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中国农学通报 ›› 2010, Vol. 26 ›› Issue (21): 305-311.

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

岩溶森林区地下河流域水文地球化学特征研究—以贵州荔波板寨地下河为例

李清艳 何师意 康志强 熊志斌   

  • 收稿日期:2010-05-13 修回日期:2010-07-28 出版日期:2010-11-05 发布日期:2010-11-05
  • 基金资助:

    地调项目“岩溶地下水监测与环境脆弱性评价”(1212010634805)及“岩溶动力系统及碳循环”项目编号:40231008

Study on Hydrogeochemical Features in Karst Forest Underground River Catchment Of Banzhai,Libo,Guizhou

  • Received:2010-05-13 Revised:2010-07-28 Online:2010-11-05 Published:2010-11-05

摘要:

通过对板寨地下河流域内岩溶泉、地表水体和地下河水各测站的水化学资料的分析,讨论了流域内各点的水化学类型、空间分布及成因。由于森林植被覆盖,计算得岩溶泉水的PCO2很高,实测得拉桥泉域内土层20cm深处CO2浓度高,达38000ppm,是退耕田地中土壤CO2浓度的30倍;森林中地表覆被形成林中滞留水含水层,它与岩溶含水岩层组形成多层水文地质含水空间结构,增加了调蓄量,延缓了水的释放,这极大改善了区内因降雨分布不均匀而引起的干旱面貌。虽然茂兰处在原始森林区,但是土壤较少,根据实验结果,森林区岩溶作用强度并不比非森林岩溶区强。自然保护区缓冲区有少量村民居住,农业活动,如施肥和生活污水排放等,造成了地下水污染。岩溶表层带泉,受地表环境、降雨量影响大,水化学动态变化较大。地下河水的水化学变化特征明显受降雨的稀释作用影响。

关键词: 羊驼, 羊驼, cDNA库筛选, AIF基因, 免疫组化

Abstract:

The hydrochemistry type, spatial distribution and the cause of formation about the river were discussed by analyzing the hydrochemistry data which from the karst springs, the surface water and the underground water monitoring stations in Banzhai. The results showed that the pCO2 of the karst spring was high, and the concentration of the CO2 in 20cm depth was 38000ppm in the area of Laqiao,which was 30 times higher than the area of returning farmland. The surface retained water which was formed by the land cover in the forest and karst aquifer make up a multilayer hydrogeology space structure, which increased discharge storage largely and decreased the water release. Then the arid landform caused by an unequal distribution of rainfall was improved greatly. The soil in maolan was much less than in not-karst zone, although the maolan in forest area, where the process of karst in the forest area was not strong. The pollution of the MaoLan Natural was mainly from agricultural activities such as the effect of fertilizer and domestic sewerage etc. The dynamical change of hydrochemistry in epikarst spring water was influenced by surface environment and rainfall greatly. The hydrochemistry of underground water was affected by the diluting processes of rainfall obviously.