摘要
湖南洛塔为西南具有一定代表性的溶丘洼地型岩溶区,本文利用近两年来洛塔水环境监测资料,进行洛塔表层岩溶带的水化学和水温场特征的研究,认为该表层岩溶带的水化学和水温场的特征与气候、生态环境和岩溶含水介质等多种因素明显相关。不同影响因素对表层岩溶水水化学组分的作用有所不同,表层岩溶带岩溶水受气候影响较大,大气降水的降雨强度,直接影响到地下水化学组分含量的大小,总硬度和HCO-3含量与降雨量呈明显的负相关关系,植被、土壤的覆盖程度与水化学组分含量高低呈正相关性。
Luota is a typical karst area of karst hilldepression in southwest China. In this paper, characteristics of hydrochemical field and water temperature field of the epikarst zone in Luota are studied by monitor data of water environment in the recent two years. It is concluded that the origin of hydrochemical field and water temperature field is evidently related with some factors, such as climate, ecological environment, karst waterbearing medium. Different influencing factors have different effects on hydrochemical component of epikarst water while epikarst water is affected largely by climate. Rainfall is the main recharge for epikarst water, of which the intensity directly affects hydrochemical component, while total hardness and HCO3 are evident negatively related to rainfall. As for a highcold mountainous area, the temperature of epikarst water is quite low and varies with the season. The impact of ecologic environment on hydrochemical component of the epikarst water is that the covered rate of vegetation and soil is positively related to hydrochemical component of the water.
出处
《中国岩溶》
CAS
CSCD
2003年第2期103-109,共7页
Carsologica Sinica
基金
地质调查项目<岩溶石山区生态系统可持续发展模式与推广>(编号水[2002]002-4)
国土资源部攻关项目<表层岩溶带调蓄与生态重建试验示范>(编号20010303)