| 基于探地雷达的喀斯特峰丛洼地土壤深度和分布探测 |
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| 引用本文： | 夏银行,黎蕾,邓少虹,陈香碧,何寻阳,吴金水,苏以荣.基于探地雷达的喀斯特峰丛洼地土壤深度和分布探测[J].水土保持通报,2016,36(1):129-135. |
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| 作者姓名： | 夏银行 黎蕾 邓少虹 陈香碧 何寻阳 吴金水 苏以荣 |
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| 作者单位： | 1. 中国科学院亚热带农业生态研究所亚热带农业生态过程重点实验室,湖南长沙410125;中国科学院大学,北京100049;中国科学院环江喀斯特生态系统观测研究站,广西环江547100;2. 广西大学农学院,广西南宁,530005;3. 中国科学院亚热带农业生态研究所亚热带农业生态过程重点实验室,湖南长沙410125;中国科学院环江喀斯特生态系统观测研究站,广西环江547100;4. 中国科学院亚热带农业生态研究所亚热带农业生态过程重点实验室,湖南长沙,410125 |
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| 基金项目： | 国家科技支撑计划项目"喀斯特石漠化中低产土壤改良技术集成示范"(2012BAD05B03-6);中国科学院战略性先导科技专项"典型石漠化地区植被恢复和增汇技术的试验示范"(XDA05070403); 国家自然科学资助项目"喀斯特非连续性土壤有机碳的剖面分布研究"(41171246) |
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| 摘 要： | 目的]研究喀斯特土壤的深度和分布,为利用探地雷达(GPR)技术开展喀斯特地区峰丛洼地土壤分布的研究提供理论依据。方法]通过室内模拟试验,建立喀斯特地区3种典型质地土壤(砂质黏壤土、黏壤土、粉(砂)质黏土)中探地雷达电磁波波速和土壤含水量的关系式。通过实地测定土壤质地和含水量,选择合适的关系式,对探地雷达图像进行校准、解译,获得土壤深度,并采用开挖法进行验证。结果]得到了3种质地土壤中电磁波波速(ν)与含水量(θ)关系的三次多项式。利用该关系式探测的喀斯特土壤理论深度与实地开挖的结果相符,误差为0—10cm。利用探地雷达软件生成了反映测线下不同位置土壤深度的二维图像和样方内土壤深度分布的三维图像,表明土壤主要分布在0—50cm。结论]利用探地雷达技术探测喀斯特地区土壤深度和分布是切实可行的。
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| 关 键 词： | 喀斯特地区 探地雷达 土壤深度 电磁波波速 土壤含水量 土壤质地 |
| 收稿时间： | 2014/12/5 0:00:00 |
| 修稿时间： | 3/8/2015 12:00:00 AM |
Detection of Soil Depths and Distribution Using Ground Penetrating Radar Technology in Karst Peak-Cluster Depression Area |
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| XIA Yinhang,LI Lei,DENG Shaohong,CHEN Xiangbi,HE Xunyang,WU Jinshui and SU Yirong.Detection of Soil Depths and Distribution Using Ground Penetrating Radar Technology in Karst Peak-Cluster Depression Area[J].Bulletin of Soil and Water Conservation,2016,36(1):129-135. |
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| Authors: | XIA Yinhang LI Lei DENG Shaohong CHEN Xiangbi HE Xunyang WU Jinshui and SU Yirong |
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| Institution: | The Key Laboratory of Agro-ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha, Hunan 410125, China;University of Chinese Academy of Sciences, Beijing 100049, China;Huanjiang Observation and Research Station for Karst Ecosystems, Chinese Academy of Sciences, Huanjiang, Guangxi 547100, China;The Key Laboratory of Agro-ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha, Hunan 410125, China;University of Chinese Academy of Sciences, Beijing 100049, China;Huanjiang Observation and Research Station for Karst Ecosystems, Chinese Academy of Sciences, Huanjiang, Guangxi 547100, China;College of Agronomy, Guangxi University, Nanning, Guangxi 530005, China;The Key Laboratory of Agro-ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha, Hunan 410125, China;Huanjiang Observation and Research Station for Karst Ecosystems, Chinese Academy of Sciences, Huanjiang, Guangxi 547100, China;The Key Laboratory of Agro-ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha, Hunan 410125, China;Huanjiang Observation and Research Station for Karst Ecosystems, Chinese Academy of Sciences, Huanjiang, Guangxi 547100, China;The Key Laboratory of Agro-ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha, Hunan 410125, China;The Key Laboratory of Agro-ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha, Hunan 410125, China;Huanjiang Observation and Research Station for Karst Ecosystems, Chinese Academy of Sciences, Huanjiang, Guangxi 547100, China |
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| Abstract: | |
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| Keywords: | karst area ground penetrating radar soil depth electromagnetic wave velocity soil water content soil texture |
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