Softening waters by ion-exchange method 
  
                              RIGIDITY of WATER 
Scum and adjournment of salts on home appliances (for example, in  teapots), 
film on tea etc. - all this parameters of rigid water.  Use  of  such  water 
for the economic purposes causes a number of  inconveniences.  For  example, 
the charge of a soap is increased at washing,  slowly  boil  soft  meat  and 
vegetables, service life of  home  appliances  decreases.  Interrelation  of 
rigidity of water and education of stones in kidneys now is known. 
The rigidity of drinking water under the working  standards  should  be  not 
higher              7  mg-ecv/g,  and  only  in  the  special  cases  it  is 
supposed up to 10 mg-ecv/g. For the industrial purposes use of  rigid  water 
is inadmissible. 
The general rigidity of water is a set of properties caused by the contents 
in it ions of magnesium and calcium. 
Hard water must be soften before  use. 
The first way – reagent method  i.e., addition slaked to  exhaust  and  soda 
Na2CO3 (a limy way), addition of polyphosphates. 
The second way - application of cationits , i.e., synthetic ion-exchange 
pitches (filtering). 
                            Ion-exchange pitches 
These are substances capable to an ionic exchange at  contact  to  solutions 
of electrolits. Ionic-exchange clearing allows to take and  utilize  a  wide 
spectrum  of  polluting  substances:  heavy  metals,  chrom,  nitrates   and 
nitrites, cyanic connections, radioactive substances, and also умягчает  and 
unironing water. Thus the high degree of clearing (up to a level of  maximum 
concentration limit) is  reached.  Except  for  that  ionits  are  used  for 
unsalting waters during water-preparation. Inorganic and organic ionits  can 
be natural (for example: zeolites,  cellulose,  peat,  wood)  and  synthetic 
(silica gel and the most important ion-exchange pitches).   Depending  on  a 
degree dissociation  of   ion-exchange  pitches  can  be  strong  and  weak. 
Depending on a sort of ions which are connected to active groups of  ionits, 
distinguish the following its form: for cationits - the  hydrogen  form  (H- 
form) and the salt form, when active groups are connected to ions of  metals 
(for example,  Na-form,  NH4-form),  for  anionits  OH-form,  Cl-form,  etc. 
Ability of ionits to a full exchange is characterized by  exchange  capacity 
which is equal to number of its active groups participating in an  exchange. 
For the quantitative characteristic of  ion-exchange  properties  of  ionits 
usually define their dynamic and sometimes full (general) exchange  capacity 
(static). Main  requirements  to  ionits,  used  for  water  treating:  high 
exchange capacity, high speed of an ionic exchange, sufficient stability  in 
relation to acids, alkalis, oxidizers and reducers, insolubility  in  water, 
organic  solvents  and  solutions  of  electrolits  and   limited   swelling 
capacity. In water-preparation in a conditions of life are  frequently  used 
high-acid cationits domestic and import manufacturers mainly  for  softening 
and iron removal of waters. An example: the structure of  cationits  can  be 
expressed formula Na2R, where Na+ - rather mobile cation. If  to  pass  hard 
water through layers of  cationits  ions  of  sodium  exchange  on  ions  of 
calcium and magnesium: 
                         Ca 2 + + Na2R = 2Na + + CaR 
                         Mg 2 + + Na2R = 2Na + + MgR 
Thus ions Ca2+ and Mg2+ pass from a solution to cationit, and ions  Na+-from 
 cationit in a solution, and rigidity is eliminated. After pauperization  of 
cationit ions of Na+ cationits usually recycle. Them  maintain  in  solution 
NaCl where there is a return replacement - ions Na+ pass  in  cationit,  and 
ions Ca2+ and Mg2+ - in a solution: 
                          CaR + 2Na+ = Na2R + Ca 2+ 
                         MgR + 2Na + = Na2R + Mg 2+ 
 After that regenerated cationit can be used for mitigation of new  portions 
of hard water. The  degree  of  regeneration  is  influenced  with  type  of 
ionits, structure of the  sated  layer,  the  nature,  concentration  and  a 
solution of recycling  substance,  temperature,  time  of  contact  and  the 
charge  of  reagents.  Restoration  of  exchange  capacity  at  regeneration 
usually makes 60 - 100 %. 
                              Kinds of rigidity 
General rigidity. It is defined by total concentration of  ions  of  calcium 
and magnesium. Represents  the  sum  of  carbonate  (time)  and  uncarbonate 
(constant) rigidity. 
Carbonate rigidity. It is caused by presence  in  water  of  hydrocarbonates 
and carbonates (at рН>  8.3)  calcium  and  magnesium.  The  given  type  of 
rigidity almost completely is eliminated at boiling waters and  consequently 
refers to as time rigidity. At heating water hydrocarbonates break  up  with 
formation of a coal acid and settling out of  a  carbonate  of  calcium  and 
oxyhydroxide of magnesium. 
Uncarbonate rigidity. It is caused by presence calcium and  magnesian  salts 
of strong acids (the chamois, nitric, hydrochloric) and  at  boiling  it  is 
not eliminated (constant rigidity). 
                             Origin of rigidity 
      Ions of calcium (Ca2+) and magnesium (Mg2+), and also  others  alkali- 
ground metals causing rigidity, are  present  at  all  mineralizeed  waters. 
Their source are natural deposits of limestones, plaster and dolomite.  Ions 
of calcium and magnesium act in water as a result of  interaction  dissolved 
dioxide of carbon with minerals and at other processes  of  dissolution  and 
chemical aeration of rocks. As a source of these ions,  the  microbiological 
processes proceeding in soil on the area of a reservoir can serve in  ground 
adjournment, and also sewage of the various enterprises also. 
      Rigidity of water changes over a wide range and  there  is  a  set  of 
types of classifications of water on a degree of its  rigidity.  Usually  in 
little mineralizeed waters prevails (up to 70%-80 %) the rigidity caused  by 
ions of calcium (though  in  separate  rare  cases  magnesian  rigidity  can 
reach(achieve) 50-60 %). With increase in a degree of  a  mineralization  of 
water the contents of ions  of  calcium  (Са2+)  quickly  falls  and  seldom 
exceeds  1  g/l.  The  contents  of  ions  of  magnesium  (Mg2+)   in   high 
mineralizeed waters can reach several grammes, and in  salty  lakes  -  tens 
grammes on one litre of water.As a whole, rigidity  of  superficial  waters, 
as a rule,  is  less  than  rigidity  of  waters  underground.  Rigidity  of 
superficial  waters  is  subject  to  appreciable   seasonal   fluctuations, 
reaching usually the greatest value at the  end  of  winter  and  the  least 
during a high water when it is plentifully  diluted  soft  rain  and  thawed 
snow. Sea and ocean water have very high rigidity (tens and hundreds in   mg 
- ecv/l) 
                            Influence of rigidity 
From the point of view of application  of  water  for  drinking  needs,  its 
acceptability on a degree of rigidity  can  vary  essentially  depending  on 
local conditions. The threshold of taste for an  ion  of  calcium  lays  (in 
recalculation on a mg - equivalent) in a range of 2-6 mg - ecv/l,  depending 
on corresponding of anionits, and a threshold of  taste  for  magnesium  and 
than that is lower. In some cases water is comprehensible to consumers  with 
rigidity above 10 mg-ecv/l. High rigidity  worsens  organoleptic  properties 
of water, giving to it bitterish taste and  having  negative  an  effect  on 
bodies of digestion. 
 The world Organization of Public health services (CART) does not offer  any 
recommended size of rigidity under indications of influence  on  health.  In 
materials the CART is spoken that though a  number  of  researches  and  has 
revealed statistically inverse  relationship  between  rigidity  of  potable 
water  and  the  cardiovascular  diseases,  the  available  data   are   not 
sufficient for a conclusion about causal character  of  this  communication. 
Similarly, unequivocally it  is  not  proved,  that  soft  water  renders  a 
negative effect on balance of mineral  substances  of  an  organism  of  the 
person 
At the same time, depending on рН and alkalinity,  water  with  rigidity  of 
                    4  mg-ecv/l  can  above  cause  in  distributive  system 
adjournment of slags and scums (a carbonate  of  calcium),  is  especial  at 
heating. For this reason  norms  of   Boiler  inspection  enter  very  rigid 
requirements to size of rigidity of the water used for  a  meal  of  boilers 
(0.05-0.1 mg-ecv/l). Besides  at  interaction  of  salts  of  rigidity  with 
washing substances (the soap, detergent powders, shampoos) occurs  formation 
of  "soap  slags"  as  foam.  It  results  not  only  in   the   significant 
overexpenditure of washing-up liquids. Such foam after drying remains  as  a 
strike on the sanitary technician, linen, a human skin, on hair  (unpleasant 
feeling of "rigid" hair well-known to much). The main negative influence  of 
these slags on the person is that they destroy a  natural  fatty  film  with 
which the normal skin is always covered and hammer its  time.  An  attribute 
of such negative influence is characteristic "scratch" of cleanly washed  up 
skin or hair. It  appears,  that  the  irritation  causing  in  some  people 
feeling "soapiness" after using soft water  is  an  attribute  of  that  the 
protective fatty film on a skin is whole and safe. It also slides. 
At the same time, it is necessary to mention and  other  side  of  a  medal. 
Soft water with rigidity less  than  2  mg-ecv/l  has  low  buffer  capacity 
(alcalinity) and can, depending on a level рН and  of  some  other  factors, 
render the increasedcorrosive attack to water pipes. Therefore, in a  number 
of applications (it is especial in the heating  engineer)  sometimes  it  is 
necessary to carry out special processing  of  water  with  the  purpose  of 
achievement of an optimum ratio between rigidity of water and its  corrosion 
activity. 
                              EXPERIMENTAL PART 
    The  adsorption  processes including both processes  cleanly  including 
physical,  and  the  processes  conducting  to  formation  of  new  chemical 
substances are  rather  various.  Processes  concern  to  them  ion-exchange 
chromatographies proceeding  between  ionits  and  solutions  of  electrolit 
also. 
    Due to the universality and these processes have found  of  flexibility 
wide application in  analytical  chemistry,  food  and  an  iron  and  steel 
industry, in power system, water-preparation and in many other  areas  of  a 
science  and  technics(technical  equipment),  and  now  supersede  from  an 
industrial practice  other  methods  sorption  [1-3].  Despite  of  the  big 
assortment  industrial   ionits,   the   majority   of   them,   especially, 
condensation type differ such low parameters, as low speed  sorption,  small 
stability to thermal, chemical influences, etc. It limits opportunities  and 
spheres of their application [4,5]. 
    By us it is received new monofunctional sulphocationite on the basis of 
interaction of styrene with an accessible and cheap  waste  of  agricultural 
and cotton scraping industries. 
    [pic] 
    Sorption abilities of  sulphocationite to ions of  calcium,  magnesium, 
copper, nickel carried out research from 0.1N  solutions  of  СаСl2,  MgCl2, 
CuSO4  and  NiSO4.  Sorption  of  calcium  and   magnesium   determined   by 
trilonometric, copper by iodometric, nickel   by  photocolorimetric  methods 
[10,11]. 
    According to the literary data, polymers and  ion-exchangers,  received 
on the basis of  derivatives  of  furan   differ  from  raised  thermal  and 
chemical stability and mechanical durability [5,6]. The basic properties  of 
 received sulphocationite are submitted in table 1. 
                                                                     Table 1 
    The main physical and chemical parameters of received sulphocationite 
|№ |Parameters                                           |Values      | 
|1.|Bulk weight, g/ml                                    |0.68        | 
|2.|Specific volume of bulk cationit in Н-form, ml/g     |3.5         | 
|3.|Static exchange capacity, in mg - ecv/g, on:         |            | 
|  |0.1N. solution of NaOH                               |5,2         | 
|  |0.1N. solution of NaCl                               |4.5         | 
|  |0.1N. solution of СaCl2    |Н-form                  |4.2         | 
|  |                           |Nа-form                 |4.8         | 
|  |0.1N. solution  of MgCl2   |Н-form                  |3.0         | 
|  |                           |Nа-form                 |3.8         | 
|  |0.1 N. solution of СuSO4   |Н-form                  |2.6         | 
|  |                           |Nа-form                 |3.0         | 
|  |0.1 N. solution of NiSO4   |Н-form                  |2.15        | 
|  |                           |Nа-form                 |2.34        | 
|4.|Mechanical durability                                |99 %        | 
    As is known in many regions of our republic  used  in  a  life  and  on 
manufacture water has high rigidity which sometimes reaches  up  to  12  mg- 
ecv/l instead of 2874-82 "Potable water" received according to GOST –  2.5-7 
mg-ecv/l. 
    From the data of table 1 it is  visible,  that  the  examinee  cationit 
possesses high enough parameters of size of exchange  capacity  on  ions  of 
calcium and magnesium. As object of  research  we  had  been  used  artesian 
water of area Shurchi in Surkhan-Darya area which has rigidity of  12.2  mg- 
ecv/l. Cationits tested in              Н-and Na-forms. 
    1 gr. of cationit filled in 200 ml of researched  water.  In  24  hours 
water separated from cationit  and  determined  its  rigidity  trilonometric 
method at the presence of the indicator chromogen black.  Thus  rigidity  of 
water in the Н-form has made 4.5 mg - ecv/l, and in the Na-form of 2.2 mg  - 
ecv/l. 
    Except for it we had been carried out researches on softening water  of 
                   2.5  mg-ecv/l having rigidity.  After  contact  within  6 
hours of water with cationit  rigidity of it corresponded  at  use  cationit 
in: 
    the Н-form – 0.8 mg-ecv/l; 
    the Na-form – 0.4 mg-ecv/l. 
    Results of the received researches testifies to perspectivity  of  work 
with the examinee with sulphocationite. 
                                 Vocabulary 
|Adjournment                  |––– |Отложения                       | 
|Artesian water               |––––|Артезианская вода               | 
|Cationit                     |––––|Катионит                        | 
|Anionit                      |––––|Анионит                         | 
|Sorption                     |––––|Сорбция                         | 
|Sulphocationite              |––––|Сульфокатионит                  | 
|Rigidity                     |––––|Жесткость                       | 
|Indicator chromogen black    |––––|Индикатор хромоген черный       | 
|Thrilonometric               |––––|Трилонометрический              | 
|Bulk weight                  |––––|Насыпной вес                    | 
|Condensation                 |––––|Конденсация                     | 
|Hydrocarbonate               |––––|Гидрокарбонат                   | 
|Slag                         |––––|Шлак                            | 
|Scum                         |––––|Накипь                          | 
|Ionits                       |––––|Ионит                           | 
|Alkalinity                   |––––|Щелочность                      | 
|Softening                    |––––|Умягчение                       | 
|Calcium                      |––––|Кальций                         | 
|Magnesium.                   |––––|Магний                          | 
|Sewage                       |––––|Сточные воды                    | 
|Corrosion activity           |––––|Деятельность коррозии           | 
|Static exchange capacity     |––––|Статическая обменная емкость    | 
|Swelling capacity            |––––|Влажность                       | 
|Iodometric,                  |––––|Иодометрический                 | 
|Photocolorimetric            |––––|Фотокалориметрический           | 
|Chemical stability           |––––|Химическая устойчивость         | 
|Thermal stability            |––––|Термическая устойчивость        | 
|Reagent method               |––––|Реагентный метод                | 
|Potable water                |    |Питьевая вода                   | 
|Cotton scraping industries   |    |Хлопчатоочистительная пром.     | 
|Polycondensation             |    |Поликонденсация                 | 
|Correspond                   |    |Переписываются                  | 
|Сopper                       |    |Медь                            | 
|desorption                   |    |Десорбция                       | 
|Potentiometric titration     |    |Потенциометрич. титрование      | 
|Flexibility                  |    |Гибкость                        | 
|Specific volume              |    |Удельный объем                  | 
                                 Литература 
1. Полянский Н.Г.  Сб.  Синтез  и  свойства  ионообменных  материалов»,  М.: 
 «Наука»,1968г. 
2. Либинсон Г.С. Физико-химические свойства  карбоксильных  катионитов,  М.: 
 «Наука», 1969. 
3. Гельферих Ф. «Иониты»,М.: Изд. ИЛ., 1962 г. 
4. Таджиходжаев З.А. Разработка  ионообменных  и  композиционных  материалов 
 многофункционального назначения на основе вторичных продуктов  производств 
 и технологии их получения».: Автореф. дисс. доктора технических  наук.  «, 
 Ташкент.: 2002. 
5.  Муталов Ш.А., Турсунов Т., Назирова   Р.А.  Исследование  сорбции  ионов 
 цветных металлов слабоосновными анионитами  поликонденсационного  типа./Ж. 
 Композиционные материалы. № 2, С.7-8. Ташкент:. 2003. 
6.   Таджиходжаев  З.А.,  Джалилов  А.Т.  Синтез  и   исследование   свойств 
 катионообменных   смол   на   основе   вторичных   продуктов    химических 
 предприятий.// Ж. Прикл. химии. 1998. т. 72. № 9. С. 1578-1580. 
7. Гриссбах Р. «Теория и практика  ионного  обмена»,  М.:  Изд.  ИЛ.  1963., 
                   с. 303 – 310. 
8. Л.Беллами «Инфракрасные спектры сложных молекул», М.: ИЛ, 1963г. 
9.  Алексеев В.Н. «Количественный анализ», М.: Химия, 1972г. 
10.     Пешкова   В.М.,   Громова   М.И.   Практическое    руководство    по 
 спектрофотометрии и калориметрии. М.: Изд.«Московского Университета», 1965 
 г. 
----------------------- 
... 
... 
CH2 
CH 
CH 
O 
+ 
H 
O 
C 
O 
CH=CH2 
... 
... 
CH2 
CH 
CH 
O 
+ 
H 
O 
C 
O 
CH=CH2 
Страницы: 1, 2 
   
  |