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Assessment of soil salinity problems in agricultural areas through spatial and temporal remote sensing.

机译:通过时空遥感评估农业地区的土壤盐分问题。

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摘要

This study is aimed at addressing the capability of using remote sensing data in detecting and tracking soil salinization variability using a series of experimental methodologies. In a controlled experiment, the spectral reflectance changes associated with salt crust formation on soil surfaces were tracked in order to detect the optimum moisture levels for salinity detection and recognize the influence of soil texture on salinity-induced spectral changes. In another experiment, lettuce plants were utilized to assess plant biophysical responses to moderate salinity levels with canopy-level reflectance data. An FR-ASD spectrometer was used to collect reflectance data in the 400-2500 nm spectral region. Finally, MODIS satellite data were employed to analyze the temporal profiles of selected high (8-11 dS/m), moderate (4-6 dS/m) and none (1-3 dS/m), salt affected sites in the Nile Delta, Egypt. The analyses of spectral data revealed that the use of remote sensing data to discriminate salinity levels in soils is highly affected by moisture content and texture. At low moisture contents, salts have high reflectance in the VIS-NIR spectral region but low reflectance in SWIR region. Spectral ambiguity with soil salinity was found across soil texture types.; Significant relationships were found between plant chlorophyll content and the REP index (R2 = 0.97), and dry biomass with SAVI values (R2 = 0.94) under different salinity treatments. The spectral vegetation indices (VI's), SAVI and REP, and water indices (WI's) were found to be effective in discriminating between plants growing under moderate conditions of soil salinity and a non-saline condition. The combination between VI's and WI's was found to be useful in improving the ability to assess salinity stressed plants from non-stressed plants. Finally, MODIS results showed separability between canopy seasonal growth under high saline (HS) and non-saline (NS) conditions based on phenology. Canopies growing under HS conditions had lower VI and WI values in the green-up period. It may be concluded that using plant biophysical response to detect soil salinity could be useful in detecting early stages of salinity. Also using the combination between VI's and WI's using MODIS data is a useful to discern between high saline and none saline areas.
机译:这项研究旨在通过一系列实验方法来解决利用遥感数据检测和追踪土壤盐渍化变异性的能力。在一个对照实验中,跟踪与土壤表面盐结皮形成有关的光谱反射率变化,以便检测盐度检测的最佳水分含量,并识别土壤质地对盐度引起的光谱变化的影响。在另一个实验中,将生菜植物用于利用冠层水平的反射率数据评估植物对中等盐度水平的生物物理响应。使用FR-ASD光谱仪收集400-2500 nm光谱范围内的反射率数据。最后,利用MODIS卫星数据分析了尼罗河中选定的高(8-11 dS / m),中度(4-6 dS / m)和无(1-3 dS / m)受盐影响的地点的时间剖面埃及三角洲。对光谱数据的分析表明,使用遥感数据区分土壤中的盐度水平受水分含量和质地的影响很大。在低水分含量下,盐在VIS-NIR光谱区域具有高反射率,而在SWIR区域具有低反射率。在土壤质地类型之间发现光谱含盐度不明确。在不同盐度处理下,植物叶绿素含量与REP指数(R2 = 0.97)和具有SAVI值的干燥生物量(R2 = 0.94)之间存在显着关系。发现光谱植被指数(VI's),SAVI和REP以及水分指数(WI's)可有效地区分在中等盐度和非盐度条件下生长的植物。发现VI和WI之间的组合对于提高评估来自非胁迫植物的盐度胁迫植物的能力是有用的。最后,MODIS结果表明,基于物候学,高盐(HS)和非盐(NS)条件下的冠层季节性生长具有可分离性。在绿化时期,在HS条件下生长的冠层具有较低的VI和WI值。可以得出结论,利用植物的生物物理反应来检测土壤盐度可能有助于检测盐度的早期阶段。同样,使用MODIS数据结合使用VI和WI之间的组合,有助于区分高盐和无盐区域。

著录项

  • 作者单位

    The University of Arizona.;

  • 授予单位 The University of Arizona.;
  • 学科 Agriculture Soil Science.; Remote Sensing.
  • 学位 Ph.D.
  • 年度 2005
  • 页码 147 p.
  • 总页数 147
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 土壤学;遥感技术;
  • 关键词

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