桂林峰林平原区岩溶含水层氮污染空间分布特征  

Spatial Distribution of Nitrogen Contamination in Karst Aquifer in Guilin Peak Forest Plain

作　　者：王开然[1,2] 郭芳[1] 姜光辉[1] 陈国富[1,2] 周文亮[1,2] 

机构地区：[1]中国地质科学院岩溶地质研究所岩溶动力学重点实验室,广西桂林541004 [2]西南大学地理科学学院,重庆400715

出　　处：《环境科学研究》2013年第3期281-286,共6页Research of Environmental Sciences

基　　金：国家自然科学基金项目(41102161;41172231;41101036)

摘　　要：为确定桂林东区岩溶含水层氮污染特征,依据地层结构及土地利用状况,选择桂林东区27个地表水与地下水采样点进行取样分析.结果显示:桂林东区地下水NO3--N污染较为严重,ρ(NO3--N)平均值(以N计,下同)为9.15 mgL,濒临世界卫生组织的地下水饮用标准界限(10 mgL);ρ(NH4+-N)基本未检出,ρ(NO2--N)较低且NO2--N主要存在于地表水中,NH4+-N和NO2--N都不是该区地下水中氮的主要存在形式.不同土地利用类型的区域ρ(NO3--N)水平(0.088～46.700 mgL)不同.居民区生活污水和牲畜粪肥是浅层地下水的主要NO3--N污染源,种植蔬菜施用的有机肥则是农业区的NO3--N污染源.此外,受水文地质条件的影响,在研究区地下水流场内沿地下水流方向ρ(NO3--N)呈逐渐升高的趋势.To determine the characteristics of nitrogen contamination in karst aquifer in the east Guilin, samples of the surface and groundwater were sampled according to the stratigraphic structure and patterns of the land use. The results showed that the groundwater in the eastern Guilin was contaminated by nitrate. The average concentration of NO3 --N was 9.15 rag/L, which was on the edge of unsuitable for drinking water according to the National Quality Standard of Groundwater （ 10 rag/L）. NH4 ~ -N was basically not detected, and the concentration of NO2 - -N was also very low, which mainly existed in the surface water. These two forms of nitrogen were not the main types of the underground water in this area. Different patterns of the land use had different NO3 - -N levels ranging from 0. 088 to 46. 700 mg/L. The main source of NO3 - -N pollution in the shallow groundwater was sewage and cattle manure in the residential area. Organic fertilizer used for vegetable planting was the source of NO3 - -N pollution in the agricultural area. In addition, influenced by the hydrogeology condition, the concentration of NO3 - -N had a rising trend with the flow direction of the groundwater in this area.

关 键 词：峰林平原区 岩溶含水层 氮污染 空间分布 

分 类 号：P64[天文地球—地质矿产勘探] X523[天文地球—地质学]