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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.

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.

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