| 地下水补给与开采量对降水变化响应特征:以京津以南河北平原为例 |
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| 引用本文： | 张光辉,费宇红,杨丽芝,郝明亮,申建梅.地下水补给与开采量对降水变化响应特征:以京津以南河北平原为例[J].地球科学,2006,31(6):879-884. |
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| 作者姓名： | 张光辉 费宇红 杨丽芝 郝明亮 申建梅 |
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| 作者单位： | 中国地质科学院水文地质环境地质研究所,河北,石家庄,050061;中国地质科学院水文地质环境地质研究所,河北,石家庄,050061;中国地质科学院水文地质环境地质研究所,河北,石家庄,050061;中国地质科学院水文地质环境地质研究所,河北,石家庄,050061;中国地质科学院水文地质环境地质研究所,河北,石家庄,050061 |
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| 基金项目： | 国家自然科学基金;国家重点基础研究发展计划(973计划) |
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| 摘 要： | 通过对京津以南河北平原年降水量、地下水补给量和农业开采量三者动态规律及其互动关系研究表明, 年降水量减增, 同期地下水补给量与开采量呈互逆变化规律, 即降水量减小, 补给量变少, 开采量增大; 年降水量增大, 补给量较多, 开采量减小.在连续枯(丰) 水年份, 当年降水量减少(增加) 10mm时, 则地下水系统水量减少7.08 (增加7.06) mm, 水位下降(上升) 5.2~8.7cm; 在10~320mm变幅内, 当年降水量减少(增加) 10%时, 则地下水系统水量减少7.98 (增加7.67) %.气候旱化过程中降水变化对引起补给量减少和开采量增加的幅度, 大于气候增雨过程中降水变化对补给量增大和开采量减少的影响程度.因此, 需要重视连续枯水年份降水变化对地下水系统影响的应对举措, 这对于提高我国北方区域地下水资源供给安全保障具有重大意义.
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| 关 键 词： | 降水量 地下水系统 补给与开采 互逆影响 连续枯水年 |
| 文章编号： | 1000-2383（2006）06-0879-06 |
| 收稿时间： | 2006-05-28 |
| 修稿时间： | 2006-05-28 |
Responses of Groundwater Recharge and Pumpage to Change in Precipitation in Hebei Plain |
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| ZHANG Guang-hui,FEI Yu-hong,YANG Li-zhi,HAO Ming-liang,SHEN Jian-mei.Responses of Groundwater Recharge and Pumpage to Change in Precipitation in Hebei Plain[J].Earth Science-Journal of China University of Geosciences,2006,31(6):879-884. |
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| Authors: | ZHANG Guang-hui FEI Yu-hong YANG Li-zhi HAO Ming-liang SHEN Jian-mei |
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| Institution: | Institute of Hydrogeology and Environmental Geology, CAGS, Shijiazhuang 050061, China |
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| Abstract: | The research from 1986 to 2000 into the dynamic processes and interactions among annual precipitation, annual groundwater recharge from rainfall and annual pumpage for agriculture in Hebei plain to the south of Beijing and Tianjin, revealed the negative relationship between the increase or decrease in annual precipitation and the contemporaneous annual groundwater recharge from rainfall and the annual pumpage. In another word, when the annual precipitation decreases, the recharge decreases, but the pumpage increases. However, when the annual precipitation increases, the recharge increases to a relatively great extent, but the pumpage decreases. During the successive years of shortage or abundance of water, if the annual precipitation decreases (or increases) by 10 mm, the water quantity of the regional groundwater system decreases by 7.08 mm (or increases by 7.06 mm) and the corresponding water level falls (rises) by 5.2 cm to 8.7 cm. In the range of the annual precipitation variation from 10 to 320 mm, if the annual precipitation decreases (or increases) by 10%, the water quantity of the regional groundwater system decreases by 7.98% (or increases by 7.67%), the corresponding water level falls (rises) at the same rate. The effect of the precipitation variation both on the decrease in recharge and on the increase in pumpage in the dehumidification season is greater than that on the increase in recharge and on the decrease in pumpage in the increasingly raining season. Therefore, more attention should be paid to some measures that may soften the effect of the precipitation variation on the underground water system in the successive years of shortage of water, which may be of great significance to the stability and security in the underground water supply system in the north of China. |
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| Keywords: | precipitation groundwater system recharge and pumpage negative relationship successive years of shortage of water |
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