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In-Situ and Remote Soil Moisture Sensing Technologies for Vadose Zone Hydrology

机译:渗流区水文学的原位和远程土壤湿度传感技术

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摘要

Serious threats to water resources are increasing as the world population is growing and more land is needed to produce food, fiber, and biofuels. Climate change is adding additional uncertainty. It is expected that water scarcity will continue to intensify in arid and semiarid areas and that humid areas will increasingly experience water shortages. The vadose zone plays a key role in many important hydrological processes, such as infiltration, runoff, soil water storage, root water uptake, and groundwater recharge. In managing limited water resources, water managers need a suite of decision support systems and management tools. Vadose zone soil water sensing, through in situ or remote techniques, has been proven extremely useful in this regard. A variety of in situ and remote soil water sensing techniques have been developed, tested, and used with different levels of success over the past decades. Observations using these two major types of soil water sensing methods are for different volumes, andwith different spatial and temporal resolutions.
机译:随着世界人口的增长,对水资源的严重威胁正在增加,并且需要更多的土地来生产食物,纤维和生物燃料。气候变化增加了更多的不确定性。预计干旱和半干旱地区的水资源短缺将继续加剧,而潮湿地区将越来越多地出现缺水现象。渗流带在许多重要的水文过程中起着关键作用,例如渗透,径流,土壤蓄水,根系吸水和地下水补给。在管理有限的水资源时,水管理者需要一套决策支持系统和管理工具。在这方面,已证实通过原位或远程技术对渗流带土壤水进行传感非常有用。在过去的几十年中,已经开发,测试和使用了多种现场和远程土壤水感测技术,并取得了不同程度的成功。使用这两种主要类型的土壤水分感测方法进行的观测是针对不同的体积,以及不同的时空分辨率。

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