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Finite element modelling and its calibrations as applied to the prediction of groundwater table movements何嘉彥, Ho, Kar-yin. January 1982 (has links)
published_or_final_version / Civil Engineering / Master / Master of Philosophy
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WELLS IMAGED ABOUT AN INTERFACE: A SAND MODELSouissi, Abderrazak January 1984 (has links)
No description available.
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Water table distributions in a sandy soil with subirrigationGallichand, Jacques. January 1983 (has links)
No description available.
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Analyse de l'efficacite de deux reseaux de drainage souterrain de la region de Nicolet.Asselin, Rémi, 1948- January 1980 (has links)
No description available.
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Soil water balance of intercropped corn under water table managementQureshi, Suhail Ahmad January 1995 (has links)
A one year water table management field study was conducted on a Soulanges sandy loam soil in Soulanges county, Quebec. Two controlled water table levels, i.e. 0.5 m and 0.75 m from the soil surface, as well as free outlet conventional drainage treatments were established in monocropped corn (Zea mays L.) and corn intercropped with ryegrass (Lolium multiflorum Lam) plots. / Cropping system showed no significant effects on evapotranspiration, and on soil moisture distribution. It was observed that the 0.5 m and 0.75 m controlled water tables (CWT) provided the same soil moisture trends in both cropping systems. The soil moisture was always higher in controlled water table plots compared to freely drained plots. The water use efficiency of 0.75 m CWT in both cropping systems was high compared to 0.5 m CWT. / The soil moisture contents at three depths were only 2% to 10% less in intercropped plots compared to monocropped plots. The soil moisture was 12 to 13% higher in CWT plots compared to freely drained plots for both cropping systems. The soil moisture in 0.5 m CWT and 0.75 m CWT plots was not significantly different. The average water table levels in monocropped plots were not significantly different from intercropped plots.
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Soil morphology and potentiometric surface relationship in an East Central Indiana toposequenceO'Brien, Eugene M. January 2000 (has links)
The objective of this study was to determine the correlation between potentiometric surface and the depth to selected soil morphological indicators of wetness for the Glynwood (Aquic Hapludalf), Blount (Aeric Epiaqulaf), and Pewamo (Typic Argiaguoll) soils in Delaware County, Indiana. Four years of potentiometric surface measurements were averaged and compared to detailed soil descriptions performed by the Natural Resources Conservation Service. Significant correlations exist between the morphological indicators and the potentiometric surface for the Glynwood (moderately well drained) 2-m depth piezometers and 2-m depth slotted pipes, the Blount (somewhat poorly drained) top of the C horizon and 2-m depth piezometers, and the Pewamo (poorly drained) top of the B horizon piezometers. The relationships among the horizons in which potentiometric surface correlated to indicator depth may be a function of the increased persistence and shallowness of the potentiometric surface in mid-April. / Department of Natural Resources and Environmental Management
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Water table management strategies for soybean productionBroughton, Stephen R. (Stephen Russell) January 1992 (has links)
A field lysimeter experiment was conducted on a sandy loam soil during the growing seasons of 1989 and 1990. The experiment tested the effects of four water table treatments on soybean (Glycine max) yields. The water table depths were 40, 60, 80, and 100 cm in depth. / Yields were measured in terms of: total seed mass per plant, number of seeds per plant, number of pods per plant, number of seeds per pod, and speed protein content at harvest. / The water management simulation model DRAINMOD, was used to develop irrigation and drainage strategies for soybean production. Three water table management methods were tested with each of three water table depths. The methods were conventional drainage, controlled drainage, and subirrigation, and the water table depths were 40, 60, 80, and 100 cm. / It was shown that for the driest year highest yields are obtained with subsurface irrigation and a weir setting of 40 cm. For the average year, highest yields are obtained with subirrigation and a 60 cm weir setting. For the wet years, best results are found when controlled drainage is used with 80 cm weir setting. It was found that in all but the driest and wettest years controlled drainage improved yields by 10% or more.
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Numerical simulation of groundwater withdrawal within the Mercury Valley Hydrographic Area, NevadaGilliam, Anna Brooke. January 2004 (has links)
Thesis (M.S.)--University of Nevada, Reno, 2004. / "December, 2004." Includes bibliographical references (leaves 79-83). Online version available on the World Wide Web.
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Hydromorphology and plinthite characterization of some Alabama coastalplains soilsSmith, Richard Carter Shaw, Joey N. January 2007 (has links) (PDF)
Thesis(M.S.)--Auburn University, 2007. / Abstract. Vita. Includes bibliographic references.
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Integrated mass, solute, isotopic and thermal balances of a coastal wetland /Rich, J. F. January 2004 (has links)
Thesis (Ph.D.) --Murdoch University, 2004. / Thesis submitted to the Division of Science and Engineering. Includes bibliographical references (leaves R-1 - R-24). Also available via the World Wide Web at.
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