Basic Environmental Engineering by R.C. Gaur
By R.C. Gaur
The publication covers the hot syllabus of the semester scheme for the 1st yr in R.T.U. and different universities. It encompasses the sensible purposes of the topic, that's the actual want of the hour and in addition discusses the foremost environmental difficulties we are facing this day. It comprises real info supplied via different Manuals ready through The C.P.H.E.E.O. It contains examples of other initiatives and schemes for representation. easy sketches and more straightforward derivations of the mathematical formulations were followed. evaluation questions on the finish of every bankruptcy are given to check the certainty of the reader. the sensible difficulties of box and basic options were correlated via the significant event and deep experience of outrage to the mum earth.
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Additional info for Basic Environmental Engineering
The water that cannot be extracted is known as the specific retention or field capacity. This specific retention is the amount of water held between the grains due to molecular attraction. This film of water is thus held by molecular adhesion on the walls of the intrices. Therefore the amount of this water will depend upon the total interstitial surface in the rock. If the total interstitial surface is more, the specific retention will be more and vice-versa. In soils like clay as the specific area is more, the specific retention would be more and hence it will result in a small specific yield.
A sample of the water entering the distribution system that does not conform to this standard calls for an immediate investigation into both the efficacy of the purification process and the method of sampling. (ii) Water in the distribution system shall satisfy all the three criteria indicated below below:• E. Coli (Escherichia Coli, bacteria found in the colon of human beings as a natural habitant) count in 100 ml of any sample should be zero. • Coliform organisms (group of B- Coli bacteria coli and E.
1 Porosity and Permeability of Some Soils S. No. 5 GROUND WATER YIELD The ground water is present in the water bearing stratum. Those soil formations through which it can be easily and economically extracted is known as aquifers. The top layer of ground water is known as water table. The ground water may come out by itself either through springs or sometimes as artisan wells, but generally extracted out through the wells. Larger diameter wells are known as open wells whereas the smaller diameter wells (30 cm or so) are known as tube-wells.