Evaluation on the River Seepage under Groundwater Pumping near Riverside

Article Preview

Abstract:

Abstract. Groundwater is to be pumping near the riverside could be induced recharge from the river surface and lateral aquifer layers, and could be reduced the negative effect on the aquifer. In this research, proposes the method of pumping groundwater from the Maoluo riverside and assesses the effect on the riverbank filtration in the middle of Taiwan. This research constructed the four analytical models using MODFLOW to identify the reliability of numerical model. Five groundwater pumping schemes based on the assessment on the effect of the Maoluo river seepage were implemented. For replace with the external water sources is 60,000 CMD, the ratio of river seepage to pumping is from 37.5% to 40.2%, and the groundwater radius of influence is from 290m to 470m. The research area is 700 m away from the residential area, none pumping schemes will thus affect the residential area.

You might also be interested in these eBooks

Info:

Periodical:

Pages:

383-390

Citation:

Online since:

October 2012

Export:

Price:

[1] Bochever F.M.: Evaluation of well-field yield in alluvial aquifers: The impact of a partially penetrating stream [C]. Proceedings of VODGEO (Hydrogeology) 13: 84-115. (1966).

Google Scholar

[2] Butler J.J., Zlotnik V.A., Tsou M.S.: Drawdown and stream depletion produced by pumping in the vicinity of a partially penetrating stream. Ground Water 39(5): 651- 659. (2001).

DOI: 10.1111/j.1745-6584.2001.tb02354.x

Google Scholar

[3] Central Geological Survey, MOEA, information on http: /www. moeacgs. gov. tw/ (2006).

Google Scholar

[4] Chen W.P., Lee C.H.: Estimating ground-water recharge from stream flow records. Environ Geol 44: 257-265. (2003).

Google Scholar

[5] Chen J.W., Pan W.J., Lee C.H.: The groundwater of safe yield in Chou-Shui alluvial fan and Pingtung plane, Taiwan. Taiwan Water Conservancy 50(3): 70-82 (2002), in Chinese.

Google Scholar

[6] Chen J.W., Hsieh H.H., Yeh H.F. and Lee C.H.: The Effect of the Variation of River Water Level on the Estimation Groundwater Recharge in Hsinhuwei River, Taiwan, Environ Geol. DOI: 10. 1007/s12665-009-0117-2. (2009).

DOI: 10.1007/s12665-009-0117-2

Google Scholar

[7] Chen X.H., Yin Y.: Semianalytical solution for stream depletion in partially penetrating streams. Ground Water 42(1): 92-96. (2004).

DOI: 10.1111/j.1745-6584.2004.tb02454.x

Google Scholar

[8] Chen X., Chen X.: Effect of aquifer anisotropic on the migration of lnfiltrated stream water to a pumping well. J Hydrol Eng 8(5): 287-293. (2003).

DOI: 10.1061/(asce)1084-0699(2003)8:5(287)

Google Scholar

[9] Glover R.E., Balmer C.G.: River depletion from pumping a well near a river. American Geophysical Union Transactions 35(3): 468-470. (1954).

DOI: 10.1029/tr035i003p00468

Google Scholar

[9] Grigoryev V.M.: The effect of streambed siltation on well-field yield in alluvial aquifers. Water Supply and Sanitation 6: 110-118. (1957).

Google Scholar

[10] Hantush M.S.: Wells near streams with semipervious beds. J Geophysical Research 70(12): 2829-2838. (1965).

DOI: 10.1029/jz070i012p02829

Google Scholar

[11] Hsieh H.H., Chen J.W., Lee C.H.: Analysis the quantity and quality of ground water for the riverside area. Water Supply Quarterly 26(3): 1-10 (2007), in Chinese.

Google Scholar

[12] Hunt B.: Unsteady stream depletion from ground water pumping. Ground Water 37(1): 98-102. (1999).

DOI: 10.1111/j.1745-6584.1999.tb00962.x

Google Scholar

[13] Jenkins C.T.: Techniques for computing rate and volume of stream depoetion by well. Ground Water 6(2): 37-46. (1968).

Google Scholar

[14] Lee C.H., Chen W.P., Lee C.H.: Estimation of groundwater recharge using water balance coupled with base-flow-record estimation and stable-base-flow analysis. Environ Geol 51(1): 73-82. (2006).

DOI: 10.1007/s00254-006-0305-2

Google Scholar

[15] Matteo L.D., Dragoni W.: Empirical relationships for estimating stream depletion by a well pumping near a gaining stream. Ground Water 43(2): 242-249. (2005).

DOI: 10.1111/j.1745-6584.2005.0006.x

Google Scholar

[16] Theis C.V.: The effect of a well on the flow of a nearby stream. American Geophysical Union Transactions 22(3): 734-738. (1941).

DOI: 10.1029/tr022i003p00734

Google Scholar

[17] Water Resources Agency, Ministry of Economic Affairs, information on http: /gweb. wra. gov. tw/ (2007).

Google Scholar

[18] Wilson J.L.: Induced infiltration in aquifer with ambient flow. Water Resour Res 29(10): 3503-3512. (1993).

DOI: 10.1029/93wr01393

Google Scholar

[19] Xue Y.: Ground water dynamics theorem. Geology publisher, Beijing (1986), in Chinese.

Google Scholar