基于探地雷达的喀斯特峰丛洼地土壤深度和分布探测

夏银行; 黎蕾; 邓少虹; 陈香碧; 何寻阳; 吴金水; 苏以荣

doi:10.13961/j.cnki.stbctb.2016.01.023

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基于探地雷达的喀斯特峰丛洼地土壤深度和分布探测

试验研究

- 基于探地雷达的喀斯特峰丛洼地土壤深度和分布探测
- Detection of Soil Depths and Distribution Using Ground Penetrating Radar Technology in Karst Peak-Cluster Depression Area
- 水土保持通报 2016年36卷第1期页码：129-135
- 作者机构：
  
  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
  2. 中国科学院大学,北京,100049
  3. 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. 广西大学农学院,广西,南宁,530005
- 作者简介：
- 基金信息：
  
  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)
- DOI：10.13961/j.cnki.stbctb.2016.01.023
  中图分类号：
- 纸质出版：2016
- 稿件说明：
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夏银行, 黎蕾, 邓少虹, 等. 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.

XIA Yinhang, LI Lei, DENG Shaohong, et al. Detection of Soil Depths and Distribution Using Ground Penetrating Radar Technology in Karst Peak-Cluster Depression Area[J]. Bulletin of Soiland Water Conservation, 2016, 36(1): 129-135.
夏银行, 黎蕾, 邓少虹, 等. 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. DOI： 10.13961/j.cnki.stbctb.2016.01.023.

XIA Yinhang, LI Lei, DENG Shaohong, et al. Detection of Soil Depths and Distribution Using Ground Penetrating Radar Technology in Karst Peak-Cluster Depression Area[J]. Bulletin of Soiland Water Conservation, 2016, 36(1): 129-135. DOI： 10.13961/j.cnki.stbctb.2016.01.023.

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—10 cm.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—50 cm. [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.

Abstract

[Objective] To analyze the depth and distribution of karst soil in order to provide theoretical basis for using ground penetrating radar(GPR) in the research on soil distribution in karst peak-cluster depression area. [Methods] Through laboratory simulation experiment

this study established the relationship between GPR velocity of electromagnetic wave and soil water content in three types of soil texture(sandy clay loam

clay loam

silty clay) in karst region. Through the field measurement of soil texture and water content

the GPR image was calibrated and interpreted based on the right formula. Then the soil depth was estimated and verified by excavation. [Results] We found the theoretical models of cubic polynomial relationship between electromagnetic wave velocity(ν) and soil water content(θ) for the three soil textures. It showed that soil depth in the field was consistent with the results estimated with theoretical model

and the error range was 0—10 cm. The 2-dimension images reflecting soil depths in the different location under the survey line and the 3-dimension images reflecting soil depths distribution in the quadrant were generated using GPR software. Soil mainly distributed within the depth of 50 cm. [Conclusion] GPR technology was feasible to detect the depths and distribution of discontinuous soil in karst region.

关键词

Keywords

references

Sweeting M M. The Karsts of North China[M]//Karst in China. Berlin, Heidelberg: Springer, 1995:151-180.

Wang S J, Liu Q M, Zhang D F. Karst rocky desertification in southwestern China: Geomorphology, landuse, impact and rehabilitation[J]. Land Degradation & Development, 2004,15(2):115-121.

李豪,张信宝,王克林,等.桂西北倒石堆型岩溶坡地土壤的

137

Cs分布特点[J].水土保持学报.2009,23(3):42-47.

Chen Xiangbi, Zheng Hua, Zhang Wei, et al. Effects of land cover on soil organic carbon stock in a karst landscape with discontinuous soil distribution[J]. Journal of Mountain Science, 2014,11(3):774-781.

于秀秀,马兴旺,迪力夏提,等.探地雷达在土层厚度调查中的试验研究[J].土壤学报,2011,48(4):874-878.

Allred B J, Daniels J J, Ehsani M R. Handbook of Agricultural Geophysics[M]. Boca Raton, London, New York: CRC Press, 2008.

余中明,丁强.地质雷达探测工程的几个问题[J].地质找矿论丛,2006,21(B10):182-184.

Al-fares W, Bakalowicz M, Guérin R, et al. Analysis of the karst aquifer structure of the Lamalou area(Hérault, France)with ground penetrating radar[J]. Journal of Applied Geophysics, 2002,51(2):97-106.

张开伟.GPR技术在隐伏岩溶探测中的异常识别及应用[J].工程勘察,2010(S1):619-627.

Podvin P, Lecomte L. Finite difference computation of traveltimes in very contrasted velocity models: A massively parallel approach and its associated tools[J]. Geophysics, 1991,105(1):271-284.

Tillard S, Dubois J C. Analysis of GPR date: Wave propagation velocity determination[J]. Journal of Applied Geophysics, 1995,33(1):77-91.

Greaves R J, Lesmes D P, Lee J M, et al. Velocity variations and water content estimated from multi-offset, ground-penetrating radar[J]. Geophysics, 1996,61(3):683-693.

袁明德.探地雷达检测中如何计算波速[J].物探与化探,2003,27(3):220-222.

吴信民,曹俊昌,杨亚新,等.黏土中电磁波波速与含水量关系研究及应用[J].水文地质工程地质,2007,34(5):120-122.

刘恒柏,朱安宁,张佳宝,等.不同水分条件下粗砂土剖面中目标物的GPR图像特征及其解译[J].土壤,2009,41(1):112-117.

吉丽青,朱安宁,张佳宝,等.低频探地雷达地波法测定土壤含水量的可行性研究[J].土壤,2011,43(1):123-129.

Grote K, Hubbard S, Rubin Y. Field-scale estimation of volumetric water content using ground-penetrating radar ground wave techniques[J]. Water Resources Research, 2003,39(11):1-13.

Topp G C, Davis J L, Annan A P. Electromagnetic determination of soil water content: Measurements in coaxial transmission lines[J]. Water Resources Research, 1980,16(3):574-582.

Huisman J A, Hubbard S S, Redman J D, et al. Measuring soil water content with ground penetrating radar[J]. Vadose Zone Journal, 2003,2(4):476-491.

汤洪志,黎正根,贺小军.探地雷达在管线探测与工程勘察中的应用[J].华东地质学院学报,1992,22(2):156-166.

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