KUSHESHWAR STHAN CHAUR (North Bihar)
KUSHESHWAR STHAN CHAUR (North Bihar)
KUSHESHWAR STHAN CHAUR (North Bihar)
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Table I1 : Soil characteristifs of Kushesbwar sthan<br />
Parameters<br />
1 values<br />
I Sand (%)<br />
Organic carbon content(%) 0.48-2.1<br />
~aramners<br />
Water temp(%!)<br />
Table I11 : Water Quality of Kusheshwar sthan Chaurs<br />
Kusheshwar Kamaldaha Dabadih Mahisalh<br />
28.4-28.8 28.2-28.7 28.2-28.7 28.2.28.7<br />
Dqmgl")<br />
7.04.8.20<br />
5.4.6.6<br />
5.0.6.2<br />
5.0.6.4<br />
Total Alkalinity (rngi'l)<br />
56-60<br />
60.68<br />
55-70<br />
65-75<br />
Phosphate (rngl")<br />
Nil<br />
Tr.0.001<br />
Tr.O.005<br />
Tr.0.003<br />
Niaatc( rngk')<br />
Traces-0.09<br />
0.01.0.06<br />
0.0-0.05<br />
0.02-0.10<br />
The rich nutrient level of the soil was not reflected at the water phase as the<br />
value were very low in traces. However, total alkalinity (56 to 75 ppm) and the specific<br />
conductance (160-440 rnmhos cm-'), indicated moderate productivity of these<br />
waterbodies. Ihe dense proliferation of aquatic macrophytes in certain chaurs acts as a<br />
bulwark to the release of nubients in the water phase from the soil, due to locking of<br />
nutrients in the hydrophytic chain. Further, reccurance of flood in the chaw area<br />
accelerates the deposition of silt, which in turn might have been forming canopies over
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