182.508E-141.258E-107.921E-25
7.0004−5.84E-112.505E-182.507E-141.258E-107.914E-25
7.0005−1.04E-102.503E-182.506E-141.257E-107.907E-25

Table 2.

Zeroing the function (32) for the system with Fe(OH)3 precipitate introduced into pure water (copy of a fragment of display).

s=[Fe+3]+[FeOH+2]+[Fe(OH)2+1]+2[Fe2(OH)2+4]E35

is close to s ≅ [Fe(OH)2+1] = 10–9.9. Alkaline reaction for this system, i.e., [OH−1] > [H+1], results immediately from Eq. (30), and pH0 = 7.0003 (>7).

At pH = 7, Fe(OH)2+1 (not Fe+3) is the predominating species in the system, [Fe(OH)2+1]/[Fe+3] = 1021.7–14 = 5·107, i.e., the equality/assumption s* = [Fe+3] is extremely invalid. Moreover, the value [OH−1] = 3·s* = 2.94·10–10 = 10–9.532, i.e., pH = 4.468; this pH-value is contradictory with the inequality [OH−1] > [H+1] resulting from Eq. (31). Similarly, extremely invalid result was obtained in Ref. [36], where the strong hydroxo-complexes were totally omitted, and weak chloride complexes of Fe+3 ions were included into considerations.

Taking only the main dissociating species formed in the solution saturated with respect to Fe(OH)3, we check whether the reaction Fe(OH)3 = Fe(OH)2+1 + OH−1 with Ksp1 = [Fe(OH)2+1][OH−1] = 1021.7·10–38.6 = 10–16.9 can be used for calculation of solubility s'=(Ksp1)1/2for Fe(OH)3; the answer is also negative. Simply, the main part of OH−1 ions originates here from dissociation of water, where the precipitate has been introduced, and then Fe(OH)2+1 and OH−1 differ significantly. As we see, the diversity in Ksp value related to a precipitate depends on its dissociation reaction notation, which disqualifies the calculation of s* based solely on the Ksp value. This fact was not stressed in the literature issued hitherto.

Concluding, the application of the option 1, based on the stoichiometry of the reaction (29), leads not only to completely inadmissible results for s+, but also to a conflict with one of the fundamental rules of conservation obligatory in electrolytic systems, namely the law of charge conservation.

Similarly, critical/disqualifying remarks can be related to the series of formulas considered in the chapter [37], e.g., Ksp = 27(s*)4 for precipitates of A3B and AB3 type, and Ksp = 108(s*)5 for A2B3 and A3B2. For Ca5(PO4)3OH, the formula Ksp = 84375(s*)9 (!) was applied [38].

As a third example let us take a system, where an excess of Zn(OH)2 precipitate is introduced into pure water. It is usually stated that Zn(OH)2 dissociates according to the reaction

Zn(OH)2=Zn+2+2OH1E36

applied to formulate the expression for the solubility product

Ksp3=[Zn+2][OH1]2(pKsp3=15.0)E37

The soluble hydroxo-complexes Zn(OH)i+2−i (i=1,…,4), with the stability constants, KiOH, expressed by the values logKiOH = 4.4, 11.3, 13.14, 14.66, are also formed in the system in question. The charge balance (ChB) has the form

2[Zn+2]+[ZnOH+1][Zn(OH)31]2[Zn(OH)42]+[H+1][OH1]=0E38

i.e., 2·10−15/[OH−1]2 + 104.4·10−15/[OH−1] – 1013.14·10−15∙[OH−1] – 2·1014.66·10−15∙[OH−1]2 = 0

y(pH)=210132pH+103.4pH1015.86+pH21028.34+2pH+10pH10pH14=0E39

The function (39) zeroes at pH0 = 9.121 (see Table 3). The basic reaction of this system is not immediately stated from Eq. (38) (there are positive and negative terms in expression for [OH−1] − [H+1]). The solubility s value

pH[OH−1][Zn+2][ZnOH+1][Zn(OH)2][Zn(OH)3−1][Zn(OH)4−2]y(pH)s [mol/L]
9.1181.3122E-055.8076E-061.9143E-060.00021.8113E-077.8705E-112.2702E-070.00020743
9.1191.3152E-055.7810E-061.9099E-060.00021.8155E-077.9068E-111.3858E-070.00020740
9.1201.3183E-055.7544E-061.9055E-060.00021.8197E-077.9433E-115.0322E-080.00020737
9.1211.3213E-055.7280E-061.9011E-060.00021.8239E-077.9800E-11−3.7750E-080.00020734
9.1221.3243E-055.7016E-061.8967E-060.00021.8281E-078.0168E-11−1.2564E-070.00020731
9.1231.3274E-055.6755E-061.8923E-060.00021.8323E-078.0538E-11−2.1335E-070.00020728

Table 3.

Zeroing the function (39) for the system with Zn(OH)2 precipitate introduced into water; pKW = 14.

s=[Zn+2]+[ZnOH+1]+[Zn(OH)2]+[Zn(OH)31]+[Zn(OH)42]=2.07·104E8433

calculated at this point is different from s* = (Kso3/4)1/3 = 6.3⋅10−6, and [OH−1]/[Zn+2] ≠ 2; such incompatibilities contradict application of this formula.

4.3. Dissolution of MeL2-type salts

Let us refer now to dissolution of precipitates MeL2 formed by cations Me+2 and anions L−1 of a strong acid HL, as presented in Table 4. When an excess of MeL2 is introduced into pure water, the concentration balances and charge balance in two-phase system thus formed are as follows:

Me+2MeOH+1Me(OH)2Me(OH)3−1L−1MeL+1MeL2MeL3−1MeL4−2MeL2
logK1OHlogK2OHlogK3OHlogK1logK2logK3logK4pKsp
Hg+210.321.721.2I−112.8723.8227.6029.8328.54
Pb+26.910.813.3I−11.262.803.423.928.98
Cl−11.622.442.041.04.79

Table 4.

logKiOH and logKi values for the stability constants Ki and Kj of soluble complexes Me(OH)i+2-i and MeLj+2-j and pKsp values for the precipitates MeL2; [MeLi+2-i] = Ki[Me+2][L1]i, Ksp = [Me+2][L1]2.

[MeL2]+[Me+2]+i=1I[Me(OH)i+2i]+j=1J[MeLj+2j]=CMeE40
2[MeL2]+[L1]+j=1Jj[MeLj+2j]=CLE41
[H+1][OH1]+2[Me+2]+i=1I(2i)[Me(OH)i+2i]+j=1J(2j)[MeLj+2j][L1]=0E42

where [MeL2] denotes the concentration of the precipitate MeL2. At CL = 2CMe, we have

2[Me+2]+2i=1I[Me(OH)i+2i]+j=1J(2j)[MeLj+2j]=[L1]E43

From Eqs. (40) and (41)

α=[H+1][OH1]=i=1Ii[Me(OH)i+2i]E44

i.e., reaction of the solution is acidic, [H+1] > [OH−1]. Applying the relations for the equilibrium constants:

[Me+2][L−1]2 = Ksp, [Me(OH)i+2−i] = KiOH[Me+2][OH−1]i (i = 1,…, I), [MeLj+2−j] = Kj[Me+2][L−1]j (j = 1,…, J)

from Eqs. (43) and (44) we have

2[Me+2]3/2(1+(1+i=1Ixi)+Ksp1/2[Me+2]j=1J(2j)Kj[L1]Ksp1/2=0E45

where

[Me+2]=αi=1Iixi;α=[H+1][OH-1]=10pH10pHpKW;[L1]=(Ksp[Me+2])1/2;xi=KiOH(KW/[H+1])iE8000

In particular, for I = 3, J = 4 (Table 4), we have

2(1+i=13xi)[Me]2Ksp1/2+K1[Me]3/2(K3Ksp+1)[Me]1/22K4Ksp3/2=0E46

Applying the zeroing procedure to Eq. (46) gives the pH = pH0 of the solution at equilibrium. At this pH0 value, we calculate the concentrations of all species and solubility of this precipitate recalculated on sMe and sL. When zeroing Eq. (46), we calculate pH = pH0 of the solution in equilibrium with the related precipitate. The solubilities are as follows:

s=sMe=[Me+2]+i=1I[Me(OH)i+2i]+j=1J[MeLj+2j]E47
s=sL=[L1]+j=14j[MeLj+2j]E48

The calculations of sMe and sL for the precipitates specified in Table 4 can be realized with use of Excel spreadsheet, according to zeroing procedure, as suggested above (Table 1).

pH[Pb+2][PbOH+1][Pb(OH)2][Pb(OH)3-1][PbCl+1][PbCl2][PbCl3−1][PbCl4−2][Cl−1]y
4.53430.0107496062.92208E-057.94315E-118.59592E-180.0174058920.0044668366.90723E-052.44685E-070.0388421910.000138249
4.53440.0107446572.92141E-057.94315E-118.5979E-180.0174018840.0044668366.90882E-052.44798E-070.0388511367.7139E-05
4.53450.010739712.92074E-057.94315E-118.59988E-180.0173978780.0044668366.91041E-052.44911E-070.0388600831.60945E-05
4.53460.0107347652.92007E-057.94315E-118.60186E-180.0173938720.0044668366.912E-052.45023E-070.038869032-4.48848E-05
4.53470.0107298232.91939E-057.94315E-118.60384E-180.0173898670.0044668366.91359E-052.45136E-070.038877983-0.000105799

Table 5.

Fragment of display for PbCl2.

For PbI2: pH0 = 5.1502, sPb = 6.5276∙10−4, sI = 1.3051∙10−3, see Table 6. The difference between sI and 2sPb = 1.3055∙10−3 results from rounding the pH0-value.

pH[Pb+2][PbOH+1][Pb(OH)2][Pb(OH)3−1][PbI+1][PbI2][PbI3−1][PbI4−2][I−1]y
5.150.0006308177.07789E-067.94152E-113.54735E-171.47894E-056.60693E-073.54853E-091.44576E-110.0012883930.000138249
5.15010.0006305277.07626E-067.94152E-113.54816E-171.4786E-056.60693E-073.54935E-091.44643E-110.0012886897.7139E-05
5.15020.0006302367.07463E-067.94152E-113.54898E-171.47826E-056.60693E-073.55016E-091.44709E-110.0012889861.60945E-05
5.15030.0006299467.073E-067.94152E-113.5498E-171.47792E-056.60693E-073.55098E-091.44776E-110.001289283-4.48848E-05
5.15040.0006296567.07137E-067.94152E-113.55061E-171.47758E-056.60693E-073.5518E-091.44843E-110.00128958-0.000105799

Table 6.

Fragment of display for PbI2.

For HgI2: pH0 = 6.7769, sHg = 1.91217∙10−5, sI = 3.82435∙10−5, see Table 7. The difference between sI and 2sHg = 3.82434∙10−5 results from rounding the pH-value. The concentration [HgI2] = K2Ksp = 1.90546∙10−5 is close to the sHg value. For comparison, 4(s*)3 = Ksp ⟹ s* = 1.93∙10−10, i.e., s*/s ≈ 10−5.

pH[Hg+2][HgOH+1][Hg(OH)2][Hg(OH)3−1][HgI+1][HgI2][HgI3−1][HgI4−2][I−1]y
6.77672.99681E-153.57569E-125.37106E-081.01569E-152.17936E-091.90546E-051.12634E-081.87646E-139.81003E-081.35932E-10
6.77682.99398E-153.57313E-125.36844E-081.01543E-152.17833E-091.90546E-051.12688E-081.87824E-139.81467E-087.72021E-11
6.77692.99114E-153.57056E-125.36583E-081.01517E-152.1773E-091.90546E-051.12741E-081.88002E-139.81932E-081.8567E-11
6.7772.98831E-153.568E-125.36322E-081.0149E-152.17627E-091.90546E-051.12794E-081.88181E-139.82398E-08-3.99731E-11
6.77712.98548E-153.56544E-125.3606E-081.01464E-152.17524E-091.90546E-051.12848E-081.88359E-139.82863E-08-9.84182E-11

Table 7.

Fragment of display for HgI2.

4.4. Dissolution of CaCO3 in the presence of CO2

The portions 0.1 g of calcite CaCO3 (M = 100.0869 g/mol, d = 2.711 g/cm3) are inserted into 100 mL of: pure water (task A) or aqueous solutions of CO2 specified in the tasks: B1, B2, B3, and equilibrated. Denoting the starting (t = 0) concentrations [mol/L]: Co for CaCO3 and CCO2for CO2 in the related systems, on the basis of equilibrium data collected in Table 8:

  1. (A) we calculate pH = pH01 and solubility s = s(pH01) of CaCO3 at equilibrium in the system;

  2. (B1) we calculate pH = pH02 and solubility s = s(pH02) of CaCO3 in the system, where CCO2refers to saturated (at 25 oC) solution of CO2, where 1.45 g CO2 dissolves in 1 L of water [39].

  3. (B2) we calculate minimal CCO2in the starting solution needed for complete dissolution of CaCO3 in the system and the related pH = pH03 value, where s = s(pH03) = Co;

  4. (B3) we plot the logsCa versus V, pH versus V and logsCa versus pH relationships for the system obtained after addition of V mL of a strong base MOH (Cb = 0.1) into V0 = 100 mL of the system with CaCO3 presented in (B1). The quasistatic course of the titration is assumed.

No.ReactionExpression for the equilibrium constantEquilibrium data
1CaCO3 = Ca+2 + CO3−2[Ca+2][CO3−2] = KsppKsp = 8.48
2Ca+2 + OH−1 = CaOH+1[CaOH+1] = K10[Ca+2][OH−1]logK10 = 1.3
3H2CO3 = H+1 + HCO3−1[H+1][HCO3−1] = K1[H2CO3]pK1 = 6.38
4HCO3−1 = H+1 + CO3−2[H+1][CO3−2] = K2[HCO3-1]pK2 = 10.33
5Ca+2 + HCO3−1 = CaHCO3+1[CaHCO3+1] = K11[Ca+2][HCO3−1]logK11 = 1.11
6Ca+2 + CO3−2 = CaCO3[CaCO3] = K12[Ca+2][CO3−2]logK12 = 3.22
7Ca(OH)2 = Ca+2 + 2OH−1[Ca+2][OH−1]2 = Ksp1pKsp1 = 5.03
8H2O = H+1 + OH−1[H+1][OH−1] = KWpKW = 14.0

Table 8.

Equilibrium data.

The volume 0.1/2.711 = 0.037 cm3 of introduced CaCO3 is negligible when compared with V0 at the start (t = 0) of the dissolution. Starting concentration of CaCO3 in the systems: A, B1, B2, B3 is Co = (0.1/100)/0.1 = 10−2 mol/L. At t > 0, concentration of CaCO3 is co mol/L. The balances are as follows:

Co=co+[Ca+2]+[CaOH+1]+[CaHCO3+1]+[CaCO3](for A,B1,B2,B3)E49
Co=co+[CaHCO3+1]+[CaCO3]+[H2CO3]+[HCO31]+CO32] (for A)E50
Co+CCO2=co+[CaHCO3+1]+[CaCO3]+[H2CO3]+[HCO31]+[CO32](forB1,B2,B3)E51
[H+1][OH1]+2[Ca+2]+[CaOH+1]+[CaHCO3+1][HCO31]2[CO32]=0(for A,B1,B2)E52
[H+1][OH1]+[M+1]+2[Ca+2]+[CaOH+1]+[CaHCO3+1][HCO31]2[CO32]=0(for B3)E52a

where [M+1] = CbV/(V0+V).

  • For (A)

    From Eqs. (49) and (50), we have

    [Ca+2]+[CaOH+1]=[H2CO3]+[HCO31]+[CO32]E53

    Considering the solution saturated with respect to CaCO3 and denoting: f1 = 1016.71−2pH + 1010.33−pH + 1, f2 = 1 + 10pH−12.7, from Eq. (53) and Table 1, we have the relations:

    [Ca+2]f2=[CO32]f1[Ca+2]=104.24(f1/f2)0.5; [CO32]=104.24(f2/f1)0.5;[CaOH+1]=10pH16.94(f1/f2)0.5;[CaCO3]=105.26;[CaHCO3+1]=102.96pH; [HCO31]=106.09pH(f2/f1)0.5; [H+1]=10pH;[OH1]=10pH14.E8300

    Inserting them into the charge balance (52), rewritten into the form

    z=z(pH)=10pH10pH14+2104.24(f1/f2)0.5+10pH16.94(f1/f2)0.5+102.96pH106.09pH(f2/f1)0.52104.24(f2/f1)0.5E54

    and applying the zeroing procedure to the function (54), we find pH01 = 9.904, at z = z(pH01) = 0. The solubility s = s(pH) of CaCO3, resulting from Eq. (49), is

    s=[Ca+2]+[CaOH+1]+[CaHCO3+1]+[CaCO3]E55
    =104.24(f1/f2)0.5+10pH16.94(f1/f2)0.5+102.96pH+105.26E55a

    We have s = s(pH = pH01) = 1.159⋅10−4 mol/L.

  • For (B1)

    Subtraction of Eq. (49) from Eq. (51) gives

    [H2CO3]+[HCO31]+[CO32]([Ca+2]+[CaOH+1])=CCO2[CO32]f1[Ca+2]f2CCO2=0[Ca+2]2f2+ CCO2[Ca+2]Kspf1=0E8400

    In this case,

    [Ca+2]=(CCO2)2+4Kspf1f2CCO22f2E56

    where CCO2= 1.45/44 = 0.0329 mol/L. Eq. (55) has the form

    s=[Ca+2]f2+102.96pH+105.26E57

    and the charge balance is transformed into the zeroing function

    z=z(pH)=10pH10pH14+[Ca+2](2+10pH12.7)+102.96pH[CO32](1010.33pH+2)E58

    where [CO3−2] = 10-8.48/[Ca+2], and [Ca+2] is given by Eq. (56). Eq. (58) zeroes at pH = pH02 = 6.031. Then from Eq. (57) we calculate s = s(pH02) = 6.393∙10−3 mol/L, at pH = pH02 = 6.031.

  • For (B2)

    At pH = pH03, where co = 0, i.e., s = Co, the solution (a monophase system) is saturated toward CaCO3, i.e., the relation [Ca+2][CO3−2] = Ksp is still valid. Applying Eqs. (56) and (57), we find pH values zeroing Eq. (58) at different, preassumed CCO2values. Applying these pH-values in Eq. (57), we calculate the related s = s(pH, CCO2) values (Eq. (57), Table 9). Graphically, CCO2= 0.100 is found at pH03 = 5.683, as the abscissa of the point of intersection of the lines: s = s(pH) and s = Co = 0.01. Table 9 shows other, preassumed s = Co values.

  • For (B3)

    We apply again the formulas used in (B1) and (B2), and the charge balance (Eq. (52a)), which is transformed there into the function

    z=z(pH,V)=10pH10pH14+CbV/(V0+V)+[Ca+2](2+10pH12.7)+102.96pH[CO32](1010.33pH+2)E59

    applied for zeroing purposes, at different V values. The data thus obtained are presented graphically in Figures 2a–c. The data presented in the dynamic solubility diagram (Figure 2b), illustrating the solubility changes affected by pH changes (Figure 2a) resulting from addition of a base, MOH; Figure 2c shows a synthesis of these changes. Solubility product of Ca(OH)2 is not crossed in this system.

CCO20.0900.0910.0920.0930.0940.0950.0960.0970.0980.0990.1000.1010.102
pH5.7165.7125.7095.7065.7025.6995.6965.6935.6905.6875.6835.6805.577
s9.58E-39.64E-39.67E-39.70E-39.77E-39.80E-39.84E-39.87E-39.91E-39.94E-310.01E-310.06E-310.10E-3

Table 9.

The set of points used for searching the CCO2value at s = Co = 0.01; at this point, we have pH03 = 5.683.

Figure 2.

Graphical presentation of the data considered in (b3): (a) pH versus V, (b) log sCa versus V, (c) log sCa versus pH relationships.

5. Nonequilibrium solid phases in aqueous media

Some solids when introduced into aqueous media (e.g., pure water) may appear to be nonequilibrium phases in these media.

5.1. Silver dichromate (Ag2Cr2O7)

The equilibrium data related to the system, where Ag2Cr2O7 is introduced into pure water, were taken from Refs. [33, 40, 41], and presented in Table 10. A large discrepancy between pKsp2 values (6.7 and 10) in the cited literature is taken here into account. We prove that Ag2Cr2O7 changes into Ag2CrO4.

ReactionEquilibrium data
H2O = H+1 + OH-1pKw = 14.0
H2CrO4=H++HCrO41pK1 = 0.8
HCrO41= H++CrO42pK2 = 6.5
HCr2O71=H+1+Cr2O72logK3 = 0.07
2HCrO41=Cr2O72+H2OlogK4 = 1.52
Ag+1 + OH−1 = AgOHlogK1OH = 2.3
Ag+1+2OH1=Ag(OH)21logK2OH = 3.6
Ag+1+3OH1=Ag(OH)32logK3OH = 4.8
Ag2CrO4=2Ag+1+CrO42pKsp1 = 11.9
Ag2Cr2O7=2Ag+1+Cr2O72pKsp2 = 6.7
AgOH=Ag+1+OH1pKsp3 = 7.84

Table 10.

Physicochemical equilibrium data relevant to the Ag2Cr2O7 + H2O system (pK = −logK), at “room” temperatures.

On the dissociation step, each dissolving molecule of Ag2Cr2O7 gives two ions Ag+1 and 1 ion Cr2O7−2, where two atoms of Cr are involved; in the contact with water, these ions are hydrolyzed, to varying degrees. In the initial step of the dissolution, before the saturation of the solution with respect to an equilibrium solid phase (not specified at this moment), we can write the concentration balances

2[Ag2Cr2O7]+[Ag+1]+[AgOH]+[Ag(OH)21]+[Ag(OH)32]=2C0E60
2[Ag2Cr2O7]+[H2CrO4]+[HCrO41]+[CrO42]+2[HCr2O71]+2[Cr2O72]=2C0E61

where 2C0 is the total concentration of the solid phase in the system, at the moment (t = 0) of introducing this phase into water, [Ag2Cr2O7] is the concentration of this phase at a given moment of the intermediary step. As previously, we assume that addition of the solid phase (here: Ag2Cr2O7) does not change the volume of the system in a significant degree, and that Ag2Cr2O7 is added in a due excess, securing the formation of a solid (that is not specified at this moment), as an equilibrium solid phase. The balances in Eqs. (60) and (61) are completed by the charge balance

[H+1][OH1]+[Ag+1][Ag(OH)21]2[Ag(OH)32][HCrO41]2[CrO42][HCr2O71]2[Cr2O72]=0E62

used, as previously, to formulation of the zeroing function, y = y(pH), and the set of relations for equilibrium data specified in Table 10. From these relations, we get

[H2CrO4]=107.32pH[CrO42];[HCrO41]=106.5pH[CrO42];[HCr2O71]=1014.593pH[CrO42]2;E63
[Cr2O72]=1014.522pH[CrO42]2E63a

Denoting by 2c0 (< 2C0) the total concentration of dissolved Ag and Cr species formed, in a transition stage, from Ag2Cr2O7, we can write

[Ag+1]+[AgOH]+[Ag(OH)21]+[Ag(OH)32]=2c0E64
[H2CrO4]+[HCrO41]+[CrO42]+2[HCr2O71]+2[Cr2O72]=2c0E65

From Table 10 and formulas (63)–(65) we get the relations:

(a)[Ag+1]=2c0/g0; 2g2[CrO42]2+g1[CrO41]2c0=0(b)[CrO42]=(g12+16c0g2)0.5g14g2E66

where g0 = 1 + 10pH−11.7 + 102pH−24.4 + 103pH−37.2; g1 = 107.3−2pH + 106.5−pH + 1; g2 = 1014.59−3pH + 1014.52−2pH. Applying them in Eq. (62), we get the zeroing function

y=y(pH)=10pH10pH14+g3[Ag+1] g4[CrO42]g5[CrO42]2E67

where g3 = 1 – 102pH−24.4 – 2∙103pH−37.2; g4 = 106.5−pH + 2; g5 = 1014.59−3pH + 2∙1014.52−2pH, and [Ag+1] and [CrO4−2] are defied above, as functions of pH.

The calculation procedure, realizable with use of Excel spreadsheet, is as follows. We assume a sequence of growing numerical values for 2c0. At particular 2c0 values, we calculate pH = pH(2c0) value zeroing the function (67), and then calculate the values of the products: q1 = [Ag+1]2[CrO4−2]/Ksp1 and q2 = [Ag+1]2[Cr2O7−2]/Ksp2, where: [Ag+1], [CrO4−2], and [Cr2O7−2] are presented above (Eqs. (66a), (66b) and (63a), resp.), pKsp1 = 11.9, pKsp2 = 6.7. As results from Figure 3, where logq1 and logq2 are plotted as functions of 2c0; logq1 = 0 ⇔ q1 = 1 ⇔ [Ag+1]2[CrO4−2] = Ksp1 at lower 2c0 value, whereas logq2 < 0 ⇔ q2 < 1 ⇔ [Ag+1]2[Cr2O7−2] < Ksp2, both for pK2 = 6.7 and 10, cited in the literature. The x1=1 value is attained at 2c0 = 3.5∙10−4 ⟹ c0 = 1.75∙10−4; then Ag2CrO4 precipitates as the new solid phase, i.e., total depletion of Ag2Cr2O7 occurs. It means that Ag2Cr2O7 is not the equilibrium solid phase in this system. This fact was confirmed experimentally, as stated in [42], i.e., Ag2Cr2O7 is transformed into Ag2CrO4 upon boiling with H2O; at higher temperatures, this transformation proceeds more effectively. Concluding, the formula s* = (Ksp2/4)1/3 applied for Ksp2 = [Ag+1]2[Cr2O7−2] is not “the best answer,” as stated in Ref. [43].

Figure 3.

The convergence of logq1 and logq2 to 0 value; Ksp1 is attained at lower 2c0 value.

The system involved with Ag2CrO4 was also considered in context with the Mohr’s method of Cl−1 determination [4446]. As were stated there, the systematic error in Cl−1 determining according to this method, expressed by the difference between the equivalence (eq) volume (Veq = C0V0/C) and the volume Vend corresponding to the end point where the Ksp1 for Ag2CrO4 is crossed, equals to

VeqVend=KspC(C01V0Ksp1)0.5(V0+Vend)0.51C(Ksp1C01V0)0.5(V0+Vend)1.5E8435

where Ksp = [Ag+1][Cl−1] (pKsp = 9.75), V0 is the volume of titrant with NaCl (C0) + K2CrO4 (C01) titrated with AgNO3 (C) solution; Vend = Veq at C01 = (1 + Vend/V0)∙Ksp1/Ksp.

All calculations presented above were realized using Excel spreadsheets. For more complex nonequilibrium two-phase systems, the use of iterative computer programs, e.g., ones offered by MATLAB [8, 47], is required. This way, the quasistatic course of the relevant processes under isothermal conditions can be tested [48].

5.2. Dissolution of struvite

The fact that NH3 evolves from the system obtained after leaving pure struvite pr1 in contact with pure water, e.g., on the stage of washing this precipitate, has already been known at the end of nineteenth century [49]. It was noted that the system obtained after mixing magnesium, ammonium, and phosphate salts at the molar ratio 1:1:1 gives a system containing an excess of ammonium species remaining in the solution and the precipitate that “was not struvite, but was probably composed of magnesium phosphates” [50]. This effect can be explained by the reaction [20]

3MgNH4PO4=Mg3(PO4)2+HPO42+NH3+2NH4+1E68

Such inferences were formulated on the basis of X-ray diffraction analysis, the crystallographic structure of the solid phase thus obtained. It was also stated that the precipitation of struvite requires a significant excess of ammonium species, e.g., Mg:N:P = 1:1.6:1. Struvite (pr1) is the equilibrium solid phase only at a due excess of one or two of the precipitating reagents. This remark is important in context with gravimetric analysis of magnesium as pyrophosphate. Nonetheless, also in recent times, the solubility of struvite is calculated from the approximate formula s* = (Ksp1)1/3 based on an assumption that it is the equilibrium solid phase in such a system.

Struvite is not the equilibrium solid phase also when introduced into aqueous solution of CO2 (CCO2, mol/L), modified (or not) by free strong acid HB (Ca, mol/L) or strong base MOH (Cb, mol/L).

The case of struvite requires more detailed comments. The reaction (68) was proved theoretically [20], on the basis of simulated calculations performed by iterative computer programs, with use of all attainable physicochemical knowledge about the system in question. For this purpose, the fractions

q1=[Mg+2][NH4+1][PO43]/Ksp1,q2=[Mg+2]3[PO43]2/Ksp2,q3=[Mg+2][HPO42]/Ksp3,q4[Mg+2][OH1]2/Ksp4E69

were calculated for: pr1 = MgNH4PO4 (pKsp1 = 12.6), pr2 = Mg3(PO4)2 (pKsp2 = 24.38), pr3 = MgHPO4 (pKsp3 = 5.5), pr4 = Mg(OH)2 (pKsp4 = 10.74) and are presented in Figure 4, at an initial concentration of pr1, equal C0 = [pr1]t=0 = 10−3 mol/L (pC0 = (ppr1)t=0 = 3); ppr1 = −log[pr1]. As we see, the precipitation of pr2 (Eq. (68)) starts at ppr1 = 3.088; other solubility products are not crossed. The changes in concentrations of some species, resulting from dissolution of pr1, are indicated in Figure 5, where s is defined by equation [20]

Figure 4.

Plots of logqi versus ppr1 = −log[pr1] relationships, at (ppr1)t=0 = 3; i = 1,2,3,4 refer to pr1, pr2, pr3 and pr4, respectively.

Figure 5.

The speciation curves for indicated species resulting from dissolution of pr1 at (ppr1)t=0 = 3.

s=sMg=[Mg+2]+[MgOH+1]+[MgH2PO4+1]+[MgHPO4]+[MgPO41]+[MgNH3+2]+[Mg(NH3)2+2]+[Mg(NH3)3+2]E70

involving all soluble magnesium species are identical in its form, irrespective of the equilibrium solid phase(s) present in this system. Moreover, it is stated that pH in the solution equals ca. 9–9.5 (Figure 6); this pH can be affected by the presence of CO2 from air. Under such conditions, NH4+1 and NH3 occur there at comparable concentrations [NH4+1] ≈ [NH3], but [HPO4−2]/[PO4−3] = 1012.36−pH ≈ 103. This way, the scheme (10) would be more advantageous, provided that struvite is the equilibrium solid phase; but it is not the case, see Eq. (68). The reaction (68) occurs also in the presence of CO2 in water where struvite was introduced.

Figure 6.

The pH versus log[pr2] relationship; pr2 = Mg3(PO4)2, at [ppr1]t=0 = 3. The numbers at the corresponding lines indicate pCO2=−logCCO2 values; pCO2=∞ ⇔ CCO2= 0.

After introducing struvite pr1 (at pC0 = [ppr1]t=0 = 2) into alkaline (Cb = 10−2 mol/L KOH, pCb = 2) solution of CO2 (pCO2 = 4), the dissolution is more complicated and proceeds in three steps, see Figure 7.

Figure 7.

The speciation curves for indicated species Xizi, resulting from dissolution of pr1 = MgNH4PO4, at (pC0, pCO2, pCb) = (2, 4, 2); s′ is defined by Eq. (71).

In step 1, pr4 precipitates first, pr1 + 2OH−1 = pr4 + NH3 + HPO4−2, nearly from the very start of pr1 dissolution, up to ppr1 = 2.151, where Ksp2 is attained. Within step 2, the solution is saturated toward pr2 and pr4. In this step, the reaction expressed by the notation 2pr1 + pr4 = pr2 + 2NH3 + 2H2O occurs up to total depletion of pr4 (at ppr1 = 2.896). In this step, the reaction 3pr1 + 2OH−1 = pr2 + 3NH3 + HPO4−1 + 2H2O occurs up to total depletion of pr1, i.e., the solubility product Ksp1 for pr1 is not crossed. The curve s′ (Figure 7) is related to the function

s=s+[MgHCO3+1]+[MgCO3]E71

where s is expressed by Eq. (70).

6. Solubility of nickel dimethylglyoximate

The precipitate of nickel dimethylglyoximate, NiL2, has soluble counterpart with the same formula, i.e., NiL2, in aqueous media. If NiL2 is in equilibrium with the solution, concentration of the soluble complex NiL2 assumes constant value: [NiL2] = K2∙[Ni2+][L]2 = K2Ksp, where K2 = 1017.24, Ksp = [Ni2+][L]2 = 10−23.66 [14, 17, 18], and then [NiL2] = 10−6.42 (i.e., log[NiL2] = −6.42). The concentration [NiL2] is the constant, limiting component in expression for solubility s = sNi of nickel dimethylglyoximate, NiL2. Moreover, it is a predominant component in expression for s in alkaline media, see Figure 8. This pH range involves pH of ammonia buffer solutions, where NiL2 is precipitated from NiSO4 solution during the gravimetric analysis of nickel; the expression for solubility

Figure 8.

Solubility curves for nickel dimethylglyoximate NiL2 in (a) ammonia, (b) acetate+ammonia, and (c) citrate+acetate+ ammonia media at total concentrations [mol/L]: CNi = 0.001, CL = 0.003, CN = 0.5, CAc = 0.3, CCit = 0.1 [14].

s=sNi=[Ni+2]+[NiOH+1]+[NiSO4]+i=16[Ni(NH3)i+2]+[NiL2]E72

The effect of other, e.g., citrate (Cit) and acetate (Ac) species as complexing agents can also be considered for calculation purposes, see the lines b and c in Figure 8. The presence of citrate does not affect significantly the solubility of NiL2 in ammonia buffer media, i.e., at pH ≈ 9, where sNi ≅ [NiL2].

Calculations of s = sNi were made at CNi = 0.001 mol/L and CL = 0.003 mol/L HL, i.e., at the excessive HL concentration equal CL – 2CNi = 0.001 mol/L. Solubility of HL in water, equal 0.063 g HL/100 mL H2O (25oC) [51], corresponds to concentration 0.63/116.12 = 0.0054 mol/L of the saturated HL solution, 0.003 < 0.0054. Applying higher CL values needs the HL solution in ethanol, where HL is fairly soluble. However, the aqueous-ethanolic medium is thus formed, where equilibrium constants are unknown. To avoid it, lower CNi and CL values were applied in calculations. The equilibrium data were taken from Ref. [31].

The soluble complex having the formula identical to the formula of the precipitate occurs also in other, two-phase systems. In some pH range, concentration of this soluble form is the dominant component of the expression for the solubility s. As stated above, such a case occurs for NiL2. Then one can assume the approximation

s=K2KspE73

Similar relationship exists also for other precipitates. By differentiation of Eq. (73) with respect to temperature T at p = const, and application of van’t Hoff’s isobar equation for K2 and Ksp, we obtain

1s(sT)p=1RT2(ΔG1o+ΔG2o)E74

where

ΔG1o=RT2(lnKspT)pandΔG2o=RT2(lnK2T)pE8436

Because, as a rule,

(KspT)p>0and(K2T)p<0E8437

then ΔG1o>0and ΔG2o<0, and Eq. (74) can be rewritten into the form

1s(sT)p=1RT2(|ΔG1o||ΔG2o|)E75

If |ΔG1o||ΔG2o|within the temperature range (T0, T), the value of s is approximately constant. Let T0 denote the room temperature (at which,as a rule—all the equilibrium constants are determined) and TT0 is the temperature at which the precipitate is filtered and washed. In this case, the solubility s and then theoretical accuracy of gravimetric analysis does not change with temperature.

7. Calculation of solubility in dynamic redox systems

7.1. Preliminary information

The redox system presented in this section is resolvable according to generalized approach to redox systems (GATES), formulated by Michałowski (1992) [8]. According to GATES principles, the algebraic balancing of any electrolytic system is based on the rules of conservation of particular elements/cores Yg (g = 1,…, G), and on charge balance (ChB), expressing the rule of electroneutrality of this system; the terms element and core are then distinguished. The core is a cluster of elements with defined composition (expressed by its chemical formula) and external charge that remains unchanged during the chemical process considered, e.g., titration. For ordering purposes, we assume: Y1 = H, Y2 = O,…. For modeling purposes, the closed systems, composed of condensed phases separated from its environment by diathermal (freely permeable by heat) walls, are considered; it enables the heat exchange between the system and its environment. Any chemical process, such as titration, is carried out under isothermal conditions, in a quasistatic manner; constant temperature is one of the conditions securing constancy of equilibrium constants values. An exchange of the matter (H2O, CO2, O2,…) between the system and its environment is thus forbidden, for modeling purposes. The elemental/core balance F(Yg) for the g-th element/core (Yg) (g = 1,…, G) is expressed by an equation interrelating the numbers of Yg-atoms or cores in components of the system with the numbers of Yg-atoms/cores in the species of the system thus formed; we have F(H) for Y1 = H, F(O) for Y2 = O, etc.

The key role in redox systems is due to generalized electron balance (GEB) concept, discovered by Michałowski as the Approach I (1992) and Approach II (2006) to GEB; both approaches are equivalent:

Therefore,ApproachIIto GEBApproachItoGEBE76

GEB is fully compatible with charge balance (ChB) and concentration balances F(Yg), formulated for different elements and cores. The primary form of GEB, pr-GEB, obtained according to Approach II to GEB is the linear combination

pr-GEB=2F(O)F(H)E77

Both approaches (I and II) to GEB were widely discussed in the literature [712, 14, 15, 17, 18, 34, 5274], and in three other chapters in textbooks [7579] issued in 2017 within InTech. The GEB is perceived as a law of nature [9, 10, 17, 67, 71, 73, 74], as the hidden connection of physicochemical laws, as a breakthrough in the theory of electrolytic redox systems. The GATES refers to mono- and polyphase, redox, and nonredox, equilibrium and metastable [20, 2123, 78, 79] static and dynamic systems, in aqueous, nonaqueous, and mixed-solvent media [69, 72], and in liquid-liquid extraction systems [53]. Summarizing, Approach II to GEB needs none prior information on oxidation numbers of all elements in components forming a redox system and in the species in the system thus formed. The Approach I to GEB, considered as the “short” version of GEB, is useful if all the oxidation numbers are known beforehand; such a case is obligatory in the system considered below. The terms “oxidant” and “reductant” are not used within both approaches. In redox systems, 2∙F(O) – F(H) is linearly independent on CHB and F(Yg) (g ≥ 3,…, G); in nonredox systems, 2∙F(O) – F(H) is dependent on those balances. This property distinguishes redox and nonredox systems of any degree of complexity. Within GATES, and GATES/GEB in particular, the terms: “stoichiometry,” “oxidation number,” “oxidant,” “reductant,” “equivalent mass” are considered as redundant, old-fashioned terms. The term “mass action law” (MAL) was also replaced by the equilibrium law (EL), fully compatible with the GATES principles. Within GATES, the law of charge conservation and law of conservation of all elements of the system tested have adequate importance/significance.

A detailed consideration of complex electrolytic systems requires a collection and an arrangement of qualitative (particular species) and quantitative data; the latter ones are expressed by interrelations between concentrations of the species. The interrelations consist of material balances and a complete set of expressions for equilibrium constants. Our further considerations will be referred to a titration, as a most common example of dynamic systems. The redox and nonredox systems, of any degree of complexity, can be resolved in analogous manner, without any simplifications done, with the possibility to apply all (prior, preselected) physicochemical knowledge involved in equilibrium constants related to a system in question. This way, one can simulate (imitate) the analytical prescription to any process that may be realized under isothermal conditions, in mono- and two-phase systems, with liquid-liquid extraction systems included.

7.2. Solubility of CuI in a dynamic redox system

The system considered in this section is related to iodometric, indirect analysis of an acidified (H2SO4) solution of CuSO4 [14, 64]. It is a very interesting system, both from analytical and physicochemical viewpoints. Because the standard potential E0 = 0.621 V for (I2, I−1) exceeds E0 = 0.153 V for (Cu+2, Cu+1), one could expect (at a first sight) the oxidation of Cu+1 by I2. However, such a reaction does not occur, due to the formation of sparingly soluble CuI precipitate (pKsp = 11.96).

This method consists of four steps. In the preparatory step (step 1), an excess of H2SO4 is neutralized with NH3 (step 1) until a blue color appears, which is derived from Cu(NH3)i+2 complexes. Then the excess of CH3COOH is added (step 2), to attain a pH ca. 3.6. After subsequent introduction of an excess of KI solution (step 3), the mixture with CuI precipitate and dissolved iodine formed in the reactions: 2Cu+2 + 4I−1 = 2CuI + I2, 2Cu+2 + 5I−1 = 2CuI + I3−1 is titrated with Na2S2O3 solution (step 4), until the reduction of iodine: I2 + 2S2O3−2 = 2I−1 + S4O6−2, I3−1 + 2S2O3−2 = 3I−1 + S4O6−2 is completed; the reactions proceed quantitatively in mildly acidic solutions (acetate buffer), where the thiosulfate species are in a metastable state. In strongly acidic media, thiosulfuric acid disproportionates according to the scheme H2S2O3 = H2SO3 + S [80].

7.3. Formulation of the system

We assume that V mL of C mol/L Na2S2O3 solution is added into the mixture obtained after successive addition of: VN mL of NH3 (C1) (step 1), VAc mL of CH3COOH (C2) (step 2), VKI mL of KI (C3) (step 3), and V mL of Na2S2O3 (C) (step 4) into V0 mL of titrand D composed of CuSO4 (C0) + H2SO4 (C01). To follow the changes occurring in particular steps of this analysis, we assume that the corresponding reagents in particular steps are added according to the titrimetric mode, and the assumption of the volumes additivity is valid.

In this system, three electron-active elements are involved: Cu (atomic number ZCu = 29), I (ZI = 53), S (ZS = 16). Note that sulfur in the core SO4−2 is not involved here in electron-transfer equilibria between S2O3−2 and S4O6−2; then the concentration balance for sulfate species can be considered separately.

The balances written according to Approach I to GEB, in terms of molar concentrations, are as follows:

  • Generalized electron balance (GEB)

    (ZCu2)([Cu+2]+[CuOH+1]+[Cu(OH)2]+[Cu(OH)31]+[Cu(OH)42]+[CuNH3+2]+[Cu(NH3)2+2]+[Cu(NH3)3+2]+[Cu(NH3)4+2]+[CuCH3COO+1]+[Cu(CH3COO)2])+(ZCu2+ZI5)[CuIO3+1]+(ZCu1)([Cu+1]+[CuNH3+1]+[Cu(NH3)2+1])+(ZCu+ZI)[CuI(s)]+(ZCu+2ZI+1)[CuI21]+(ZI+1)[I1]+(3ZI+1)[I31]+2ZI([I2]+a[I2(s)])+(ZI1)([HIO]+[IO1])+(ZI5)([HIO3]+[IO31])+(ZI7)([H5IO6]+[H4IO61]+[H3IO62])+2(ZS2)([H2S2O3]+[HS2O31])+[S2O32])+ 4(ZS2.5)[S4O62]+(ZCu1+2(ZS2))[CuS2O31]+(ZCu1+4(ZS2))[Cu(S2O3)23]+(ZCu1+6(ZS2))[Cu(S2O3)35]((ZCu2)C0V0+(ZI+1)C3VKI+2(ZS2)CV)/(V0+VN+VAc+VKI+V)=0E78

  • CHB

    [H+1][OH1]+[K+1]+[Na+1][HSO41]2[SO42]+[NH4+1][CH3COO1]+2[Cu+2]+[CuOH+1][Cu(OH)31]2[Cu(OH)42]+2[Cu(NH3)+2]+2[Cu(NH3)3+2]+2[Cu(NH3)3+2]+2Cu(NH3)4+2]+[CuCH3COO+1][I1]-[I31][IO1][IO31][H4IO61]2[H3IO62]+[Cu+1]+[CuNH3+1]+[Cu(NH3)2+1][CuI21]+[CuIO3+1][HS2O31]2[S2O32]2[S4O62][CuS2O31]3[Cu(S2O3)23]5[Cu(S2O3)35]=0E79

  • F(Cu)

    [Cu+2]+[CuOH+1]+[Cu(OH)2]+[Cu(OH)31]+[Cu(OH)42]+[CuSO4]+[CuNH3+2] +[Cu(NH3)2+2]+[Cu(NH3)3+2]+[Cu(NH3)4+2]+[CuCH3COO+1]+[Cu(CH3COO)2]+[Cu+1]+[CuNH3+1]+[Cu(NH3)2+1]+ [CuI21]+[CuI(s)]+[CuIO3+1]+[CuS2O31]+[Cu(S2O3)23]+[Cu(S2O3)35]C0V0/(V0+VN+VAc+VKI+V)=0E80

  • F(SO4)

    [HSO41]+[SO42]+[CuSO4]C01V0/(V0+VN+VAc+VKI+V)=0E81

  • F(NH3)

    [NH4+1]+[NH3]+[CuNH3+2]+2[Cu(NH3)2+2]+3[Cu(NH3)3+2]+4[Cu(NH3)4+2]+[CuNH3+1]+2[Cu(NH3)2+1]C1VN/(V0+VN+VAc+VKI+V)=0E82

  • F(CH3COO)

    [CH3COOH]+[CH3COO1]+[CuCH3COO+1]+2[Cu(CH3COO)2]C2VAc/(V0+VN+VAc+VKI+V)=0E83

  • F(K)

    [K+1]=C3VKI/(V0+VN+VAc+VKI+V)E84

  • F(I)

    [I1]+3[I31]+2([I2]+[I2(s)])+[HIO]+[IO1]+[HIO3]+[IO31]+[H5IO6]+[H4IO61]+[H3IO62]+ 2[CuI2−1]+[CuI(s)]+[CuIO3+1]C3VKI/(V0+VN+VAc+VKI+V)=0E85

  • F(S)

    2[H2S2O3]+2[HS2O31]+2[S2O32]+4[S4O62]+2[CuS2O31]+4[Cu(S2O3)23]+6[Cu(S2O3)35]2CV/(V0+VN+VAc+VKI+V)=0[H2S2O3]+[HS2O31]+[S2O32]+2[S4O62] + [CuS2O31] + 2[Cu(S2O3)23]+3[Cu(S2O3)35]CV/(V0+VN+VAc+VKI+V)=0E86

  • F(Na)

    [Na+1]=2CV/(V0+VN+VAc+VKI+V)E87

The GEB is presented here in terms of the Approach I to GEB, based on the “card game” principle, with Cu (Eq. (80)), I (Eq. (85)) as S (Eq. (86)) as “players,” and H, O, S (Eq. (81)), C (from Eq. (83)), N (from Eq. (82)), K, Na as “fans.” There are together 47 species involved in 2 + 6 = 8, Eqs. (78)–(83), (85), (86) and two equalities; [K+1] (Eq. (84)) and [Na+1] (Eq. (87)) are not involved in expressions for equilibrium constants, and then are perceived as numbers (not variables), at a particular V-value. Concentrations of the species in the equations are interrelated in 35 independent equilibrium constants:

[H+1]=10pH,[OH1]=10pH14(pKW=14),[CuOH+1]=107.0[Cu+2][OH−1],[Cu(OH)2]=1013.68[Cu+2][OH1]2,[Cu(OH)31]=1017.0[Cu+2][OH1]3,[Cu(OH)42]=1018.5[Cu+2][OH1]4,[CuNH3+2]=103.39[Cu+2][NH3],[Cu(NH3)2+2]=107.33[Cu+2][NH3]2, [Cu(NH3)32+]=1010.06[Cu+2][NH3]3,[Cu(NH3)4+2]=1012.03[Cu+2][NH3]4,[CuSO4]=102.36[Cu+2][SO42],[NH4+1]=109.35[H+1][NH3],[HSO41]=101.8[H+1][SO42],[CH3COOH]=104.65[H+1][CH3COO1],[Cu+1][I1]=1011.96(solubitlityproductforCuI),[CuI21]=108.85[Cu+1][I1]2,[CuIO3+1]=100.82[Cu+2][IO31],[CuCH3COO+1]=102.24[Cu+2][CH3COO1],[Cu(CH3COO)2]=103.30[Cu+2][CH3COO1]2,[HS2O31]=101.72[H+1][S2O32],[H2S2O3]=102.32[H+1]2[S2O32],[CuS2O31]=103.30[Cu+1][S2O32],[Cu(S2O3)23]=1012.2[Cu+1][S2O32]2,[Cu(S2O3)35]=1013.8[Cu+1][S2O32]3E8420

Applying A = 16.92 [16], we have

[Cu+2]=[Cu+1]10A(E0.153);[I2]=[I1]2102A(E0.621),s=1.33103mol/L(solubilityofI2(s)),[I31]=[I1]3102A(E0.545),[IO1]=[I]102A(E0.49)+2pH28, [HIO]=1010.6[H+1][IO1],[IO31]=[I1]106A(E1.08)+6pH,[HIO3]=100.79[H+1][IO31],[H5IO6]=[I1]108A(E1.24)+7pH,[H4IO61]=[H5IO6]103.3+pH,[H3IO62]=[I1]108A(E0.37)+9pH126.E8438

In the calculations made in this system according to the computer programs attached to Ref. [64], it was assumed that V0 = 100, C0 = 0.01, C01 = 0.01, C1 = 0.25, C2 = 0.75, C3 = 2.0, C4 = C = 0.1; VN = 20, VAc = 40, VK = 20. At each stage, the variable V is considered as a volume of the solution added, consecutively: NH3, CH3COOH, KI, and Na2S2O3, although the true/factual titrant in this method is the Na2S2O3 solution, added in stage 4.

The solubility s [mol/L] of CuI in this system (Figures 8a and b) is put in context with the speciation diagrams presented in Figure 9. This precipitate appears in the initial part of titration with KI (C3) solution (Figure 8a) and further it accompanies the titration, also in stage 4 (Figure 8b). Within stage 3, at V ≥ C0V0/C3, we have

Figure 9.

The speciation plots for indicated Cu-species within the successive stages. The V-values on the abscissas correspond to successive addition of V mL of: 0.25 mol/L NH3 (stage 1); 0.75 mol/L CH3COOH (stage 2); 2.0 mol/L KI (stage 3); and 0.1 mol/L Na2S2O3 (stage 4). For more details see text.

s=s3=[Cu+2]+i=14[Cu(OH)i+2i]+i=14[Cu(NH3)i+2]+[CuSO4]+[CuIO3+1]+i=12[Cu(CH3COO)i+2i]+[Cu+1]+[CuI21]+i=12[Cu(NH3)i+1]E88

and in stage 4

s=s4=s3+i=13[Cu(S2O3)i+12i]E89

The small concentration of Cu+1 (Figure 9, stage 3) occurs at a relatively high total concentration of Cu+2 species, determining the potential ca. 0.53–0.58 V, [Cu+2]/[Cu+1] = 10A(E – 0.153), see Figure 10a. Therefore, the concentration of Cu+2 species determine a relatively high solubility s in the initial part of stage 3. The decrease in the s value in further parts of stage 3 is continued in stage 4, at V < Veq = C0V0/C = 0.01∙100/0.1 = 10 mL. Next, a growth in the solubility s4 at V > Veq is involved with formation of thiosulfate complexes, mainly CuS2O3−1 (Figure 9, stage 4). The species I3−1 and I2 are consumed during the titration in stage 4 (Figure 9d). A sharp drop of E value at Veq = 10 mL (Figure 10b) corresponds to the fraction titrated Φeq = 1.

Figure 10.

Plots of E versus V for (a) stage 3 and (b) stage 4.

The course of the E versus V relationship within the stage 3 is worth mentioning (Figure 10a). The corresponding curve initially decreases and reaches a “sharp” minimum at the point corresponding to crossing the solubility product for CuI. Precipitation of CuI starts after addition of 0.795 mL of 2.0 mol/L KI (Figure 11a). Subsequently, the curve in Figure 10a increases, reaches a maximum and then decreases. At a due excess of the KI (C3) added on the stage 3 (VK = 20 mL), solid iodine (I2(s), of solubility 0.00133 mol/L at 25oC) is not precipitated.

Figure 11.

Solubility s of CuI within stage 3 (a) and stage 4 (b).

8. Final comments

The solubility and dissolution of sparingly soluble salts in aqueous media are among the main educational topics realized within general chemistry and analytical chemistry courses. The principles of solubility calculations were formulated at a time when knowledge of the two-phase electrolytic systems was still rudimentary. However, the earlier arrangements persisted in subsequent generations [81], and little has changed in the meantime [82]. About 20 years ago, Hawkes put in the title of his article [83] a dramatic question, corresponding to his statement presented therein that “the simple algorithms in introductory texts usually produce dramatic and often catastrophic errors”; it is hard not to agree with this opinion.

In the meantime, Meites et al. [84] stated that “It would be better to confine illustrations of the solubility product principle to 1:1 salts, like silver bromide (…), in which the (…) calculations will yield results close enough to the truth.” The unwarranted simplifications cause confusion in teaching of chemistry. Students will trust us enough to believe that a calculation we have taught must be generally useful.

The theory of electrolytic systems, perceived as the main problem in the physicochemical studies for many decades, is now put on the side. It can be argued that the gaining of quantitative chemical knowledge in the education process is essentially based on the stoichiometry and proportions.

Overview of the literature indicates that the problems of dissolution and solubility calculation are not usually resolved in a proper manner; positive (and sole) exceptions are the studies and practice made by the authors of this chapter. Other authors, e.g., [13, 85], rely on the simplified schemes (ready-to-use formulas), which usually lead to erroneous results, expressed by dissolution denoted as s* [mol/L]; the values for s* are based on stoichiometric reaction notations and expressions for the solubility product values, specified by Eqs. (1) and (2). The calculation of s* contradicts the common sense principle; this was clearly stated in the example with Fe(OH)3 precipitate. Equation (27) was applied to struvite [50] and dolomite [86], although these precipitates are nonequilibrium solid phases when introduced into pure water, as were proved in Refs. [2023]. The fact of the struvite instability was known at the end of nineteenth century [49]; nevertheless, the formula s* = (Ksp)1/3 for struvite may be still encountered in almost all textbooks and learning materials; this problem was raised in Ref. [15]. In this chapter, we identified typical errors involved with s* calculations, and indicated the proper manner of resolution of the problem in question.

The calculations of solubility s*, based on stoichiometric notation and Eq. (3), contradict the calculations of s, based on the matter and charge preservation. In calculations of s, all the species formed by defined element are involved, not only the species from the related reaction notation. A simple zeroing method, based on charge balance equation, can be applied for the calculation of pH = pH0 value, and then for calculation of concentrations for all species involved in expression for solubility value.

The solubility of a precipitate and the pH-interval where it exists as an equilibrium-solid phase in two-phase system can be accurately determined from calculations based on charge and concentration balances, and complete set of equilibrium constant values referred to the system in question.

In the calculations performed here we assumed a priori that the Ksp values in the relevant tables were obtained in a manner worthy of the recognition, i.e., these values are true. However, one should be aware that the equilibrium constants collected in the relevant tables come from the period of time covering many decades; it results from an overview of dates of references contained in some textbooks [31, 85] relating to the equilibrium constants. In the early literature were generally presented the results obtained in the simplest manner, based on Ksp calculation from the experimentally determined s* value, where all soluble species formed in solution by these ions were included on account of simple cations and anions forming the expression for Ksp. In many instances, the Ksp* values should be then perceived as conditional equilibrium constants [87]. Moreover, the differences between the equilibrium constants obtained under different physicochemical conditions in the solution tested were credited on account of activity coefficients, as an antidote to any discrepancies between theory and experiment.

First dissociation constants for acids were published in 1889. Most of the stability constants of metal complexes were determined after the announcement 1941 of Bjerrum’s works, see Ref. [88], about ammine-complexes of metals, and research studies on metal complexes were carried out intermittently in the twentieth century [89]. The studies of complexes formed by simple ions started only from the 1940s; these studies were related both to mono- and two-phase systems. It should also be noted that the first mathematical models used for determination of equilibrium constants were adapted to the current computing capabilities. Critical comments in this regard can be found, among others, in the Beck [90] monograph; the variation between the values obtained by different authors for some equilibrium constants was startling, and reaching 20 orders of magnitude. It should be noted, however, that the determination of a set of stability constants of complexes as parameters of a set of suitable algebraic equations requires complex mathematical models, solvable only with use of an iterative computer program [9193].

The difficulties associated with the resolution of electrolytic systems and two-phase systems, in particular, can be perceived today in the context of calculations using (1o) spreadsheets (2o) iterative calculation methods. In (1o), a calculation is made by the zeroing method applied to the function with one variable; both options are presented in this chapter.

The expression for solubility products, as well as the expression of other equilibrium constants, is formulated on the basis of mass action law (MAL). It should be noted, however, that the underlying mathematical formalism contained in MAL does not inspire trust, to put it mildly. For this purpose, the equilibrium law (EL) based on the Gibbs function [94] and the Lagrange multipliers method [9597] with laws of charge and elements conservation was suggested lately by Michałowski.

From semantic viewpoint, the term “solubility product” is not adequate, e.g., in relation to Eq. (8). Moreover, Ksp is not necessarily the product of ion concentrations, as indicated in formulas (4), (5), and (11). In some (numerous) instances of sparingly soluble species, e.g., sulfur, solid iodine, 8-hydroxyquinoline, dimethylglyoxime, the term solubility product is not applied. In some instances, e.g., for MnO2, this term is doubtful.

One of the main purposes of the present chapter is to familiarize GEB within GATES as GATES/GEB to a wider community of analysts engaged in electrolytic systems, also in aspect of solubility problems.

In this context, owing to large advantages and versatile capabilities offered by GATES/GEB, it deserves a due attention and promotion. The GATES is perceived as a step toward reductionism [19, 71] of chemistry in the area of electrolytic systems and the GEB is considered as a general law of nature; it provides the real proof of the world harmony, harmony of nature.

© 2017 The Author(s). Licensee IntechOpen. This chapter is distributed under the terms of the Creative Commons Attribution 3.0 License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

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Anna Maria Michałowska-Kaczmarczyk, Aneta Spórna-Kucab and Tadeusz Michałowski (August 23rd 2017). Solubility Products and Solubility Concepts, Descriptive Inorganic Chemistry Researches of Metal Compounds, Takashiro Akitsu, IntechOpen, DOI: 10.5772/67840. Available from:

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