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DEGRADATION OF AN ARID ENVIRONMENT: EARTH FISSURES IN CENTRAL ARIZONA.

机译:干旱环境的退化:中央亚利桑那州的地球裂缝。

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摘要

The surficial desertification and degradation characteristics of major elements of the natural environment (vegetation, drainage, and morphology) associated with the development of earth fissures were investigated. Three appropriate fissure sites within a general study area located southeast of Phoenix, Arizona were carefully selected to minimize cultural influences.; Data for analysis were collected from satellite imagery and aerial photography, and from ground level surveys. Traditional remote sensing analysis techniques were employed to identify degradational characteristics which appear on the various remotely-sensed data bases. Remote sensing techniques were incorporated into the investigation to provide an overall, comprehensive view to enhance the spatial arrangement of anomalies suggestive of degradational characteristics. On-site data collection involved taking calculated transects across the various fissures to provide micro-scale information suggestive of degradational characteristics. These ground surveys involved the collection of physical measurements of individual fissures; apparent plant stress information; gross thermal characteristics; erosional characteristics and anomalies; and apparent surficial changes in the natural drainage, morphology, and vegetation.; The results of analysis indicate that the occurrence of true desertification does not exist, but that degradation clearly exists, primarily in the form of erosion, and is the result of earth fissure development. Erosion was found to occur in two ways: that which is commonplace beginning at fissures and migrating up-slope, and that which washes soil from around plant roots. In addition, minor selective changes in the vegetation, drainage, and morphology were clearly identified and proven to be the result of earth fissure development. It is concluded that erosion can not be effectively halted and, as a result, will spread widely resulting eventually in desertification.
机译:研究了与裂隙发展有关的自然环境主要要素(植被,排水和形态)的表面荒漠化和退化特征。精心选择了位于亚利桑那州凤凰城东南部的一个普通研究区内的三个裂隙部位,以最大程度地减少文化影响。用于分析的数据是从卫星图像和航空摄影以及地面调查中收集的。传统的遥感分析技术被用来识别出现在各种遥感数据库上的退化特征。遥感技术被纳入调查,以提供一个整体的,全面的视图,以增强暗示退化特征的异常的空间排列。现场数据收集涉及跨各种裂缝采取计算的样条,以提供暗示降解特性的微观信息。这些地面调查涉及对单个裂缝的物理测量的收集。表观植物胁迫信息;总热特性;侵蚀特征和异常;自然排水,形态和植被的表观变化。分析结果表明,不存在真正的荒漠化,但明显存在退化,主要是以侵蚀的形式存在,这是地球裂缝发展的结果。人们发现侵蚀发生的方式有两种:一种是常见的现象,它始于裂隙并向上迁移,另一种是从植物根部周围冲洗土壤。此外,清楚地确定了植被,排水系统和形态的微小选择性变化,并被证明是地球裂缝发展的结果。结论是,不能有效地制止侵蚀,结果,侵蚀将广泛传播,最终导致荒漠化。

著录项

  • 作者

    ALGER, LEONARD HUGH, JR.;

  • 作者单位

    Indiana State University.;

  • 授予单位 Indiana State University.;
  • 学科 Physical Geography.; Geological Survey.; Remote Sensing.
  • 学位 Ph.D.
  • 年度 1982
  • 页码 115 p.
  • 总页数 115
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 自然地理学;遥感技术;
  • 关键词

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