太行山前平原非河道条件下地下调蓄功能实验研究——以滹沱河冲洪积平原为例
摘要
通过实验研究探讨了太行山前平原地下调蓄能力,实验研究表明,在汇水坑渗、井灌和引水渠渗条件下,太行山前冲洪积平原地下调蓄功能不仅与地表积水深度、入渗时间有关,而且还与汇水总量的多少有关。单位时间渗漏量的大小与地表蓄水深度呈正相关关系。地表蓄水深度愈大,单位时间渗漏量愈大;累计渗漏量随着入渗时间的延长而增加,渗漏速率随着累计渗漏量的增加而减小。采用井灌方式进行地下调蓄的关键,是选择具有强渗透性的层位。
The result of experiments implies that the reserve function of the aquifers from artificial recharge in
Taihang piedmont plain of China is related, not only to the reservoir depth of surface water and the time of
water infiltration but also to the accumulative total volume of water which flows into the reservoir under the
condition of pond infiltration, well injection and channel infiltration. The infiltration rate increases with the
increasing of the reservoir depth of surface water and decreases with its decreasing, while the accumulative
amount of infiltrated water increases with the increasing time. The key for underground artificial reserve trough
well injection is to select the high permeable formation.
The result of experiments implies that the reserve function of the aquifers from artificial recharge in
Taihang piedmont plain of China is related, not only to the reservoir depth of surface water and the time of
water infiltration but also to the accumulative total volume of water which flows into the reservoir under the
condition of pond infiltration, well injection and channel infiltration. The infiltration rate increases with the
increasing of the reservoir depth of surface water and decreases with its decreasing, while the accumulative
amount of infiltrated water increases with the increasing time. The key for underground artificial reserve trough
well injection is to select the high permeable formation.
引文
① 张光辉,等.太行山前平原南水北调地下调蓄潜力研究[R].国土资源部水文地质环境地质研究所,2002．
② 张光辉,等.太行山前平原动水条件下地下调蓄功能实验研究[R].石家庄:中国地质科学院水文地质环境地质研究所,2002．
[1] Ponce V M. Pandey R P, Kumar S. Groundwater recharge by channel infiltration in E1 Barbon basin Baja California [J].Mexico.J Hydrol,1999, 214:1-7．
[2] Scanlon B R. Water and heat fluxes in desert soils field studies [J].Water Resour Res,1994,30:709-719．
[3] Shentsis I, Meirovich L,Ben Zvi A,Rosenthal E. Assessment of transmission losses and groundwater recharge from runoff events in a wadi under shortage of data on lateral inflow[J].Negev.Israel. Hydrol Process,1999,13: 1649-1663．
[4] Sophocleous M. Interactions between groundwater and surface water:the state of science[J].Hydrogeology J, 2002,10(1) : 52-67．
[5] Bouwer H.Artificial recharge of groundwater:hydrogeology and engineering[J].Hydrogeology,2002,10(1) :121-142．
[6] de Vries J J, Simmers I.Groundwater recharge:an overview of processes and challenges[J].Hydrogeology J,2002,10(1) : 5-17．
[7] Healy R W, Cook P G. Using groundwater level. to estimate recharge [J].Hydrogeology J,2002,10(1) : 91-109．
[8] Bohlke J K.Groundwater recharge and agricultural contamination [J].Hydrogeology J,2002,10(1) :153-166．
[9] Gieske A S M. Dynamics of groundwater recharge:a case study in send-arid eastern Botswana [D].Vrije Universiteit.Amsterdam,1992． 289．
[10] Sanford W. Recharge and groundwater models:an overview [J].Hydrogeology J, 2002,10(1) :110-120．
[11] Lloyd J W, Binsaritti A, Salem O, et al. The groundwater assessment for the western Jamahiriya system well field[C].Libya. Proceedings of 30th International Geological Congress,1997,22:258-269． VSP.
[12] Simmers I.Recharge of phreatic aquifers in semi-arid areas[J].IAH Int Contrib Hydrogeol,1997,19:277．
[13] 籍传茂,王兆兴.地下水资源的可持续利用[M].北京:地质出版社.1999． 117-119．
[14] 陈望和,丁惠生,曾渊深.等.河北地下水[M].北京:地震出版社,1999． 184-196．
[15] 张光辉,费宇红,陈宗宇,等.海河流域平原深层地下水补给特征及其可利用性[J].地质论评,2002,48(6) :651-658．
[16] 张光辉,费宇红.李惠娣,等.海河流域平原浅层地下水位持续下降动因与效应[J].干旱区资源与环境,2002,16(2) :32-36
[17] 费宇红,陈树娥,刘克岩.滹沱河断流区水环境劣变特征与地下水调蓄潜力[J].水利学报,2001,(6) :41-44．
② 张光辉,等.太行山前平原动水条件下地下调蓄功能实验研究[R].石家庄:中国地质科学院水文地质环境地质研究所,2002．
[1] Ponce V M. Pandey R P, Kumar S. Groundwater recharge by channel infiltration in E1 Barbon basin Baja California [J].Mexico.J Hydrol,1999, 214:1-7．
[2] Scanlon B R. Water and heat fluxes in desert soils field studies [J].Water Resour Res,1994,30:709-719．
[3] Shentsis I, Meirovich L,Ben Zvi A,Rosenthal E. Assessment of transmission losses and groundwater recharge from runoff events in a wadi under shortage of data on lateral inflow[J].Negev.Israel. Hydrol Process,1999,13: 1649-1663．
[4] Sophocleous M. Interactions between groundwater and surface water:the state of science[J].Hydrogeology J, 2002,10(1) : 52-67．
[5] Bouwer H.Artificial recharge of groundwater:hydrogeology and engineering[J].Hydrogeology,2002,10(1) :121-142．
[6] de Vries J J, Simmers I.Groundwater recharge:an overview of processes and challenges[J].Hydrogeology J,2002,10(1) : 5-17．
[7] Healy R W, Cook P G. Using groundwater level. to estimate recharge [J].Hydrogeology J,2002,10(1) : 91-109．
[8] Bohlke J K.Groundwater recharge and agricultural contamination [J].Hydrogeology J,2002,10(1) :153-166．
[9] Gieske A S M. Dynamics of groundwater recharge:a case study in send-arid eastern Botswana [D].Vrije Universiteit.Amsterdam,1992． 289．
[10] Sanford W. Recharge and groundwater models:an overview [J].Hydrogeology J, 2002,10(1) :110-120．
[11] Lloyd J W, Binsaritti A, Salem O, et al. The groundwater assessment for the western Jamahiriya system well field[C].Libya. Proceedings of 30th International Geological Congress,1997,22:258-269． VSP.
[12] Simmers I.Recharge of phreatic aquifers in semi-arid areas[J].IAH Int Contrib Hydrogeol,1997,19:277．
[13] 籍传茂,王兆兴.地下水资源的可持续利用[M].北京:地质出版社.1999． 117-119．
[14] 陈望和,丁惠生,曾渊深.等.河北地下水[M].北京:地震出版社,1999． 184-196．
[15] 张光辉,费宇红,陈宗宇,等.海河流域平原深层地下水补给特征及其可利用性[J].地质论评,2002,48(6) :651-658．
[16] 张光辉,费宇红.李惠娣,等.海河流域平原浅层地下水位持续下降动因与效应[J].干旱区资源与环境,2002,16(2) :32-36
[17] 费宇红,陈树娥,刘克岩.滹沱河断流区水环境劣变特征与地下水调蓄潜力[J].水利学报,2001,(6) :41-44．
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