用 Ca 2+ 离子浓度估算岩溶地区岩石溶蚀速率: 以贵州普定为例*

南京大学学报(自然科学版) ›› 2010, Vol. 46 ›› Issue (6): 664–670.

用 Ca 2+ 离子浓度估算岩溶地区岩石溶蚀速率: 以贵州普定为例*

王腊春 1 ** , 蒙海花 1 , 苏维词 2 , 徐泽林 3

出版日期:2015-04-07 发布日期:2015-04-07
作者简介: ( 1. 南京大学地理与海洋科学学院, 南京, 210093; 2. 贵州科学院山地资源研究所, 贵阳, 550001; 3. 贵州普定岩溶研究试验站, 普定, 562100)
基金资助:
国家自然科学基金( 40571024) , 国家"973"基础研究计划( 2006CB403208)

Estimate of erosion rates in a karst region using calcium concentrations: A case study of Puding, Guizhou, southern China

Wang La Chun 1 , Meng H ai Hua 1 , Su Wei Ci 2 , X u Ze?Lin 3

Online:2015-04-07 Published:2015-04-07
About author: (1. School of Geography and Ocean Sciences, Nanjing University, Nanjing, 210093, China;
2. Institute of Mountain Resources, Guizhou Academy of Sciences, Guiyang, 550001, China;
3. Karst Research Station of Puding County, Guizhou, 562100, China)

摘要/Abstract

摘要： 在探讨岩石溶蚀速率计算方法的基础上, 根据研究区特殊的岩溶地质特征, 提出了采用 Ca 2+ 浓度估算岩溶流域岩石溶蚀速率的新方法. 首先, 将 Ca 2+ 浓度换算成 CaCO 3 浓度, 结合实测流量, 计算
出实际流失的 CaCO 3 , 并换算成流域平均岩石溶蚀量, 然后根据岩石的平均容重, 计算出流域岩石溶蚀厚度, 经过换算得到流域岩石溶蚀速率, 该方法适用于可溶岩中碳酸钙的比例较大的闭合区域. 贵州普
定后寨河流域母猪洞子流域为可溶岩中碳酸钙的比例约 98% 的封闭的洼地, 因此可以使用该方法进行计算. 通过该方法对研究区岩石溶蚀速率的计算可知, 该研究区的平均溶蚀速率为 41 ? 5mm/ ka, 该研究
区枯水期的岩溶溶蚀速率基本都小于丰水期的岩溶溶蚀速率, 与前人对该地区的研究结果非常相近, 说明该方法是可行的, 为以灰岩为主的岩溶地区地质溶蚀研究提供了一种新的思路.

Abstract: This paper puts forward a new method for estimate of the erosion rates of a karst region using calcium concentrations. First, the calcium concentrations are converted into the calcium carbonate concentrations; then, the
CaCO 3 loss rates are calculated based on the calcium carbonate concentrations and the discharges; finally, the corrosion rates of the rocks are calculated. T he erosion rates are concluded from the average bulk densities and the
corrosion rates of the rocks. T his method can be applied to an area that is closed and has a high calcium carbonate ratio of rocks. The Muzhudong sub?catchment (Guizhou province, southern China) is a very closed region and the
calcium carbonate ratios of the rocks are up to 98%, so this method can be applied to this region. Our results show that the average erosion rate of the Muzhudong sub ?catchment is about 41 ? 5 mm/ ka, which is very close to the
previous estimates obtained based on other methods. Therefore, we believe this method is valuable in that it provides a new tool for studying erosion of the karst regions.

王腊春 1 ** , 蒙海花 1 , 苏维词 2 , 徐泽林 3
. 用 Ca 2+ 离子浓度估算岩溶地区岩石溶蚀速率: 以贵州普定为例*
[J]. 南京大学学报(自然科学版), 2010, 46(6): 664–670.

Wang La Chun 1 , Meng H ai Hua 1 , Su Wei Ci 2 , X u Ze?Lin 3
. Estimate of erosion rates in a karst region using calcium concentrations: A case study of Puding, Guizhou, southern China
[J]. Journal of Nanjing University(Natural Sciences), 2010, 46(6): 664–670.

参考文献

[ 1 ] Yu J B, Yang L C, Zhang H S, et al. T ypical study on developmental regularity of karst in China. Beijing: Science Publishing, 1990, 10. ( 俞锦标, 杨立铮, 章海生等. 中国喀斯特发育规律典型研究. 北京: 科学出版社, 1990, 10) .
[ 2 ] Ruan X D, Wang Y, Wu S Y, et al. T he re search of corrosion rate. Physics of Guangxi, 2005, 26(2) : 1~ 3. ( 阮向东, 汪越, 武绍勇等. 灰岩侵蚀速率的研究. 广西物理, 2005, 26 ( 2) : 1~ 3) .
[ 3 ] Ma P X, Guo Z Y, Li K, et al. Production rates and accumulation models of in situ produced 10 Be and 26 Al in surface rocks. Progress in Geophysics, 1998, 13(1) : 101~ 114. ( 马配学,
郭之虞, 李坤等.10 Be 和 26 Al 就地产率与在地表岩石中浓度积累的定量模型. 地球物理学进展, 1998, 13( 1) : 101~ 114).
[ 4 ] Heisinger B, Nolte E. Cosmogenic in situ production of radionuclides: Exposure ages and erosion rates. Nuclear Instruments and Methods in Physics Research, 2000, 172: 790~ 795.
[ 5 ] Liu Z H. Field experimental research on the corrosion kinetics of limestone and dolomite in allogenic water?case from Yao Shan Mt, Guilin. Carsologica Sinica, 2000, 19( 1): 1~ 4. ( 刘再
华. 外源水对灰岩和白云岩的侵蚀速率野外试验研究! !! 以桂林尧山为例. 中国岩溶, 2000, 19(1): 1~ 4).
[ 6 ] Jia L P, LiW, Zhu M, etal. Dynamic corrosion effect of different microbes on limestone. Chinese Journal of Applied and Environmental Biology, 2007, 13( 1) : 126~ 130. ( 贾丽萍, 李? 为,
朱敏等. 典型细菌、真菌、放线菌对石灰岩动态溶蚀效果比较. 应用与环境生物学报, 2007, 13(1): 126~ 130).
[ 7 ] Corbels J. Erosion en terrain calcaire. Annales De Geographie, LXVIII annee, 1959, 36.
[ 8 ] Tuo C G, Yuan D X. Formation of karst cavities and comparison between carbonate rock dissolution rates in China and some other parts of the world. Carsologica Sinica, 1987, 6( 2): 131~
136. (托格, 袁道先. 溶蚀空间的形成及中国与世界其它地区碳酸盐岩近期溶蚀量的对比研究. 中国岩溶, 1987, 6(2): 131~ 136).
[ 9 ] Ford D C, Williams P W. Karst geomorphology and hydrology. London: Unwin Hyman. 1969, 376.
[ 10] Pulina M. preliminary studies on denudation in sw Spitsbergen. Bulletin de Lacademie Polonaise des Sciences?Serie des Sciences de la Terre, 1974, 22(2): 83~ 95.
[ 11] Atkinson T C, Smith D I. The erosion of limestones. In Ford T D, Cullingford C H D, editors, T he Science of Speleology, Academic Press, 1976.
[ 12] Bono P, Percopo C. Flow dynamics and erosion rate of a representative karst basin ( Upper Aniene River, Central Italy) . Environmental Geology, 1996, 27: 210~ 218.
[ 13] Warfvinge P. Basic principles of frequently used models. In T rudgill S T, editor, Solute modeling in catchment systems. Chiche[ 14] ? Shih S M, Lin J P, Shiau G W. Dissolution
rates of limestones of different sources. Journal of Hazardous Materials B, 2000 ( 79 ) : 159~ 171.
[ 15] Harmon R S, Wicks C M. Perspectives on Karst geomorphology, hydrology, and geochemistry ! a tribute volume to Ford and White W B. Geological Society of America, Special Paper 2006, 404.
[ 16] Wang L C, Xu Y P, Zhang L F, et al. T he characteristic study of karst water at Houzhai underground basin in Puding county, Guizhou Province. Scientia Geographica Sinica, 2000, 20
( 6) : 557~ 562. ( 王腊春, 许有鹏, 张立峰等. 贵州普定后寨地下河流域岩溶水特征研究, 地理科学, 2000, 20( 6) : 557~ 562).
[ 17] Wang L C, Shi Y L. Formation process and ra tional use of water resources and transform of rainfall, surface water and underground water in
karst mountainous area in southwest China. Scientia Geographica Sinica, 2006, 26( 2) : 173~ 17. (王腊春, 史运良. 西南喀斯特山区三水转化与水资源过程及合理利用. 地理科学, 2006, 26 (2): 173~ 178).
[ 18] Wang F Y. The relationship of the plateau karst geomorphology and the drainage structure. Journal of Nanjing University ( Natural Sciences. Geography Special Issue), 1992, 13: 122~ 133.
(王飞燕. 高原喀斯特地貌及其与流域结构的关系. 南京大学学报( 自然科学. 地理学专辑), 1992, 13: 122~ 133) .
[ 19] Yu J B, Li C H, Zhao P D, et al. Study on carbon dioxide content in soil air and corrosion of carbonate rocks in karst area of Puding county,
Guizhou Province. Carsologica Sinica, 1984, 4: 325~ 331. ( 俞锦标, 李春华, 赵培道等. 贵州普定县岩溶地区土壤空气中 CO 2 含量分布及溶蚀作用的研究. 中国岩溶, 1985(4): 325~ 331).
[ 20] Shang X S, Wang D. Application of two different hydrological models in the typical karsf area, Guizhou, Southem China. Journal of Nanjing
University ( Natural Sciences), 2009, 45( 3): 409~ 416. ( 尚晓三, 王栋. 两种不同类型的水文模型在贵州典型岩溶地区的应用. 南京大学学报( 自然科学), 2009, 45(3): 409~ 415) .ster: Wiley. 1995

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