黔西北裸露岩溶地区水文地球化学特征对土地利用方式的响应研究

杨桂花; 潘晓东; 袁建飞; 邓国仕; 唐业旗

doi:10.11932/karst20180407

黔西北裸露岩溶地区水文地球化学特征对土地利用方式的响应研究

doi: 10.11932/karst20180407

1.
中国地质调查局成都地质调查中心
2.
中国地质科学院岩溶地质研究所/自然资源部、广西岩溶动力学重点实验室/联合国教科文组织国际岩溶研究中心

基金项目: 基金项目：中国地质调查局地质调查项目(12120113052500、DD20160285)；国家自然科学基金项目(41502245)

计量
- 文章访问数: 1959
- HTML浏览量: 686
- PDF下载量: 569
- 被引次数: 0
出版历程
- 发布日期: 2018-08-25

Response of hydrogeochemical characteristics to land-use modes in exposed karst areas of northwestern Guizhou Province

1.
Chengdu Center, China Geological Survey
2.
Institute of Karst Geology,CAGS/Key Laboratory of Karst Dynamics ,MNR＆GZAR/International Research Center on Karst under the Auspices of UNESCO

摘要

摘要: 为了探讨不同土地利用方式下的水文地球化学特征与地下水循环演化的关系，文章选取贵州省毕节市典型农业区的农田、林地、草地灌木和建筑用地等四类土地利用方式，通过区域地质调查、遥感解译、水化学分析和图解方法，研究裸露岩溶地区其对地下水水化学组分的影响。结果表明：这四类土地利用区域地下水主要组分的浓度和主要矿物的饱和指数都呈差异性。此外，土壤易溶盐组分也随土地利用类型发生改变。并且发现，绝大多数样品中，土壤易溶盐组分浓度高于地下水中相同的组分。因此，降雨入渗补给条件下淋滤作用可导致土壤中易溶盐组分进入地下水中，进而影响地下水化学组分浓度的演化趋势。研究区域地下水均以HCO3-Ca型，HCO3-Ca-Mg型和HCO3-SO4-Ca型水为主，但是，受自然地理因素和人类活动的影响，地下水组分和水化学类型在不同土地利用类型区域中存在差异性。基于本研究建立了地下水演化的两种概念模型。
- 岩溶地区 /
- 土地利用 /
- 地下水 /
- 水化学特征 /
- 人类活动
Abstract: Land use modes are important to assess the impact of human activity on the earth surface, especially in bare karst areas. The hydrogeochemical characteristics can be used in this assessment. This study was based on geological survey combined with remote sensing and hydrochemical analysis of groundwater. The purpose was to reveal the response of hydrogeochemistry to land-use modes in a typical karst agricultural region of Bijie city, Guizhou Province. The major land-use modes include farmland, woodland, grassland and construction land. It was found that there are differences in the concentrations of major ions of groundwater and SI (Saturation Index) values of dominant minerals for these four different landuse modes. In addition, the contents of water-soluble salts of soil are higher than that of major ions of groundwater in almost all of samples, indicating that under the condition of rainfall infiltration recharge, the leaching of water-soluble salts can affect the concentrations of major ions in groundwater. Moreover, the dominant groundwater types are ofHCO3-Ca, HCO3-Ca-Mg, and HCO3-SO4-Ca in compositions for these four land-use modes. However, due to the influences of natural geographical factors and human activity, there are differences in the compositions and hydrochemical types for these four land-use modes. Based on these results, two conceptual models are established for the evolution of groundwater in the study area.
- karst area /
- land use /
- groundwater /
- hydrochemical characteristics /
- human activity

HTML

参考文献(30)

[1]	蒋忠诚，王瑞江，裴建国，等. 我国南方表层岩溶带及其对岩溶水的调蓄功能［J］. 中国岩溶,2001, 20(2):24-28.
[2]	蒋向明，吉淑华. 岩溶水水化学特征在水文地质条件分析中的应用：以娘子关泉群岩溶水系统寿阳区为例［J］.中国煤田地质, 2007,19(4):45-47.
[3]	裴建国，梁茂珍，陈阵. 西南岩溶石山地区岩溶地下水系统划分及其主要特征值统计［J］. 中国岩溶, 2008, 27(1): 6-10.
[4]	王学平，李稳哲. 地质构造对鄂尔多斯盆地南缘岩溶地下水的控制作用［J］. 西北地质, 2010, 43(3):106-112.
[5]	闫福贵，梁永平，张翼龙，等. 鄂尔多斯盆地周边地区岩溶发育模式及岩溶地下水开发利用探讨［J］. 地学前缘, 2010, 17(6):227-234.
[6]	胡伟，吕玉香，熊开治，等.地层岩性对重庆渝东南渝东北地区岩溶地下水的富集影响分析［J］.地下水,2014,36(6):188-190.
[7]	邹胜章，李录娟，卢海平，等. 岩溶地下水系统防污性能评价方法［J］. 地球学报, 2014, 35(2):262-268.
[8]	Turk J, Malard A, Jeannin P Y, et al. Hydrogeological characterization of groundwater storage and drainage in an alpine karst aquifer (the Kanin massif, Julian Alps)［J］. Hydrological Processes, 2015, 29 (8):1986-1998.
[9]	潘晓东，梁杏，唐建生，等. 黔东北高原斜坡地区4种岩溶地下水系统模式及特点：基于地貌和蓄水构造特征［J］. 地球学报, 2015, 36(1):85-93.
[10]	袁建飞，邓国仕，徐芬，等. 毕节市北部岩溶地下水水文地球化学特征［J］. 水文地质工程地质, 2016,43(1):12-21.
[11]	袁建飞，邓国仕，徐芬，等. 毕节市北部岩溶地下水水化学特征及影响因素的多元统计分析［J］. 中国地质, 2016, 43(4):1446-1456.
[12]	Wang Y, Guo Q, Su C, et al. Strontium isotope characterization and major ion geochemistry of karst water flow, shentou, northern china［J］. Journal of Hydrology, 2006, 328(3-4):592-603.
[13]	张群利，郭会荣，吴孔军，等. 荥巩矿区岩溶地下水系统的水文地球化学特征及其指示意义［J］.水文地质工程地质,2011, 38 (2):1-7.
[14]	Yuan J, Xu F, Deng G, et al. Using stable isotopes and major ions to identify hydrogeochemical characteristics of karst groundwater in xide country, sichuan province ［J］. Carbonates and Evaporites,2018,33:223-234.
[15]	袁建飞，邓国仕，徐芬，等. 川西南喜德热田地下水水文地球化学特征［J］. 现代地质, 2017, 31(1):200-208.
[16]	贾亚男. 农业土地利用对岩溶地下水影响研究综述［J］. 中国岩溶, 2003, 22 (4):306-317.
[17]	覃小群，蒙荣国，莫日生. 土地覆盖对岩溶地下河碳汇的影响：以广西打狗河流域为例［J］. 中国岩溶, 2011, 30 (4):372-378.
[18]	贾亚男，袁道先. 土地利用变化对水城盆地岩溶水水质的影响［J］. 地理学报, 2003, 58 (6):831-838.
[19]	张军以，王腊春，苏维词，等. 岩溶地区人类活动的水文效应研究现状及展望［J］. 地理科学进展, 2014, 33 (8):1125-1135.
[20]	Jiang Y. The impact of land use on soil properties in a karst agricultural region of southwest china: a case study of xiaojiang watershed, yunnan［J］. Journal of Geographical Sciences, 2006, 16(1): 69-77.
[21]	Jiang Y, Zhang C, Yuan D,et al. Impact of land use change on groundwater quality in a typical karst watershed of southwest china: a case study of the xiaojiang watershed, yunnan province［J］. Hydrogeology Journal, 2008, 16 (4):727-735.
[22]	Jiang Y J, Yuan D X, Zhang C, et al. Impact of land-use change on soil properties in a typical karst agricultural region of southwest china: a case study of xiaojiang watershed, yunnan［J］. Environmental Geology, 2006, 50 (6):911-918.
[23]	Li Y, Xie D, Wang S, et al. Impact of land cover types on the soil characteristics in karst area of chongqing［J］. Journal of Geographical Sciences, 2006, 16(2):143-154.
[24]	Yanan J, Daoxian Y. The influence of land use change on karst water quality of shuicheng basin in Guizhou province［J］. Journal of Geographical Sciences, 2004, 14 (2):143150.
[25]	Zhang C, Pei J, Xie Y, et al. Impact of land use covers upon karst processes in a typical fengcong depression system of nongla, Guangxi, china［J］. Environmental Geology, 2007,55 (8):1621-1626.
[26]	贾亚男，刁承泰，袁道先. 土地利用对埋藏型岩溶区岩溶水质的影响:以涪陵丛林岩溶槽谷区为例［J］. 自然资源学报, 2004, 19 (4):455-461.
[27]	王焰新，高旭波. 人类活动影响下娘子关岩溶水系统地球化学演化［J］. 中国岩溶, 2009, 28(2):103-112.
[28]	Jingan S, Jiupai N, Chaofu W, et al. Land use change and its corresponding ecological responses: A review［J］. Journal of Geographical Sciences, 2005, 15 (3):305-328.
[29]	Koh D C, Ko K S, Kim Y,et al. Effect of agricultural land use on the chemistry of groundwater from basaltic aquifers, Jeju Island, South Korea［J］. Hydrogeology Journal, 2007,15(4):727-743.
[30]	邓国仕，唐业旗，李鹏岳，等. 乌蒙山片区1∶5万海子街幅水文地质环境地质调查报告［R］.成都：中国地质调查局成都地质调查中心, 2015:9-36.