Seawater intrusion into groundwater and its impact on irrigation and agriculture: Evidence from the coastal region of West Bengal, India

被引:43
|
作者
Sarkar, Biplab [1 ]
Islam, Aznarul [1 ]
Majumder, Arijit [2 ]
机构
[1] Aliah Univ, Dept Geog, 17 Gorachand Rd, Kolkata 700014, India
[2] Jadavpur Univ, Dept Geog, Kolkata 700032, India
关键词
Irrigation hazards; Diastrophic process; Catastrophic process; Groundwater overexploitation; Coastal region; SEA-LEVEL RISE; SALTWATER INTRUSION; WATER INTRUSION; HYDROGEOCHEMICAL CHARACTERISTICS; AQUIFER SYSTEM; MAHANADI DELTA; TAMIL-NADU; SOUTH; VULNERABILITY; SALINIZATION;
D O I
10.1016/j.rsma.2021.101751
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
The present study aims to trace out the signatures of seawater intrusion into the groundwater and the irrigation hazards in the coastal region of West Bengal, India based on 56 groundwater samples. The result reveals that 48.21 % of the groundwater samples have exhibited the values of seawater mixing index greater than 1 indicating the effect of seawater mixing into the fresh groundwater. The electrical conductivity (EC) in the studied samples ranges from 338 to 4330 mu S/cm and as per the United States Salinity Laboratory (USSL) classification of EC for irrigation water quality, about 31% of samples come under medium (251-750 mu S/cm), 53% under high (751-2250 mu S/cm), and 16 % under very high (2251-5000 mu S/cm) salinity hazard classes. Besides, the potential salinity (PS) reveals that about 52 % of samples have high salinity problems while 16 % are moderately suitable (water may be used for medium to coarse-textured soils) and 32 % are suitable which can safely be used for fine and medium, and coarse-textured soils. The problem of salinity intrusion acts as a catalyst to impair agricultural practice. For example, the average yield of rice production is low (1.5-2.0 t ha(-1)) for South 24 Parganas compared to the neighbouring districts. The study finds that similar to 49 % of samples having Na+/Cl- ratio greater than 1 indicates that silicate weathering is the dominant process controlling groundwater hydro-chemistry and sodium concentration. Moreover, a higher sea-level rise (3.90 +/- 0.13 mm a(-1)), frequent storm surge (142 events of moderate to severe cyclone during 1582 to 1991) and overexploitation of groundwater and fall of piezometric level (e.g. 10.96 m in 1956-2005 at Gobra, Kolkata) are major driving forces of seawater intrusion. (C) 2021 Elsevier B.V. All rights reserved.
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页数:19
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