Chemistry of sea water Constancy of composition

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Presentation transcript:

Chemistry of sea water Constancy of composition Elements present in sea water Artificial sea water Dissolves gases in sea water Carbondioxide system and alkalinity Inorganic agencies affecting composition of sea water.

Seawater is a complex mixture of 96. 5% water, 2 Seawater is a complex mixture of 96.5% water, 2.5% salts, and small amounts of other substances. chemical formula for water is H2O and for salt NaCl.Chemical formula for water is H2o . Its atomic weight is 18.Chemical formula of salt depends on the compounds or elements under going reaction when producing a saltcommon salts are Sodium chloride...

Water molecule

Constancy of composition The ration of any two major salt constituents in ocean water is constant and is independent of salinity To quantity salinity – measure of single major ion dissolved in sample of seawater is enough Cl is measured to determine salinity The principle of constant composition was evolved during glomar challenger eypedition The ration of Na+/K+ or cl /So42 is a fixed value weather the salinity is 25,30,50% or whatever.

Elements present in sea water Ion Concentration Percent Free Ion g/kg mMa Cl- 19.354 558 100 Na+ 10.77 479 98 Mg++ 1.290 54.3 89 SO4-- 2.712 28.9 39 Ca++ 0.412 10.5 88 K+ 0.399 10.4 HCO3-b 0.12 2.0 80

Ag silver AgCl-2 25 pmol/kg++ Al Aluminium Al(OH)-4 20nmol/kg Ar argon Ar (gas)   As Arsenic AsO4H2- 23nmol/kg Au Gold AuCl-4 ? B Boron B(OH)3 0.42mmol/kg Ba Barium Ba2+ 100nmol/kg Be beryllium BeOH+, Be(OH) ° 2 20 pmol/kg Bi Bismuth BiO+ ,Bi (OH)+2 0.01-0.2 pmol/kg Br Bromine Br- 0.84mmol/kg

C Carbon Co3+ H-, organic C 2.3mmol/kg Ca Calcium Ca2+ 10.3mmol/kg Cd Cadmium CdCl ° 2 0.7nmol/kg Ce Cerium CeCO+3, Ce3+, CeCl2+ 20 pmol/kg Cl Chlorine Cl- 0.546 mol/kg Co Cobalt Co2+,CoCO ° 3 , CoCl+ 0.02nmol/kg Cr Chromium CrO2-4, NaCrO4 4nmol/kg Cs Cesium Cs+ 2.2nmol/kg Cu Copper CuCo ° 3 ,CuOH+, Cu2+ F Fluorine F-, MgF+ 68 µ mol/kg Fe Iron Fe(OH) ° 3 1 nmol/kg Ga Gallium Ga(OH)-4 ? Ge Germanium Ge(OH)4, H3Geo-4 70 pmol/kg H Hydrogen H2O   He helium He(gas)

Trace elements in seawater Chemical ingredients that occur in minute guantities in the ocean Mn,pb,Hg,Au,I and iron (fe)occur in concentration less than 1 ppm Low concentrations make certain elements difficult to detect Trace elements are critically important for marine organisms.

Trace elements in seawater Concentration(ppb)* Lithium(Li) 170 Iodine (I) 60 Molybdenum (Mo) 10 Zinc (Zn) Iron (Fe) Aluminium (Al) Copper(Cu) 3 Manganese(Mn) 2 Cobalt (Co) 0.1 Lead (Pb) 0.03 Mercury (Hg) Gold(Au) 0.004

Gases in seawater include Nitrogen (N2) Oxygen (O2) Carbondioxide (Co2) Hydrogen (H2) And noble gases-Argon (Ar) neon (Ne), helium (He) Nitrogen and noble gases are unreactive and do not involve in photosynthesis. Oxygen and CO2 involve in photosynthesis and respiration and they vary with space

Dissolved gases % in sea water S.No Gas In surface ocean water % 1. Nitrogen (N2) 47.5 2. Oxygen(O2) 36.0 3. Carbondioxide 15.1

Dissolved gases in sea water In Dry Air (%) In Surface Ocean Water (%) Water-Air Ratio Nitrogen (N2) 78.03 47.5 0:6 Oxygen(O2) 20.99 36.0 1:7 Carbon dioxide(CO2) 0.03 15.1 503:3 Argon (Ar), hydrogen(H2), neon (Ne) and helium (He) 0.95 1.4 1:5

Carbon dioxide and carbonate cycles Ocean the major reservoir of CO2 Ocean contains 50% of CO2 in Atmosphere CO2 occurs as dissolved gas Highly soluble in seawater Respiration of Plants and Animals produce CO2 CO2 in sea water forms H2CO3 Formation and destruction of carbonate shells affects the abundance of carbonate in sea water The exchange of CO2 with atmosphere will be at the rate proportional to difference in partial pressure of gas in two media. The rate of which the exchange of CO2 between atmosphere and sea interface depends on the rate at which carbon is exchanged between surface layer and deep ocean

Alkalinity AT is measure of ability of a solution to neutralize acids to the equivalence point of corbonate or biearbonate. Alkalinity is equal to the stoichrometric sum of the bases in solution In nature carbonate alkalinity makes up most of the total alkalinity Compounds that controbute to alkalinity include borate, hydroxide, phosphate, silicate, nitrate and dissolved ammonia.

Dissolved Inorganic matter The inorgonic mater in seawater includes Co3, So42 , Cl, No3, Ca++,Mg++

Inorganic agencies affecting composition of sea water Inflow of river water, freezing and melting of sea ice, biological activity, and exchange of substances with Atmosphere are the factors – affecting composition of seawater. Spray along the shores also leads to removal of salts along shores choride content in water is varied through this process Exchange of gases also modify the quantity of substances in seawater