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A dense network of cosmic-ray neutron sensors for soil moisture observation in a highly instrumented pre-Alpine headwater catchment in Germany

机译:德国高度仪表预高山壁盆地区的土壤水分观测宇宙射线中子传感器密集网络

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Monitoring soil moisture is still a challenge: it varies strongly in space and time and at various scales while conventional sensors typically suffer from small spatial support. With a sensor footprint up to several hectares, cosmic-ray neutron sensing (CRNS) is a modern technology to address that challenge. So far, the CRNS method has typically been applied with single sensors or in sparse national-scale networks. This study presents, for the first time, a dense network of 24 CRNS stations that covered, from May to July 2019, an area of just 1 km2: the pre-Alpine Rott headwater catchment in Southern Germany, which is characterized by strong soil moisture gradients in a heterogeneous landscape with forests and grasslands. With substantially overlapping sensor footprints, this network was designed to study root-zone soil moisture dynamics at the catchment scale. The observations of the dense CRNS network were complemented by extensive measurements that allow users to study soil moisture variability at various spatial scales: roving (mobile) CRNS units, remotely sensed thermal images from unmanned areal systems (UASs), permanent and temporary wireless sensor networks, profile probes, and comprehensive manual soil sampling. Since neutron counts are also affected by hydrogen pools other than soil moisture, vegetation biomass was monitored in forest and grassland patches, as well as meteorological variables; discharge and groundwater tables were recorded to support hydrological modeling experiments. As a result, we provide a unique and comprehensive data set to several research communities: to those who investigate the retrieval of soil moisture from cosmic-ray neutron sensing, to those who study the variability of soil moisture at different spatiotemporal scales, and to those who intend to better understand the role of root-zone soil moisture dynamics in the context of catchment and groundwater hydrology, as well as land–atmosphere exchange processes. The data set is available through the EUDAT Collaborative Data Infrastructure and is split into two subsets: https://doi.org/10.23728/b2share.282675586fb94f44ab2fd09da0856883 (Fersch et?al.,?2020a) and https://doi.org/10.23728/b2share.bd89f066c26a4507ad654e994153358b (Fersch et?al.,?2020b).
机译:监测土壤水分仍然是一个挑战:它在空间和时间和时间强烈地变化,而在各种尺度上,而传统传感器通常遭受小的空间支撑。通过传感器占地面积,高达几公顷,宇宙射线中子传感(CRNS)是一种解决这一挑战的现代技术。到目前为止,CRNS方法通常已用单个传感器或稀疏的国家级网络应用。这项研究表明,从5月到2019年7月,覆盖的24个CRNS站的密集网络是一个只有1平方公里的地区:德国南部的高山罗特伐木艇集水区,其特点是土壤水分强大在异质景观的梯度与森林和草原。通过大致重叠的传感器占用脚印,该网络旨在在集水区尺度上研究根区土壤水分动力学。密集CRNS网络的观察通过广泛的测量辅成,允许用户在各种空间尺度上研究土壤湿度可变性:罗瓦(移动)CRNS单元,来自无人的区域(uass),永久和临时无线传感器网络的远程感测的热图像,概况探头和综合手动土壤采样。由于中子计数也受土壤水分以外的氢气的影响,因此在森林和草原斑块以及气象变量中监测植被生物量;记录放电和地下水表以支持水文建模实验。因此,我们为几个研究社区提供了一个独特而综合的数据:那些调查从宇宙射线中子传感的土壤水分检索的人,对那些在不同的时空鳞片上研究土壤水分变异的人,以及那些谁打算更好地了解根部区域土壤水分动力学在集水区和地下水水文的背景下的作用,以及土地 - 大气交换过程。数据集可通过eudat协作数据基础架构获得,并分为两个子集:https://doi.org/10.23728/b2舍尔282675586fb94f44ab2fd09da0856883(fersch et?al。,?2020a)和https://doi.org/ 10.23728 / B2Share.BD89F066C26A4507AD654E994153358B(FERSCH et?al。,?2020b)。

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