溶滤和蒸发作用是内陆干旱盆地平原区松散沉积层地下水咸化的主要原因。
Lixiviation and evaporation are main salinization processes of groundwater stored in loose sediments in inland arid basins.
地下水长期超采诱发了地面沉降、海(咸)水入侵等地质灾害，并呈加剧趋势。
For a long time overexploitation of groundwater, land subsidence and seawater intrusion and other geological disasters were induced and development tendency of geological disasters became serious.
硫酸根离子呈现北低南高分带性可能与地下水流动与大陆咸化作用有关。
The sulfate radical ion shows hight in south and low in north is possible relate with the ground water flows and the mainland salty function.
阿拉尔地区地下水矿化度含量高、水咸，地表水也随季节变化时咸时淡。
Subterranean water in Alar area is salty, with high total salinity, and surface water becomes less salty or saltier with seasonal rhythm.
阿拉尔地区地下水矿化度含量高、水咸，地表水也随季节变化时咸时淡。
Subterranean water in Alar area is salty, with high total salinity, and surface water becomes less salty or saltier with seasonal rhythm.
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