CAO Mingda,ZHOU Zhongfa,PAN Yanxi,et al.Temporal and Spatial Variation of Water Chemistry and Environmental Indication of Drip Water in Karst Cave —A Case Study of Zhijin Cave， Guizhou Province[J].Research of Soil and Water Conservation,2017,24(03):339-346.
喀斯特洞穴滴水水文化学过程的时空变化及其环境指示——以贵州织金洞为例
- Title:
- Temporal and Spatial Variation of Water Chemistry and Environmental Indication of Drip Water in Karst Cave —A Case Study of Zhijin Cave， Guizhou Province
- 分类号:
- P641.3
- 摘要:
- 洞穴水地球化学过程的研究对于洞穴内次生沉积物景观的发育有着重要的意义，2015年1—12月通过现场滴定测量和实验室仪器分析对贵州织金洞洞穴水的水化学指标进行了为期一个完整水文年的动态监测，采样时间均为每月26—28日。结果表明：（1） 洞穴滴水滴率和Ca2+，Mg2+，Sr2+离子浓度均与降水量有很好的响应，但同时都表现出一定的滞后性，其中Mg2+，Sr2+离子所携带的气候信号较为持久，Ca2+离子浓度在雨季波动较大。（2） 滴水水化学性质在化学计量上总体符合石灰岩喀斯特地区的侵蚀方程，Ca2+/HCO3-的比值均在1/2上下波动；（3） 滴水中的SIc和SId之间存在显著的正相关关系，滴水中的液相CO2分压[lgPCO2（water）]与pH值之间呈现出显著的负相关，体现了上覆土壤层中的高浓度CO2对洞穴滴水化学过程的重要影响。（4） 滴水中的Mg/Ca与Sr/Ca比值在雨季到来后的曲线变化呈现出明显的同增同减性特征，证明CaCO3在未到达洞穴之前就已经在土壤层和基岩层中发生了优先沉积（PCP），致使运移到洞内的Ca2+离子浓度相对其他离子的升高程度小；（5） 滴水中Mg/Ca比值与Sr/Ca比值都有较明显的季节变化，但是Sr/Ca比值季节滞后性明显，而Mg/Ca比值年际变化更具波动性，对外界降水变化响应较敏感。
- Abstract:
- The study of the geochemical process of the cave is of great significance to the development of the secondary deposits in the cave. From January 2015 to December 2015, the water chemistry indexes of Zhijin Cave in Guizhou Province were monitored in a whole year. Results showed that: (1) the drip rate of dripwater and Ca2+, Mg2+, Sr2+ ion concentrations had the very good response to precipitation, but also reflected the certain lag, and Mg2+, Sr2+ ions carried by the climate signal is very persistent, Ca2+ ion concentration in the rainy season fluctuated; (2) drip water chemical properties in the chemical measurement were compliance with the erosion of limestone in Karst area on the overall, the ratio of Ca2+/HCO3- was 1/2 with up and down fluctuations; (3) significant positive correlation between the drop of SIc and SId was founed, drop of water in the liquid phase partial pressure of CO2 [lgPCO2(water)] and pH values showed a significant negative correlation, reflecting the important influence of the high concentration of CO2 in the overlying soil layer of cave drip water chemical processes; (4) the Mg/Ca and Sr/Ca ratios of drip water in rainy season after the arrival of the curve show obvious increase and reduction of feature, indicating that CaCO3 has in the soil layers before it did not reach the cave, and the bedrock layer occurred prior calcite precipitation (PCP), resulting in the increase of migrating to the inside of the Ca2+ ion concentration was less compared with the other ions; (5) The ratios of Mg/Ca and Sr/Ca in drip water presented the obvious seasonal variation, but seasonal ratios of Sr/Ca lagged significantly, and Mg/Ca ratios of interannual variation was more volatility, the change response is sensitive to the outside precipitation.
参考文献/References:
[1] Gonzales L A, Carpenter S J, Lohmann K C. Inorganic calcite morphology:roles of fluid chemistry and fluid flow[J]. Journal of Sedimentary Research, 1992,63(3):382-399.
[2] Ford D C, Williams P D. Karst Hydrogeology and Geomorphology[M]. John Wiley &.Sons, Ltd., 2007:36-180.
[3] Cowell D W, Ford D C. Hydrochemistry of a dolomite karst:the Bruce Peninsula of Ontario[J]. Canadian Journal of Earth Sciences, 2011,17(17):520-526.
[4] Bogli A. Karst Hydrology and Physical Speleology[M]. Berlin:Springer-Verlag,1980:150-180.
[5] 袁道先,章程.岩溶动力学的理论探索与实践[J]地球学报,2008,29(3):361-371.
[6] 蒋忠诚,裴建国,夏日元,等.我国"十一五"期间的岩溶研究进展与重要活动[J].中国岩溶,2010,29(4):349-354.
[7] 张美良,朱晓燕,吴夏,等.广西巴马县水晶宫洞穴沉积物特征及其沉积环境[J].中国岩溶,2013,32(3):345-357.
[8] 张美良,朱晓燕,吴夏,等.地下河水人工补给洞穴滴水、碳酸盐(钙)沉积特征及景观恢复探讨[J].中国岩溶,2015,34(1):17-26.
[9] 李涛,曹建华,张美良,等.桂林盘龙洞岩溶表层带土壤CO2浓度的季节变化研究[J].中国岩溶2011,30(3):348-353.
[10] 袁道先.中国岩溶动力系统[M].北京:地质出版社,2002:62-108.
[11] 叶明阳,李廷勇,王建力,等.芙蓉洞洞穴水Ca2+,Mg2+浓度变化对气候事件的响应[J].水土保持学报,2009,23(3):82-86.
[12] 李景阳,安裕国.暗河型溶洞的形成和演化过程:以贵州织金洞等为例[J].贵州工学院学报,1991,20(3):1-9.
[13] 安裕国,戎昆方,李景阳,等岩溶洞穴生物地质作用研究:以贵州织金洞等为例[J].贵州地质,1996,3(48):203-207.
[14] 贺卫,朱文孝.织金洞扫尾豪猪灭迹之原因探讨[J].中国岩溶,1996,15(3):239-245.
[15] 贵州省地层古生物工作队.西南地区区域地层表(贵州省分册)[M].北京:地质出版社,1976:220-350.
[16] 贵州省地质矿产局.全国地层多重划分对比研究:贵州省岩石地层[M].武汉:中国地质大学出版社,1997.225-336.
[17] 王新中,班凤梅,潘根兴.洞穴滴水地球化学的空间和时间变化及其控制因素[J].第四纪研究,2005.25(2):258-264.
[18] 闫志为,刘辉利,张志卫.温度及CO2对方解石、白云石溶解度影响特征分析[J].中国岩溶,2009,28(1):7-10.
[19] HuangY M, Fairchild I J, Borsato A, et al. Seasonal variations in Sr, Mg and P in modern speleothems (Grotta di Ernesto, Italy)[J]. Chemical Geology, 2001,175(3/4):429-448.
[20] Fairchild I J, Borsato A, Tooth A F, et al. Controls on trace element(Sr-Mg)compositions of carbonate cave waters:Implications for speleothem climatic records[J]. Chemical Geology, 2000,166(3/4):255-269.
[21] 李吉龙.安徽蓬莱仙洞洞穴滴水水文地球化学指标变化及其意义[D].南京:南京师范大学,2014.
[22] Roberts M S, Smart P L, Baker A. Annual trace element variations in a Holocene Speleothem[J]. Earth and Planetary Science Letters, 1998,154(1/4):237-246.
[23] 章典.喀斯特洞穴环境特征[J].中国岩溶,1983,2(1):31-39.
[24] Burton E A, Walter L M. The effects of PCO2and temperature on magnesium incorporation in calcite in seawater and MgCl2-CaCl2 solutions[J]. Geochimica et Cosmochimica Acta, 1991,55(3):777-785.
[25] Morse J W, BenderM L. Partition coefficients in calcite:Examination of factors influencing the validity of experimental results and their application to natural systems[J]. ChemicalGeology, 1990,82:265-277.
[26] Lorens R B. Sr, Cd, Mn, andCo distribution coefficients in calcite as a function of calcite pricipition rate[J]. Geochimical et Cosmochimical Acta, 1981,45(3):553-561.
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备注/Memo
收稿日期:2016-04-13;改回日期:2016-05-19。
基金项目:国家自然科学基金“岩溶洞穴CO2迁移变化机制及对洞穴岩溶环境的影响研究”（41361081）；贵州省科技计划“贵州省洞穴调查数据技术服务”（黔科合G字[2014]4004-2号）；贵州省重大应用基础研究项目“喀斯特石漠化生态修复及生态经济系统优化调控研究——岩土类型格局”（黔科合JZ字[2014]200201）
作者简介:曹明达(1992-),男,安徽滁州人,硕士研究生,研究方向为喀斯特地貌与洞穴。E-mail:cmd965621@sina.com
通讯作者:周忠发(1969-),男,贵州遵义人,教授,博士生导师,主要从事喀斯特资源环境、GIS与遥感研究。E-mail:fa6897@163.com