Physical and hydraulic properties of inorganic amendments and modeling their effects on water movement in sand-based root zones

被引:0
|
作者
Leonard J. M. Githinji
Jacob H. Dane
Robert H. Walker
机构
[1] Tuskegee University,Environmental and Natural Resource, Department of Agricultural and Environmental Sciences
[2] Auburn University,Department of Agronomy and Soils
来源
Irrigation Science | 2011年 / 29卷
关键词
Root Zone; Diatomaceous Earth; Hydraulic Property; Volumetric Water Content; Saturated Hydraulic Conductivity;
D O I
暂无
中图分类号
学科分类号
摘要
The objective of this study was to evaluate the physical and hydraulic properties of selected inorganic amendments and their mixtures with sand (85:15% v/v), and model how they affect the water movement in sand-based root zones of sports fields. The amendments are composed of: calcined diatomaceous earth materials (Axis and Isolite); zeolites (Clinolite and Ecolite); and calcined clays (Moltan Plus, Profile, and Pro’s Choice). The bulk density, particle density, porosity, particle-size distribution, saturated hydraulic conductivity, water retention and available water-holding capacity were analyzed. A numerical model was applied to simulate soil water movement for a scenario with and without amendment incorporation. The results showed that amendments significantly (P < 0.05) improved the physical and hydraulic properties of root zone. Modeling results revealed reduced surface dryness, higher volumetric water content and storage and higher initial root water uptake rate for the root zones with amendments. These results suggest there are multiple benefits of amended root zones in terms of improvement of the physical and hydraulic properties of sand-based root zones.
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页码:65 / 77
页数:12
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