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地表微地形测量及定量化方法研究综述
引用本文:朱良君,张光辉.地表微地形测量及定量化方法研究综述[J].中国水土保持科学,2013(5):114-122.
作者姓名:朱良君  张光辉
作者单位:[1]北京师范大学地理学与遥感科学学院,北京100875 [2]中国科学院水利部水土保持研究所,黄土高原土壤侵蚀与旱地农业国家重点实验室,陕西杨凌712100
基金项目:中国科学院“百人计划”择优支持项目“土壤侵蚀水动力学机制研究”(K318001110);国家自然科学基金“输沙对坡面侵蚀的影响及其水动力学机理研究”(41271287)
摘    要:地表微地形测量是地表粗糙度定量化的基础,对地表形态动态监测、水文过程模拟以及土壤侵蚀过程模型的构建具有重要意义。目前,微地形测量方法主要分为接触式和非接触式2大类,前者包括测针法、链条法、差分GPS法等,后者包括超声波测距法、红外线传感器法、结构光激光扫描法、激光测距扫描法、三维激光扫描仪法、近景摄影测量法等。在全面回顾各方法原理、优缺点及其应用的基础上,分析地表粗糙度定量化常用方法:统计方法指数、地统计学指数和分形及多重分形模型。认为:1)差分GPS法、结构光激光扫描法、三维激光扫描仪法和近景摄影测量法将在亚毫米一,厘米级地表微地形测量及地表粗糙度多尺度特征研究中发挥重要作用,同时简单、方便的测针法可能在野外测量中依然占据主导地位;2)以地表微地形测量技术为基础,在土壤侵蚀过程模型中亟需形成一套完整的“测量一定量化一模型应用”范式,同时应加强对地表微地形空间异质性和各向异性的研究,发展新的统一的地表粗糙度定量化方法。

关 键 词:地表微地形  地表粗糙度  定量化  接触式  非接触式

Review of measurement and quantification of surface microtopography
Zhu Liangjun,Zhang Guanghui.Review of measurement and quantification of surface microtopography[J].Science of Soil and Water Conservation,2013(5):114-122.
Authors:Zhu Liangjun  Zhang Guanghui
Institution:1'2 ( 1. School of Geography, Bcijing Normal University, 100875, Beijing, China; 2. State Key Laboratory of Soil Erosion and Dryland Farming on Loess Plateau, Institute of Soil and Water Conservation Chinese Academy of Science and Ministry of Water Research, 712100, Yangling, Shaanxi, China)
Abstract:Surface microtopography, as the basis of quantification of surface roughness, is closely related to dynamic changes of soil erosion, hydrological process simulation and the soil erosion process modeling. At present, techniques used to quantify surface microtopography can be divided into two categories, contact and non-contact measurement. The former consists of pins, chain and GPS-RTK methods, while the latter includes ultrasonic, infrared sensor, structured lighting laser scanner, laser scanner based on distance measuring, 3D laser scanner and close -range photogrammetry. In first instance, a comprehensive review of the principle, merits and demerits and applications of all techniques is given in this paper. The next part is a brief introduction of often-used indices for water erosion research, which are based on statistical, geostatistical, fractal and multifractal models. Finally, two major conclusions are drawn. First of all, GPS-RTK, structured lighting laser scanner, 3D laser scanner and close-range photogrammetry will continually contribute to the measurement of microtopography at millimeter to centimeter scale and the research of muhiscale surface roughness characteristics, while the pins method will be still widely used in field test because of its simplification and convenience. However, based on the measurement techniques, more efforts should be made in generating an integrated technological process of measurement, quantification and model application in soil erosion models. Besides, by considering spatial anisotropy and heterogeneity of surface roughness, it is essential to develop a new and uniform quantification method for describing microtopography.
Keywords:soil microtopography  surface roughness  quantification  contact measurement  non-contactmeasurement
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