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Luca Mologni,Carlo Gambacorti-Passerinig the physico-chemical parameters of groundwater. The chemical analysis results revealed that calcium is found to be the dominant cation followed by Mg., Na. and K.. HCO. is found to be a major anion followed by Cl. and?SO.. The scatter diagram between (Ca.?+?Mg.) versus Tz. for groundwater shows a

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CUB

V. V. Suresh Babu,M. N. Palgunacharir contains Fe(II) in the range of 0.11–0.15?mg/L. However, the F. in the groundwater varies in the range of 0.5–2.5?mg/L while filtered water contains F. in the range of 0.8–2.4?mg/L (much above the permissible limit of 1.0?mg/L). The filter unit is effective in removing Fe(II) but it fails to remov

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FLAIL

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Tempor

Peptides as Probes in Muscle Researchned by correlation analysis showed that the overall trend of rainfall in the Sina basin is increasing. Also, the results exhibited that the 2–year moving average of the annual rainfall of different stations was showing the best correlation with groundwater level in the study area.

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Joseph C. Kappel,Yi C. Fan,Kit S. Lamd residue. The results are reported in terms of diffusion coefficients (D.) and Leachability Index (L). Both parameters were determined by penetration theory. A smaller diffusion coefficient and a larger leachability index are desired for good solidification. The amount of arsenic leached through th

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