Spelling suggestions: "subject:"soil -- moisture"" "subject:"soil -- amoisture""
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Studies in Soils Structure VI. Water Bound by Individual Soil Constituents as Influenced by PuddlingBuehrer, T. F., Aldrich, D. G. Jr. 06 1900 (has links)
This item was digitized as part of the Million Books Project led by Carnegie Mellon University and supported by grants from the National Science Foundation (NSF). Cornell University coordinated the participation of land-grant and agricultural libraries in providing historical agricultural information for the digitization project; the University of Arizona Libraries, the College of Agriculture and Life Sciences, and the Office of Arid Lands Studies collaborated in the selection and provision of material for the digitization project.
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The use of remote sensing and other system state estimates in the calibration of a distributed hydrological modelFisher, James I. January 1995 (has links)
No description available.
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SOIL MOISTURE UNIFORMITY IN AN IRRIGATED FIELD.Santos, Francisco Lucio dos Reis Borges Brito dos. January 1985 (has links)
No description available.
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The hydrology of a restored coastal dune slack, St. Fergus, north-east Scotland : an integrated field and modelling approachMalcolm, Robert January 1998 (has links)
This thesis examines the hydrological processes of a restored coastal dune slack at St. Fergus, north-east Scotland. The fundamental hydrological processes of the saturated and unsaturated zones of these habitats is relatively poorly understood yet these ecosystems are under increasing pressure from industrial and recreational development and the possible impact of climate change. Within a 1.2km<sup>2</sup> catchment, a detailed field investigation was initiated at differing spatial scales to examine; (i) the spatial and temporal variability in soil moisture retention and movement through the unsaturated zone; (ii) the behaviour of the water table and; (iii) the main hydrogeochemical processes over the year October 1996 to September 1997. The field research was augmented with the development of a groundwater flow model of the site which was used in a predictive role to examine the possible implications of future climate change on the groundwater regime of the dune slack and the impact of this on the ecology and geomorphology of the dune system. The field and modelling results were integrated to provide a relatively holistic interpretation of the hydrological processes of the dune slack system. The soils of all study sites were relatively similar in their retention and temporal variability of soil moisture over the year. Soil moisture contents were generally very low, which was predominantly related to the low organic matter content and highly porous sediment. These soil properties resulted in great temporal variability in soil moisture content over the year with no pattern of higher retention in the winter and lower in the summer. Groundwater behaviour was also relatively homogeneous in the catchment, though local scale, transient processes and phenomena appeared to be important. The main influences on groundwater levels and direction of flow included; (i) the groundwater recharge processes (influenced by variable specific yield phenomena, preferential flow paths and the height of the capillary fringe); (ii) the hydrogeology of the site, particularly the complex plateau region; (iii) site topography; (iv) the shallow water table and; (v) terminal encroachment on to the dune slack. The modelling procedure highlighted the need for an integrated field and modelling approach as problems encountered were resolved through interpretation of the field data. Issues raised focused on scale and scaling in groundwater modelling, the validation of such models and the importance of good spatially distributed field data.
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Soil water regime, root water extraction and the growth of fine roots of Sitka SpruceEvans, Douglas January 1988 (has links)
The effect of removing soil water stress on fine root growth and the pattern of water use was studied by irrigating a small plot (20 m x 20 m) of 40 year old Sitka spruce. A control plot was established close by. Soil water content and soil matric potential were measured independently on both plots at several depths. Root growth was measured using monthly coring for the surface horizons (c. 10 cm depth) and ingrowth cores to study rooting at depth. In the absence of irrigation the 2 plots had similar water regimes. The irrigation kept matric potential > 20 kPa and water content > 20%. Areas between trees were wetter than areas close to stems and wetted up more during periods of rainfall. This is in contrast to young plantations where stemflow accounts for a much larger proportion of precipitation reaching the forest floor. At field capacity most of the water uptake was from near the surface but as the profile dries the proportion from depth increases, at the end of a dry period 50% of uptake was from the bottom half of the rooted zone. Water uptake from below the rooted zone was small. Irrigation had a significant effect on root tip density and on small root mass but not on fine and dead root masses. Root tip density stayed high through the summer with irrigation but fell on the control plot, the number of tips began to increase earlier on the control plot. This is interpreted as irrigation increasing the longevity of tips from 2-3 months (control) to 5 months. Rewetting of the soil in autumn appears to act as a cue for an increase in root growth. Irrigation had no effect on root growth at depth and there was no difference in growth at different depths on either plot.
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A study of the combined effect of soil moisture and seasonal rainfall upon wheat yields on western Kansas farmsCompton, Laurence Larue January 1940 (has links)
No description available.
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The influence of a waterproofing agent on soil moisture propertiesBowers, Sidney Allen. January 1958 (has links)
Call number: LD2668 .T4 1958 B69 / Master of Science
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Predicting soil moisture and wheat vegetative growth from ERTS-1 imageryKrupp, John Wayne January 2011 (has links)
Digitized by Kansas Correctional Industries
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Soil moisture modeling and scaling using passive microwave remote sensingDas, Narendra N. 25 April 2007 (has links)
Soil moisture in the shallow subsurface is a primary hydrologic state governing
land-atmosphere interaction at various scales. The primary objectives of this study are to
model soil moisture in the root zone in a distributed manner and determine scaling
properties of surface soil moisture using passive microwave remote sensing. The study
was divided into two parts. For the first study, a root zone soil moisture assessment tool
(SMAT) was developed in the ArcGIS platform by fully integrating a one-dimensional
vadose zone hydrology model (HYDRUS-ET) with an ensemble Kalman filter (EnKF)
data assimilation capability. The tool was tested with dataset from the Southern Great
Plain 1997 (SGP97) hydrology remote sensing experiment. Results demonstrated that
SMAT displayed a reasonable capability to generate soil moisture distribution at the
desired resolution at various depths of the root zone in Little Washita watershed during
the SGP97 hydrology remote sensing experiment. To improve the model performance,
several outstanding issues need to be addressed in the future by: including "effective"
hydraulic parameters across spatial scales; implementing subsurface soil properties data
bases using direct and indirect methods; incorporating appropriate hydrologic processes across spatial scales; accounting uncertainties in forcing data; and preserving
interactions for spatially correlated pixels.
The second study focused on spatial scaling properties of the Polarimetric
Scanning Radiometer (PSR)-based remotely sensed surface soil moisture fields in a
region with high row crop agriculture. A wavelet based multi-resolution technique was
used to decompose the soil moisture fields into larger-scale average soil moisture fields
and fluctuations in horizontal, diagonal and vertical directions at various resolutions. The
specific objective was to relate soil moisture variability at the scale of the PSR footprint
(800 m X 800 m) to larger scale average soil moisture field variability. We also
investigated the scaling characteristics of fluctuation fields among various resolutions.
The spatial structure of soil moisture exhibited linearity in the log-log dependency of the
variance versus scale-factor, up to a scale factor of -2.6 (6100 m X 6100 m) irrespective
of wet and dry conditions, whereas dry fields reflect nonlinear (multi-scaling) behavior
at larger scale-factors.
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Soil moisture and soil water solutes during freeze-back at Lake Levinson-Lessing, Taymyr Peninsula, SiberiaOverduin, P. P. January 1997 (has links)
Thesis (M. Sc.)--York University, 1997. / Typescript. Includes bibliographical references (leaves 104-113). Also available on the Internet. MODE OF ACCESS via web browser by entering the following URL: http://wwwlib.umi.com/cr/yorku/fullcit?pMQ27369.
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