湖水矿化度即湖水含盐量。指一升湖水中所含各种盐类的总重量。
湖泊水质逐渐淡化，700年后湖水矿化度将达平衡浓度。
The water will gradually desalinate and the mineralization will tend to equilibrium concentration after 700 years.
利用将水体中的污染物作为保守物质的水质模型，通过数值模拟，计算得出的博斯腾湖湖水矿化度与实测资料基本吻合。
A water quality model considering pollutants as conservative materials is presented, and the numerical simulation results of salinity in Bosten Lake are found agreeable with the measured results.
不同的环流结构对入流与湖水混合程度有一定的影响，从而影响湖区的矿化度分布及泵站取水水质。
Different circulation structures have a definite effect on mixed degree between inflow and lake water, which influences mineral distributing of lake area and intake water quality of pumping stations.
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