By Edward M Gosschalk
Reservoir Engineering: directions for Practice offers the authors recommendations and information on reservoir engineering practice.
This unheard of new advisor presents authoritative info on reservoir engineering world-wide and may be a useful source for these meaning to carry or really maintaining senior point accountability within the box of reservoir engineering. Reservoir Engineering: directions for Practice also will offer scholars and academics with hugely informative suggestions and references.
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Additional resources for Reservoir Engineering: Guidelines for Practice
Sample text
Depending on transport facilities, alternative modes of travel to the site by mule, foot, vehicle and boat, etc. are all possibilities in use. In somewhat unexplored country, video photography from a helicopter can be very helpful Ð for example when travelling up river to obtain a continuous scan of the changing topography. The reconnaissance `team' might possibly be just one person Ð the chief experienced reservoir or project civil engineer. Ideally, however, the smallest team desirable would include the chief engineer accompanied by the experienced engineering geologist and the hydrologist.
Topographical data in the form of maps and aerial photographs (in stereo pairs if available) . geological data in the form of maps and the results of drilling and testing in the project area . data on historic seismic activity in the region . meteorological and hydrological data Ð what records are available of parameters such as rainfall, atmospheric and water temperatures, evaporation, humidity, wind speeds, hours of sunshine, river ¯ows and/or river levels, and sediment transport, and over what periods are the records of each parameter available?
G. 6 Â average annual runo is required (on average) to provide a continuous yield equal to the monthly average in¯ow to the average in¯ow) over the period of record (assuming no spill to waste during ¯oods) is represented by the greatest height above the in¯ow curve at any point of a horizontal discharge line which is tangent to the highest crest of the in¯ow curve (a line a little bit lower than the average in¯ow line shown on Fig. 4(b)). Note that `out¯ow' must include losses due to waste, leakage and evaporation.