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dc.contributor.authorFrittont, Daniel
dc.contributor.authorOlson, Gerald
dc.date.accessioned2006-12-21T18:24:20Z
dc.date.available2006-12-21T18:24:20Z
dc.date.issued1972-03
dc.identifier.urihttps://hdl.handle.net/1813/4045
dc.description.abstractWhen a pit is dug in soil, it commonly happens that at a certain depth, water seeps from the soil to form a shallow pool at the bottom; at this point, the pit is said to have reached the water table. When the pit is dug below this point, the water surface in it will equilibrate to the water table level. Soil below this level will be saturated and the water under pressure. Above this level, the soil will be unsaturated and the water under tension.en_US
dc.format.extent3173271 bytes
dc.format.mimetypeapplication/pdf
dc.language.isoen_USen_US
dc.publisherNew York State Agricultural Experiment Stationen_US
dc.relation.ispartofseriesNew York's Food and Life Sciences Bulletinen_US
dc.relation.ispartofseries13en_US
dc.subjectNew York Soilen_US
dc.subjectwater table depthen_US
dc.titleDepth to the Apparent Water Table in 17 New York Soils from 1963 to 1970en_US
dc.typeperiodicalen_US


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  • Food and Life Sciences Bulletin
    New York's Food and Life Sciences (FLS) Bulletin reports new developments in fruit and vegetable breeding, performance, diseases, and integrated pest management. It is of interest to researchers and the public.

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