AI Chat Paper
Note: Please note that the following content is generated by AMiner AI. SciOpen does not take any responsibility related to this content.
{{lang === 'zh_CN' ? '文章概述' : 'Summary'}}
{{lang === 'en_US' ? '中' : 'Eng'}}
Chat more with AI
PDF (20.8 MB)
Collect
Submit Manuscript AI Chat Paper
Show Outline
Outline
Show full outline
Hide outline
Outline
Show full outline
Hide outline

Migration of total chromium and chloride anion in the Rocha River used for estimating degradation of agricultural soil quality at the Thiu Rancho zone

Jhim Terrazas-Salvatierra1( )Galo Munoz-Vásquez1Ana Romero-Jaldin2
Hydraulics Laboratory of San SimȮn University (UMSS), Cochabamba 2500, Bolivia
Water and Environmental Sanitation Center of San SimȮn University (UMSS), Cochabamba 2500, Bolivia
Show Author Information

Abstract

The Rocha River is a receptor to receive wastewater from household, hospital and industry, from where contaminants are transported in the river, affecting biodiversity and the ecosystem of the area. In this paper we estimated the maximum transport of total chromium and chloride anion by applying the analytical model of Ogata & Banks (1961), and the results obtained are grouped into three zones: Contaminated, transition, and uncontaminated. The analytical model was applied with 13 samples collected from the river piezometers installed near Rocha, where they are arranged in two lines, i.e. RH-1 to RH-6 as the first line and RH-9 to RH-12 as the second line. The total chromium concentrations range from 0.16 mg/L (RH-1) and 0.11 mg/L (RH-9) at the closest points to Rocha River, to 0.13 mg/L (RH-7) and 0.03 mg/L (RH-12) at the most remote points to the river. The advance of the pollutants does not exceed 50 meters with respect to the axis of the Rocha River.

References

 

Anderson MP. 1979. Using models to simulate the movement of contaminates through groundwater flow system. CRC Critical Reviews in Environmental Control, 9(2): 97-156.

 

Crank J. 1956. The mathematics of diffusion. New York: Oxford University Press.

 

Dundar MS, Altundag H. 2006. Investigation of heavy metal contaminations in the lower Sakarya river water and sediments. Sakarya University, Environmental Monitoring Assess-ment, 128: 177-181.

 

Faust CR, Mercer JW. 1980. Groundwater modeling: Recent developments. Ground Water, 18(6): 569-77.

 
Fetter CW. 2001. Applied hydrogeology. Fourth Edition. Prentice-Hall.
 
Fetter CW. 1999. Contaminant hydrogeology. Second Edition. Prentice-Hall.
 
Fetter CW. 1994. Applied hydrogeology. Third Edition. Prentice-Hall.
 

Fetter CW. 1977. Attenuation of waste water elutriated through glacial outwash. Ground Water, 15(5): 365-371.

 

HUANG Yong, WANG Ping, FU Zhi-min, et al. 2019. Experimental and numerical research on migration of LNAPL contaminants in fractured porous media. Hydrogeology Journal, 28: 1269-1284. https://doi.org/10.1007/s10040-020-02118-w

 
Hvorslev MJ. 1951. Time lag and soil permeability in ground water observations. U.S. Army Corps of Engineers Water-way Experi-mentation Station, Bulletin 36.
 

Kavouri KP, Karatzas GP, Plagnes V. 2017. A coupled groundwater flow-modelling and vulnerability-mapping methodology for karstic terrain management. Hydrogeology Journal, 25(5): 1301-1317. https://doi.org/10.1007/s10040-017-1548-6

 
LI An, Tsai FTC, Yuill BT, et al. 2020. A three-dimensional stratigraphic model of the Mississippi River Delta, USA: Implications for river deltaic hydrogeology. Hydrogeology Journal. https://doi.org/10.1007/s10040-020-02198-8
 

Maldonado M, Van Damme P, Rojas J. 1998. Pollution and eutrophication in the Rocha river basin. Bolivian Journal of Ecology and Environmental, 3: 3-9.

 

Malott S, O'Carroll DM, Robinson CE. 2016. Dynamic groundwater flows and geochemistry in a sandy nearshore aquifer over a wave event. Water Resource Research, 52(7): 5248-5264. https://doi.org/10.1002/2015wr017537

 
Ogata A. 1970. Theory of dispersion in a granular medium. U.S. Geological Survey Professional Paper 411-I.
 
Ogata A, Banks RB. 1961. Solution of the differential equation of longitudinal dispersion in porous media. US. Geological Survey Professional Paper 411-A.
 
Prickett TA, Naymik CT, Lonnquist CG. 1981. A "random walk" solute transport model for selected ground-water quality evaluations. Illinois State Water Survey, Bulletin 65: 103. http://hdl.handle.net/2142/94526
 

Romero AM, Vandecasteele C, Cooreman H. 2000. Metals (Cr, Pb, and Zn) in sediments and chironomids of the Rocha river. Bolivian Jour-nal of Ecology and Environmental, 8: 37-47.

 

Sefelnasr A, Gossel W, Wycisk P. 2014. Three-dimensional groundwater flow modeling approach for the groundwater management options for the Dakhla Oasis, Western Desert, Egypt. Environmental Earth Sciences, 72(4): 12227-122241. https://doi.org/10.1007/s12665-013-3041-4

 

Sookhak LK, Johnston CD, Rayner JL, et al. 2018. Field-scale multi-phase LNAPL remediation: Validating a new computational framework against sequential field pilot trials. Journal of Hazard Material, 345: 87-96.https://doi.org/10.1016/j.jhazmat.2017.11.006

 

Sookhak LK, Rayner JL, Davis GB. 2018b. Towards characterizing LNAPL remediation endpoints. J Environ Manag, 224: 97-105. https://doi.org/10.1016/j.jenvman.2018.07.041

 

Sookhak LK, Davis GB, Rayner JL, et al. 2019a. Natural source zone depletion of LNAPL: A critical review supporting modelling appro-aches. Water Resource Research, 157: 630-646.https://doi.org/10.1016/j.watres.2019.04.001

 

Sookhak LK, Rayner JL, Davis GB. 2019b. Toward optimizing LNAPL remediation. Water Resour Research, 55(2): 923-936. https://doi.org/10.1029/2018wr023380

 

Srinivasan P, Mercer JW. 1988. Simulation of biodegradation and sorption processes in ground wáter. Ground Water, 26(4): 475-487.

 
Terrazas J. 2018. Potential non-point pollution index (PNPI) in the Rocha Basin. San Simón University (UMSS). http://hdl.handle.net/123456789/10984
Journal of Groundwater Science and Engineering
Pages 223-229
Cite this article:
Terrazas-Salvatierra J, Munoz-Vásquez G, Romero-Jaldin A. Migration of total chromium and chloride anion in the Rocha River used for estimating degradation of agricultural soil quality at the Thiu Rancho zone. Journal of Groundwater Science and Engineering, 2020, 8(3): 223-229. https://doi.org/10.19637/j.cnki.2305-7068.2020.03.003

330

Views

7

Downloads

0

Crossref

2

Web of Science

2

Scopus

Altmetrics

Received: 06 November 2019
Accepted: 19 February 2020
Published: 28 September 2020
© 2020 Journal of Groundwater Science and Engineering Editorial Office
Return