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首页> 外文期刊>Journal of the American Water Resources Association >REAL-TIME SOIL WATER MONITORING FOR OPTIMUM WATER MANAGEMENT
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REAL-TIME SOIL WATER MONITORING FOR OPTIMUM WATER MANAGEMENT

机译:实时土壤水监测,实现最佳水管理

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Efficient water resource management is one of the most important policy issues facing agriculture in Hawaii in the years ahead. Soil water sensors, multisensor capacitance probes (MCP), have been successfully used for different water management projects. These MCPs monitor water content at multiple depths and at various locations in real-time. The objectives of this study were to determine the effect of water content on field soil bulk density of Wahiawa silty clay tropical soil; measure field saturated hydraulic conductivity of this tropical soil; calibrate MCP system for this soil; and monitor and evaluate real-time soil water content variations under a tomato crop using the calibrated MCP system. Sensor calibration was conducted under laboratory conditions. Soil bulk density at different water contents and saturated hydraulic conductivity were measured on the field. Bulk density increased with increasing water content; there was a 30 percent bulk density increase as a result of 0.25 cm~3 cm~(-3) water content variation. Compared with the manufacturer's calibration, site specific laboratory calibration of MCP gave a more accurate determination of soil water. Field determined saturated hydraulic conductivity was higher than laboratory determined values reported in the literature for the same soil type. Real-time soil water content monitoring within the root zone showed substantial variations due to water input (irrigation and rainfall) and water output (evapo-transpiration and deep percolations). However, water content variations were much further reduced in the soil layer below the root zone.
机译:高效的水资源管理是未来几年夏威夷农业面临的最重要的政策问题之一。土壤水传感器,多传感器电容式探针(MCP)已成功用于不同的水管理项目。这些MCP实时监控多个深度和各个位置的水含量。本研究的目的是确定含水量对Wahiawa粉质粘土热带土壤田间土壤容重的影响。测量该热带土壤的田间饱和导水率;校准该土壤的MCP系统;并使用校准后的MCP系统监测和评估番茄作物下的实时土壤水分含量变化。传感器校准是在实验室条件下进行的。在野外测量了不同含水量和饱和导水率下的土壤容重。堆积密度随含水量的增加而增加;由于水分含量变化0.25 cm〜3 cm〜(-3),堆密度增加了30%。与制造商的校准相比,MCP的现场特定实验室校准可以更准确地确定土壤水。现场测定的饱和导水率高于文献报道的相同土壤类型的实验室测定值。根部区域内的实时土壤水分含量监测显示,由于输入水(灌溉和降雨)和输出水(蒸发蒸腾和深层渗滤)而产生了很大的差异。但是,根区以下的土壤层中的水含量变化大大减少了。

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