How can you use ICE tables to solve multiple coupled equilibria?How to calculate the concentration of all relevant species in a buffer of a given pH?Determining equilibrium concentrations from initial conditions and equilibrium constantDetermining solubility of silver sulfate in its saturated solutionIs LiOH a weaker base than NaOH?What's the Kp value?Equilibrium Bond Dissociationice tables equilibirium qConfusion about the ICE tableHow do I find the theoretical pH of a buffer solution after HCl and NaOH were added, separately?Q. 36 2018 molar solubility of CaF2 at pH3 given molar solubility at pH7 and pKa of HF

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How can you use ICE tables to solve multiple coupled equilibria?


How to calculate the concentration of all relevant species in a buffer of a given pH?Determining equilibrium concentrations from initial conditions and equilibrium constantDetermining solubility of silver sulfate in its saturated solutionIs LiOH a weaker base than NaOH?What's the Kp value?Equilibrium Bond Dissociationice tables equilibirium qConfusion about the ICE tableHow do I find the theoretical pH of a buffer solution after HCl and NaOH were added, separately?Q. 36 2018 molar solubility of CaF2 at pH3 given molar solubility at pH7 and pKa of HF













4












$begingroup$


If I have a problem involving multiple coupled equilibrium reactions, such as




Calcium fluoride, $ceCaF2$, has a molar solubility of $pu2.1e−4 mol L−1$ at pH = 7.00. By what factor does its molar solubility increase in a solution with pH = 3.00? The p$K_mathrma$ of $ceHF$ is 3.17.




The relevant reactions are:



$$ceCaF2(s) <=> Ca^2+(aq) + 2 F-(aq)$$ and
$$ceHF(aq) <=> H+(aq) + F-(aq)$$



They are coupled because fluoride occurs in both of them.



Is there a way to use ICE tables to organize the information (stoichiometry, initial concentrations, mass balance) as a way to solve the problem?



For example, I could try to set up one ICE table for each reaction (the column for $ceH+$ is strange because in the problem, the pH is set to a value through an unspecified mechanism):



$$
beginarray
hline
&[ceCa^2+] & [ceF-] \
hline
I & pu2.1e−4 & pu4.2e−4 \
hline
C & +x & +2x \
hline
E & pu2.1e−4+x & pu4.2e−4+2x \
hline
endarray
$$



and



$$
beginarray
hline
&[ceHF] & [ceH+] & [ceF-] \
hline
I & 0 & textN/A & pu4.2e−4 \
hline
C & +x &textN/A & -x \
hline
E & +x & 10^-3.00 & pu4.2e−4 - x\
hline
endarray
$$



However, how do the fluoride concentrations "talk to each other" in the two tables? Is the $x$ in one table the same as the $x$ in the other table?










share|improve this question











$endgroup$











  • $begingroup$
    Your "initial state" seems to be pH 7 so you do know the [H+] at the start.
    $endgroup$
    – Tan Yong Boon
    3 hours ago










  • $begingroup$
    Yes, but the pH is adjusted externally, so we can't take the change in [H+] to deduce how much [HF] and [F-] are changing. For that reason, I left that box as N/A. I could have left the entire column out instead.
    $endgroup$
    – Karsten Theis
    2 hours ago















4












$begingroup$


If I have a problem involving multiple coupled equilibrium reactions, such as




Calcium fluoride, $ceCaF2$, has a molar solubility of $pu2.1e−4 mol L−1$ at pH = 7.00. By what factor does its molar solubility increase in a solution with pH = 3.00? The p$K_mathrma$ of $ceHF$ is 3.17.




The relevant reactions are:



$$ceCaF2(s) <=> Ca^2+(aq) + 2 F-(aq)$$ and
$$ceHF(aq) <=> H+(aq) + F-(aq)$$



They are coupled because fluoride occurs in both of them.



Is there a way to use ICE tables to organize the information (stoichiometry, initial concentrations, mass balance) as a way to solve the problem?



For example, I could try to set up one ICE table for each reaction (the column for $ceH+$ is strange because in the problem, the pH is set to a value through an unspecified mechanism):



$$
beginarray
hline
&[ceCa^2+] & [ceF-] \
hline
I & pu2.1e−4 & pu4.2e−4 \
hline
C & +x & +2x \
hline
E & pu2.1e−4+x & pu4.2e−4+2x \
hline
endarray
$$



and



$$
beginarray
hline
&[ceHF] & [ceH+] & [ceF-] \
hline
I & 0 & textN/A & pu4.2e−4 \
hline
C & +x &textN/A & -x \
hline
E & +x & 10^-3.00 & pu4.2e−4 - x\
hline
endarray
$$



However, how do the fluoride concentrations "talk to each other" in the two tables? Is the $x$ in one table the same as the $x$ in the other table?










share|improve this question











$endgroup$











  • $begingroup$
    Your "initial state" seems to be pH 7 so you do know the [H+] at the start.
    $endgroup$
    – Tan Yong Boon
    3 hours ago










  • $begingroup$
    Yes, but the pH is adjusted externally, so we can't take the change in [H+] to deduce how much [HF] and [F-] are changing. For that reason, I left that box as N/A. I could have left the entire column out instead.
    $endgroup$
    – Karsten Theis
    2 hours ago













4












4








4





$begingroup$


If I have a problem involving multiple coupled equilibrium reactions, such as




Calcium fluoride, $ceCaF2$, has a molar solubility of $pu2.1e−4 mol L−1$ at pH = 7.00. By what factor does its molar solubility increase in a solution with pH = 3.00? The p$K_mathrma$ of $ceHF$ is 3.17.




The relevant reactions are:



$$ceCaF2(s) <=> Ca^2+(aq) + 2 F-(aq)$$ and
$$ceHF(aq) <=> H+(aq) + F-(aq)$$



They are coupled because fluoride occurs in both of them.



Is there a way to use ICE tables to organize the information (stoichiometry, initial concentrations, mass balance) as a way to solve the problem?



For example, I could try to set up one ICE table for each reaction (the column for $ceH+$ is strange because in the problem, the pH is set to a value through an unspecified mechanism):



$$
beginarray
hline
&[ceCa^2+] & [ceF-] \
hline
I & pu2.1e−4 & pu4.2e−4 \
hline
C & +x & +2x \
hline
E & pu2.1e−4+x & pu4.2e−4+2x \
hline
endarray
$$



and



$$
beginarray
hline
&[ceHF] & [ceH+] & [ceF-] \
hline
I & 0 & textN/A & pu4.2e−4 \
hline
C & +x &textN/A & -x \
hline
E & +x & 10^-3.00 & pu4.2e−4 - x\
hline
endarray
$$



However, how do the fluoride concentrations "talk to each other" in the two tables? Is the $x$ in one table the same as the $x$ in the other table?










share|improve this question











$endgroup$




If I have a problem involving multiple coupled equilibrium reactions, such as




Calcium fluoride, $ceCaF2$, has a molar solubility of $pu2.1e−4 mol L−1$ at pH = 7.00. By what factor does its molar solubility increase in a solution with pH = 3.00? The p$K_mathrma$ of $ceHF$ is 3.17.




The relevant reactions are:



$$ceCaF2(s) <=> Ca^2+(aq) + 2 F-(aq)$$ and
$$ceHF(aq) <=> H+(aq) + F-(aq)$$



They are coupled because fluoride occurs in both of them.



Is there a way to use ICE tables to organize the information (stoichiometry, initial concentrations, mass balance) as a way to solve the problem?



For example, I could try to set up one ICE table for each reaction (the column for $ceH+$ is strange because in the problem, the pH is set to a value through an unspecified mechanism):



$$
beginarray
hline
&[ceCa^2+] & [ceF-] \
hline
I & pu2.1e−4 & pu4.2e−4 \
hline
C & +x & +2x \
hline
E & pu2.1e−4+x & pu4.2e−4+2x \
hline
endarray
$$



and



$$
beginarray
hline
&[ceHF] & [ceH+] & [ceF-] \
hline
I & 0 & textN/A & pu4.2e−4 \
hline
C & +x &textN/A & -x \
hline
E & +x & 10^-3.00 & pu4.2e−4 - x\
hline
endarray
$$



However, how do the fluoride concentrations "talk to each other" in the two tables? Is the $x$ in one table the same as the $x$ in the other table?







equilibrium






share|improve this question















share|improve this question













share|improve this question




share|improve this question








edited 6 hours ago









Mathew Mahindaratne

3,870318




3,870318










asked 9 hours ago









Karsten TheisKarsten Theis

2,705434




2,705434











  • $begingroup$
    Your "initial state" seems to be pH 7 so you do know the [H+] at the start.
    $endgroup$
    – Tan Yong Boon
    3 hours ago










  • $begingroup$
    Yes, but the pH is adjusted externally, so we can't take the change in [H+] to deduce how much [HF] and [F-] are changing. For that reason, I left that box as N/A. I could have left the entire column out instead.
    $endgroup$
    – Karsten Theis
    2 hours ago
















  • $begingroup$
    Your "initial state" seems to be pH 7 so you do know the [H+] at the start.
    $endgroup$
    – Tan Yong Boon
    3 hours ago










  • $begingroup$
    Yes, but the pH is adjusted externally, so we can't take the change in [H+] to deduce how much [HF] and [F-] are changing. For that reason, I left that box as N/A. I could have left the entire column out instead.
    $endgroup$
    – Karsten Theis
    2 hours ago















$begingroup$
Your "initial state" seems to be pH 7 so you do know the [H+] at the start.
$endgroup$
– Tan Yong Boon
3 hours ago




$begingroup$
Your "initial state" seems to be pH 7 so you do know the [H+] at the start.
$endgroup$
– Tan Yong Boon
3 hours ago












$begingroup$
Yes, but the pH is adjusted externally, so we can't take the change in [H+] to deduce how much [HF] and [F-] are changing. For that reason, I left that box as N/A. I could have left the entire column out instead.
$endgroup$
– Karsten Theis
2 hours ago




$begingroup$
Yes, but the pH is adjusted externally, so we can't take the change in [H+] to deduce how much [HF] and [F-] are changing. For that reason, I left that box as N/A. I could have left the entire column out instead.
$endgroup$
– Karsten Theis
2 hours ago










1 Answer
1






active

oldest

votes


















5












$begingroup$

The way to use ICE tables in this case would be to combine the ICE tables, and use "$x$" for the changes due to one reaction and "$y$" for the changes due to the other. For each reaction, you have one unknown (how far it reacted, i.e. $x$ and $y$), so you need two pieces of information to solve it, in this case the two equilibrium constants.



Here is the combined ICE table:



$$
beginarrayc
hline
&[ceCa^2+] & [ceF-] & [ceH+]&[ceHF] \
hline
I & pu2.1e−4 & pu4.2e−4 & textN/A & 0 \
hline
C & +x & +2x-y & textN/A & +y \
hline
E & pu2.1e−4+x & pu4.2e−4+2x-y & 10^-3.00 & +y \
hline
endarray
$$



Now, you can use the equilibrium constants for the two reactions to solve for $x$ and $y$, giving you the equilibrium concentrations.



What the combined table shows is that the fluoride concentration depends on both reactions, so you can't first deal with one equilibrium and then with the other but have to solve a system of two equations with two unknowns.



Once you combine the tables, you could also have initial conditions where nothing is dissolved yet, to get easier expressions (I'm using $p$ and $q$ because they will be different from $x$ and $y$):



$$
beginarrayc
hline
&[ceCa^2+] & [ceF-] & [ceH+]&[ceHF] \
hline
I & 0 & 0 & textN/A & 0 \
hline
C & +p & +2p-q & textN/A & +q \
hline
E & +p & +2p-q & 10^-3.00 & +q \
hline
endarray
$$






share|improve this answer











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    1 Answer
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    1 Answer
    1






    active

    oldest

    votes









    active

    oldest

    votes






    active

    oldest

    votes









    5












    $begingroup$

    The way to use ICE tables in this case would be to combine the ICE tables, and use "$x$" for the changes due to one reaction and "$y$" for the changes due to the other. For each reaction, you have one unknown (how far it reacted, i.e. $x$ and $y$), so you need two pieces of information to solve it, in this case the two equilibrium constants.



    Here is the combined ICE table:



    $$
    beginarrayc
    hline
    &[ceCa^2+] & [ceF-] & [ceH+]&[ceHF] \
    hline
    I & pu2.1e−4 & pu4.2e−4 & textN/A & 0 \
    hline
    C & +x & +2x-y & textN/A & +y \
    hline
    E & pu2.1e−4+x & pu4.2e−4+2x-y & 10^-3.00 & +y \
    hline
    endarray
    $$



    Now, you can use the equilibrium constants for the two reactions to solve for $x$ and $y$, giving you the equilibrium concentrations.



    What the combined table shows is that the fluoride concentration depends on both reactions, so you can't first deal with one equilibrium and then with the other but have to solve a system of two equations with two unknowns.



    Once you combine the tables, you could also have initial conditions where nothing is dissolved yet, to get easier expressions (I'm using $p$ and $q$ because they will be different from $x$ and $y$):



    $$
    beginarrayc
    hline
    &[ceCa^2+] & [ceF-] & [ceH+]&[ceHF] \
    hline
    I & 0 & 0 & textN/A & 0 \
    hline
    C & +p & +2p-q & textN/A & +q \
    hline
    E & +p & +2p-q & 10^-3.00 & +q \
    hline
    endarray
    $$






    share|improve this answer











    $endgroup$

















      5












      $begingroup$

      The way to use ICE tables in this case would be to combine the ICE tables, and use "$x$" for the changes due to one reaction and "$y$" for the changes due to the other. For each reaction, you have one unknown (how far it reacted, i.e. $x$ and $y$), so you need two pieces of information to solve it, in this case the two equilibrium constants.



      Here is the combined ICE table:



      $$
      beginarrayc
      hline
      &[ceCa^2+] & [ceF-] & [ceH+]&[ceHF] \
      hline
      I & pu2.1e−4 & pu4.2e−4 & textN/A & 0 \
      hline
      C & +x & +2x-y & textN/A & +y \
      hline
      E & pu2.1e−4+x & pu4.2e−4+2x-y & 10^-3.00 & +y \
      hline
      endarray
      $$



      Now, you can use the equilibrium constants for the two reactions to solve for $x$ and $y$, giving you the equilibrium concentrations.



      What the combined table shows is that the fluoride concentration depends on both reactions, so you can't first deal with one equilibrium and then with the other but have to solve a system of two equations with two unknowns.



      Once you combine the tables, you could also have initial conditions where nothing is dissolved yet, to get easier expressions (I'm using $p$ and $q$ because they will be different from $x$ and $y$):



      $$
      beginarrayc
      hline
      &[ceCa^2+] & [ceF-] & [ceH+]&[ceHF] \
      hline
      I & 0 & 0 & textN/A & 0 \
      hline
      C & +p & +2p-q & textN/A & +q \
      hline
      E & +p & +2p-q & 10^-3.00 & +q \
      hline
      endarray
      $$






      share|improve this answer











      $endgroup$















        5












        5








        5





        $begingroup$

        The way to use ICE tables in this case would be to combine the ICE tables, and use "$x$" for the changes due to one reaction and "$y$" for the changes due to the other. For each reaction, you have one unknown (how far it reacted, i.e. $x$ and $y$), so you need two pieces of information to solve it, in this case the two equilibrium constants.



        Here is the combined ICE table:



        $$
        beginarrayc
        hline
        &[ceCa^2+] & [ceF-] & [ceH+]&[ceHF] \
        hline
        I & pu2.1e−4 & pu4.2e−4 & textN/A & 0 \
        hline
        C & +x & +2x-y & textN/A & +y \
        hline
        E & pu2.1e−4+x & pu4.2e−4+2x-y & 10^-3.00 & +y \
        hline
        endarray
        $$



        Now, you can use the equilibrium constants for the two reactions to solve for $x$ and $y$, giving you the equilibrium concentrations.



        What the combined table shows is that the fluoride concentration depends on both reactions, so you can't first deal with one equilibrium and then with the other but have to solve a system of two equations with two unknowns.



        Once you combine the tables, you could also have initial conditions where nothing is dissolved yet, to get easier expressions (I'm using $p$ and $q$ because they will be different from $x$ and $y$):



        $$
        beginarrayc
        hline
        &[ceCa^2+] & [ceF-] & [ceH+]&[ceHF] \
        hline
        I & 0 & 0 & textN/A & 0 \
        hline
        C & +p & +2p-q & textN/A & +q \
        hline
        E & +p & +2p-q & 10^-3.00 & +q \
        hline
        endarray
        $$






        share|improve this answer











        $endgroup$



        The way to use ICE tables in this case would be to combine the ICE tables, and use "$x$" for the changes due to one reaction and "$y$" for the changes due to the other. For each reaction, you have one unknown (how far it reacted, i.e. $x$ and $y$), so you need two pieces of information to solve it, in this case the two equilibrium constants.



        Here is the combined ICE table:



        $$
        beginarrayc
        hline
        &[ceCa^2+] & [ceF-] & [ceH+]&[ceHF] \
        hline
        I & pu2.1e−4 & pu4.2e−4 & textN/A & 0 \
        hline
        C & +x & +2x-y & textN/A & +y \
        hline
        E & pu2.1e−4+x & pu4.2e−4+2x-y & 10^-3.00 & +y \
        hline
        endarray
        $$



        Now, you can use the equilibrium constants for the two reactions to solve for $x$ and $y$, giving you the equilibrium concentrations.



        What the combined table shows is that the fluoride concentration depends on both reactions, so you can't first deal with one equilibrium and then with the other but have to solve a system of two equations with two unknowns.



        Once you combine the tables, you could also have initial conditions where nothing is dissolved yet, to get easier expressions (I'm using $p$ and $q$ because they will be different from $x$ and $y$):



        $$
        beginarrayc
        hline
        &[ceCa^2+] & [ceF-] & [ceH+]&[ceHF] \
        hline
        I & 0 & 0 & textN/A & 0 \
        hline
        C & +p & +2p-q & textN/A & +q \
        hline
        E & +p & +2p-q & 10^-3.00 & +q \
        hline
        endarray
        $$







        share|improve this answer














        share|improve this answer



        share|improve this answer








        edited 6 hours ago









        Mathew Mahindaratne

        3,870318




        3,870318










        answered 9 hours ago









        Karsten TheisKarsten Theis

        2,705434




        2,705434



























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            Старые Смолеговицы Содержание История | География | Демография | Достопримечательности | Примечания | НавигацияHGЯOLHGЯOL41 206 832 01641 606 406 141Административно-территориальное деление Ленинградской области«Переписная оброчная книга Водской пятины 1500 года», С. 793«Карта Ингерманландии: Ивангорода, Яма, Копорья, Нотеборга», по материалам 1676 г.«Генеральная карта провинции Ингерманландии» Э. Белинга и А. Андерсина, 1704 г., составлена по материалам 1678 г.«Географический чертёж над Ижорскою землей со своими городами» Адриана Шонбека 1705 г.Новая и достоверная всей Ингерманландии ланткарта. Грав. А. Ростовцев. СПб., 1727 г.Топографическая карта Санкт-Петербургской губернии. 5-и верстка. Шуберт. 1834 г.Описание Санкт-Петербургской губернии по уездам и станамСпецкарта западной части России Ф. Ф. Шуберта. 1844 г.Алфавитный список селений по уездам и станам С.-Петербургской губернииСписки населённых мест Российской Империи, составленные и издаваемые центральным статистическим комитетом министерства внутренних дел. XXXVII. Санкт-Петербургская губерния. По состоянию на 1862 год. СПб. 1864. С. 203Материалы по статистике народного хозяйства в С.-Петербургской губернии. Вып. IX. Частновладельческое хозяйство в Ямбургском уезде. СПб, 1888, С. 146, С. 2, 7, 54Положение о гербе муниципального образования Курское сельское поселениеСправочник истории административно-территориального деления Ленинградской области.Топографическая карта Ленинградской области, квадрат О-35-23-В (Хотыницы), 1930 г.АрхивированоАдминистративно-территориальное деление Ленинградской области. — Л., 1933, С. 27, 198АрхивированоАдминистративно-экономический справочник по Ленинградской области. — Л., 1936, с. 219АрхивированоАдминистративно-территориальное деление Ленинградской области. — Л., 1966, с. 175АрхивированоАдминистративно-территориальное деление Ленинградской области. — Лениздат, 1973, С. 180АрхивированоАдминистративно-территориальное деление Ленинградской области. — Лениздат, 1990, ISBN 5-289-00612-5, С. 38АрхивированоАдминистративно-территориальное деление Ленинградской области. — СПб., 2007, с. 60АрхивированоКоряков Юрий База данных «Этно-языковой состав населённых пунктов России». Ленинградская область.Административно-территориальное деление Ленинградской области. — СПб, 1997, ISBN 5-86153-055-6, С. 41АрхивированоКультовый комплекс Старые Смолеговицы // Электронная энциклопедия ЭрмитажаПроблемы выявления, изучения и сохранения культовых комплексов с каменными крестами: по материалам работ 2016-2017 гг. в Ленинградской области