نتایج جستجو برای: soil hydrology processes

تعداد نتایج: 702444  

1998
S. Newman J. Schuette J. B. Grace K. Rutchey T. Fontaine K. R. Reddy M. Pietrucha

Since the early 1900s, the Everglades have been influenced by anthropogenic actions including altered hydrology and increased nutrient loading. In the northern Everglades an apparent effect of Ž . these disturbances has been the development and proliferation of dense cattail Typha spp. stands Ž . in areas previously dominated by sawgrass Cladium jamaicense Crantz and sloughs. Cattail cover, soi...

2014
Karen S. Harpp Eric Mittelstaedt Noémi d’Ozouville Anne J. Jefferson Ken L. Ferrier Ricardo Ramalho

Volcanic ocean islands and shield volcanoes form superb natural experiments for investigating changes in topography and hydrology over geologic time. As volcanoes age, their surfaces evolve from un-dissected, highpermeability landscapes into deeply dissected, low-permeability terrain. Here we review the tight links and co-evolution of topographic and hydrologic processes in volcanic landscapes....

2009
M. van der Laan

M. van der Laan1, J.G. Annandale1*, C.C. du Preez2 and S.A. Lorentz3 1 Department of Plant Production and Soil Science, University of Pretoria, Pretoria 0002, South Africa 2Department of Soil, Crop and Climate Sciences, University of the Free State, Bloemfontein 9300, South Africa 3School of Bioresources Engineering and Environmental Hydrology, University of KwaZulu-Natal, Pietermaritzburg 3209...

2016
Ying Zhao Bingcheng Si Hailong He Jinghui Xu Stephan Peth Rainer Horn Jun Xu

Accurate simulation of soil water and heat transfer is critical to understand surface hydrology under cold conditions. Using an extended freezing code in HYDRUS-1D (freezing module), this study was conducted: (1) to evaluate the freezing module using field data collected in a grazed steppe of Inner Mongolia; and (2) to further simulate grazing effects on frozen soil hydrological processes. The ...

2010
M. Musgrove

0022-1694/$ see front matter Published by Elsevier doi:10.1016/j.jhydrol.2010.04.036 * Corresponding author at: US Geological Survey, 1505 Ferguson Lane, Austin, TX 78754, United States. E-mail address: [email protected] (M. Musgrov A two and a half year study of two adjacent watersheds at the Honey Creek State Natural Area (HCSNA) in central Texas was undertaken to evaluate spatial and tempora...

2006
M. Rogora

Papers published in Hydrology and Earth System Sciences Discussions are under open-access review for the journal Hydrology and Earth System Sciences Abstract The role of meteorology, hydrology and atmospheric deposition on the temporal pattern of SO 4 and NO 3 concentrations was investigated for three streams draining alpine catchments in Northern Italy. The study sites lie on a gradient of atm...

دستورانی, محمد تقی, رنگ آور, عبد الصالح, طالبی, علی, فعله گری, محسن,

Computer simulation models are increasingly popular for predicting soil loss to quantify the processes of detachment, transport and deposition of eroded soils. To assess the effects of different management on soil erosion, selecting the best models and their validation a positive step is considered. In this research the Rangeland Hydrology and Erosion Model (RHEM) was evaluated by using soil er...

2015
Randy Kolka Scott D. Bridgham Chien-Lu Ping

Peatlands are a subset of wetlands that have accumulated significant amounts of soil organic matter. Soils of peatlands are colloquially known as peat, with mucks referring to peats that are decomposed to the point that the original plant remains are altered beyond recognition (Chapter 6, SSSA 2008). Generally, soils with a surface organic layer >40 cm thick have been classified as Histosols in...

2011
P. V. Caldwell M. J. Vepraskas J. D. Gregory R. W. Skaggs R. L. Huffman

Although millions of dollars are spent restoring wetlands, failures are common, in part because the planted vegetation cannot survive in the restored hydrology. Wetland restoration would be more successful if the hydrologic requirements of wetland plant communities were known so that the most appropriate plants could be selected for the range of projected hydrology at the site. Here we describe...

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