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1)  Tianshuihai Lake core
甜水海钻孔
1.
Based on a R / S analysis of FeO,Fe2O3 and ratio of FeO/ Fe2O3 from Tianshuihai Lake core, which is scaled with time, it is found that there are obvious Hurst effect with Hurst indexes of 0.
运用R/S分析法,对经过等时处理的甜水海钻孔氧化铁3项指标FeO、Fe2O3及其比值FeO/Fe2O3进行了分析计算,其指标都存在明显的Hurst现象,Hurst指数H分别为:Fe2O3为0。
2)  Tianshuihai microcontinent
甜水海块
3)  Tianshuihai Lake
甜水海
1.
Non-linear Analyses of Some Geochemical Indexes of Tianshuihai Lake Core TS95 and Their Implications;
甜水海钻孔TS95若干地球化学指标的非线性分析与意义
2.
Palynological Evidence of Ecological Environment Change Since 240 ka BP for the Tianshuihai Lake, West Kunlun Mountains;
西昆仑山甜水海24万年以来生态环境演化的孢粉学证据
3.
A lake core ,located at 100 m to the southeast of the Tianshuihai Lake (35°21 N, 79°25 ,E, 4 840 m asl) on the southern flank of the west Kunlun Mountains,was drilled in July of 1995.
为探讨青藏高原演化过程,在高原西北部甜水海湖盆地区进行了钻探,井深56。
4)  Tianshuihai Basin
甜水海盆地
5)  Tianshuihai Group Complex
甜水海岩群
1.
The Qingbaikouan stromatolites from the Tianshuihai Group Complex in the Karakorum region, Xinjiang;
新疆喀喇昆仑地区甜水海岩群发现青白口纪叠层石
6)  Lake Tianshuihai
甜水海湖泊
补充资料:冷凝甜水
分子式:
CAS号:

性质:粗甘油蒸馏制取精甘油的过程中,甘油蒸汽被多组串联起来的冷凝器冷凝,最前面的冷凝器温度较高所得甘油浓度和纯度均高,随后冷凝器温度逐步下降,所得甘油浓度也逐步降低,到最后的冷凝器冷凝温度在100℃以下。最后这部分冷凝液中甘油含量很低,称为冷凝甜水。冷凝甜水并入甘油蒸发器的进料。

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