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Relationships between vegetation indices and root zone soil moisture under maize and soybean canopies in the US Corn Belt: a comparative study using a close-range sensing approach

机译:美国玉米带玉米和大豆冠层下植被指数与根区土壤水分之间的关​​系:使用近距离传感方法的比较研究

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摘要

Understanding the relationships between root zone soil moisture and vegetation spectral signals will enhance our ability to manage water resources and monitor drought-related stress in vegetation. In this article, the relationships between vegetation indices (VIs) and in situ soil moisture under maize and soybean canopies were analysed using close-range reflectance data acquired at a rainfed cropland site in the US Corn Belt. Because of the deep rooting depths of maize plants, maize-based VIs exhibited significant correlations with soil moisture at a depth of 100 cm (P < 0.01) and kept soil moisture memory for a long period of time (45 days). Among the VIs applied to maize, the chrolophyll red-edge index (CI_(red-edge)) correlated best with the concurrent soil moisture at 100 cm depth (P < 0.01) for up to 20 day lag periods. The same index showed a significant correlation with soil moisture at a 50 cm depth for lag periods from 10 (P < 0.05) to 60 days (P < 0.01). VIs applied to soybean resulted in statistically significant correlations with soil moisture at the shallower 10 and 25 cm depths, and the correlation coefficients declined with increasing depths. As opposed to maize, soybean held a shorter soil moisture memory as the correlations for all VIs versus soil moisture at 10 cm depth were strongest for the 5 day lag period. Wide dynamic range VI and normalized difference VI performed better in characterizing soil moisture at the 10 and 25 cm depths under soybean canopies when compared with enhanced VI and CI_(red-edge).
机译:了解根区土壤水分与植被光谱信号之间的关系将增强我们管理水资源和监测植被中与干旱相关的压力的能力。在本文中,使用在美国玉米带雨养农田站点获得的近距离反射数据,分析了玉米和大豆冠层下植被指数(VIs)与原位土壤水分之间的关​​系。由于玉米植株的生根深度较深,因此基于玉米的VI在100 cm的深度处表现出与土壤水分的显着相关性(P <0.01),并能长期保持土壤水分记忆(45天)。在用于玉米的VI中,叶绿素红边指数(CI_(red-edge))与100 cm深度上同时存在的土壤水分(P <0.01)的相关性最高,长达20天的滞后时间。相同的指标显示,在10厘米(P <0.05)至60天(P <0.01)的滞后时间内,深度为50 cm的土壤水分与土壤湿度显着相关。应用于大豆的VIs在较浅的10和25 cm深度处与土壤水分具有统计学上的显着相关性,并且相关系数随深度的增加而降低。与玉米相反,大豆保持较短的土壤水分记忆,因为在5天的滞后时间内,所有VI与10 cm深度土壤水分的相关性最强。与增强的VI和CI_(红边)相比,宽动态范围VI和归一化差异VI在表征大豆冠层下10和25 cm深度的土壤水分方面表现更好。

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  • 来源
    《International journal of remote sensing》 |2013年第8期|2814-2828|共15页
  • 作者单位

    Center for Advanced Land Management Information Technologies, School of Natural Resources,University of Nebraska, Lincoln, NE 68583-0973, USA National Drought Mitigation Center,School of Natural Resources, University of Nebraska, Lincoln, NE 68583-0988, USA;

    Center for Advanced Land Management Information Technologies, School of Natural Resources,University of Nebraska, Lincoln, NE 68583-0973, USA National Drought Mitigation Center,School of Natural Resources, University of Nebraska, Lincoln, NE 68583-0988, USA;

    Center for Advanced Land Management Information Technologies, School of Natural Resources,University of Nebraska, Lincoln, NE 68583-0973, USA;

    Center for Advanced Land Management Information Technologies, School of Natural Resources,University of Nebraska, Lincoln, NE 68583-0973, USA;

    National Drought Mitigation Center,School of Natural Resources, University of Nebraska, Lincoln, NE 68583-0988, USA;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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