Groundwater Salinization and Freshening Processes in the Luy River Coastal Aquifer, Vietnam

被引:9
作者
Dieu, Linh Pham [1 ,2 ]
Cong-Thi, Diep [1 ,2 ]
Segers, Tom [1 ]
Ho, Huu Hieu [2 ]
Nguyen, Frederic [3 ,4 ]
Hermans, Thomas [1 ]
机构
[1] Univ Ghent, Dept Geol, Lab Appl Geol & Hydrogeol, Krijgslaan 281-S8, B-9000 Ghent, Belgium
[2] Vietnam Inst Geosci & Mineral Resources VIGM, Hanoi 100000, Vietnam
[3] Univ Liege, Urban & Environm Engn Res Unit, Allee Decouverte 9, B-4000 Liege, Belgium
[4] Katholieke Univ Leuven, Dept Earth & Environm Sci Geol, Celestijnenlaan 200e bus 2411, B-3001 Leuven, Belgium
关键词
hydrochemistry; freshening; saltwater intrusion; coastal aquifer; SEA-WATER INTRUSION; SEAWATER INTRUSION; HFE-DIAGRAM; IDENTIFY; DELTA; PLAIN; AUSTRALIA; TRANSPORT; SALINITY; FLANDERS;
D O I
10.3390/w14152358
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The Vietnamese Binh Thuan province located along the Southern Central part of the coast is one of the driest in the country. The population is relying largely on groundwater for irrigation, and the groundwater resources are threatened by climate change and saltwater intrusion in river estuaries. Recent studies, however, reveal that the extension of saltwater intrusions was larger than expected, raising some doubts on the actual origin of the intrusions. In this study, we use the geochemical characterization of groundwater samples collected in both the dry and rainy seasons in the Luy river coastal area to identify hydrochemical processes responsible for the salinization and variations taking place in the shallow aquifers. The distribution of chemical components of groundwater and the indicators presenting the freshening and salinization processes, such as cation exchange code and chloride conservative element, the ionic delta, the HFE-diagram, and geochemical modelling, were studied. The results show that 65% of the samples exceed the WHO limit for drinking water and 100% of them have a degree of restriction on use from slight-moderate to severe in potential irrigation problems according to FAO. In contrast to previous expectations, freshening is the dominant process in the aquifers, and it is more advanced in the rainy season. Due to a lack of recharge and aquifer exploitation, salinization is more severe in the deeper aquifer and during the dry season. Saltwater intrusion is not limited to the zone close to the river but extends further inland and at depth, and salinity can vary quickly over short distances. Based on these new insights, we develop a new conceptual model for the evolution of salinization in the Luy river catchment involving a natural freshening process of connate water combined with anthropic influence. The conceptual model will form the basis for the development of a groundwater model of the study area and eventually lead to sustainable management scenarios for this coastal region, preventing further deterioration of the groundwater resources.
引用
收藏
页数:27
相关论文
共 69 条
[1]   Using the Cl/Br ratio as a tracer to identify the origin of salinity in aquifers in Spain and Portugal [J].
Alcala, Francisco J. ;
Custodio, Emilio .
JOURNAL OF HYDROLOGY, 2008, 359 (1-2) :189-207
[2]   Geochemical processes and solute transport at the seawater/freshwater interface of a sandy aquifer [J].
Andersen, MS ;
Jakobsen, VNR ;
Postma, D .
GEOCHIMICA ET COSMOCHIMICA ACTA, 2005, 69 (16) :3979-3994
[3]  
[Anonymous], 2013, SALTWATER INTRUSION
[4]  
[Anonymous], 2018, NAWAPI GROUNDW RES B
[5]  
[Anonymous], 2015, NAWAPI GROUNDW RES B
[6]  
Antonellini M, 2015, HYDROGEOL J, V23, P1009, DOI 10.1007/s10040-015-1263-0
[8]  
Appelo CAJ., 2005, GEOCHEMISTRY GROUNDW, V2
[9]  
Ayers R.S., 1985, Water quality for agriculture. FAO Irrigation and drainage paper 29 Rev. 1
[10]  
Barlow PM, 2010, HYDROGEOL J, V18, P247, DOI 10.1007/s10040-009-0514-3