青藏高原盐湖有关水样地球化学测试数据集(2024)
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该数据包括了2024年6-8月份青藏高原考察期间在蓬错、巴木错、班戈错、阿木错、恰岗错、毕洛错、才多茶卡、鄂雅错、其香错、瀑赛尔错、果根错、尕阿错、杜佳里湖、果普克、赤日错、错弄却、念灯纳布错、错温布、塔瓦卡勒错、错果果、母底错、洞古错、拉昂错、玛旁雍错、佩枯错、错戢龙、扎西措、昆楚克错、把拉、喀湖错、勒玛擦、查木错、别塘、阿鲁错、四家湖、美马错、芒错、窝尔巴错、马头湖、兽形湖、邦达错、普尔错及月牙湖共43个湖泊所采水样的酸碱度、盐度、基本阴阳离子及铷和铯的地球化学数据,每个湖泊采集水样若干且不低于2件,共计169件样品。测试元素主要包括K、Na、Ga、Mg、Cl、Li、Br、B2O3、CO3、SO4、HCO3、Rb及Cs共计13种元素含量数据,以g/L或mg/L表示。样品测试分析工作均在中国地质科学院矿产资源研究所自然资源部成矿作用与资源评价重点实验室完成。其中K(检出限:4.5ug/L)、Na(6.36 ug/L)、Ca(6.61ug/L)、Mg(1.94 ug/L)、B2O3(1.25ug/L)、Li(0.33ug/L)、Rb(0.04ug/L)、Cs(0.03ug/L)测定采用电感耦合等离子体质谱法,所测样品相对偏差≤20%,Cl(0.007mg/L)、Br(0.016mg/L)、SO4(0.018mg/L)测定采样离子色谱法,所测样品相对偏差≤10%,CO3与HCO3测定采用盐酸滴定法测定。所测数据对于查明西藏盐湖资源储量现状、进行远景评估及开发利用具有重要意义。
This dataset comprises geochemical data including pH value, salinity, major anions and cations, rubidium (Rb) and cesium (Cs) from water samples collected from 43 lakes during the field survey on the Qinghai-Tibet Plateau from June to August 2024. The 43 lakes are Pengcuo, Bamucuo, Banggucuo, Amucuo, Qiagangcuo, Biluocuo, Caiduochaka, Eyacuo, Qixiangcuo, Pusaiercuo, Guogencuo, Ga'acuo, Duijiali Lake, Guopuke, Chirikucuo, Cuonongque, Niandengnabucuo, Cuowenbu, Tawakalecuo, Cuoguoguo, Mudicuo, Donggucuo, Lagancuo, Mapamyumco, Peikuco, Cuojilong, Zhaxicuo, Kunchukucuo, Bala, Kahucuo, Lemaca, Chamcuo, Bietang, Alucuohu, Sijiahu, Meimacuohu, Mangcuo, Wobacuo, Matouhu, Shouxinghu, Bangdacuohu, Puercuo and Yueyahu. A total of 169 water samples were collected, with no fewer than 2 samples obtained from each individual lake. The contents of 13 targeted elements, namely K, Na, Ga, Mg, Cl, Li, Br, B₂O₃, CO₃²⁻, SO₄²⁻, HCO₃⁻, Rb and Cs, were measured, with the units reported in g/L or mg/L. All sample testing and analytical work were completed at the Key Laboratory of Mineralization and Resource Assessment, Ministry of Natural Resources, Institute of Mineral Resources, Chinese Academy of Geological Sciences. For K (detection limit: 4.5 μg/L), Na (6.36 μg/L), Ca (6.61 μg/L), Mg (1.94 μg/L), B₂O₃ (1.25 μg/L), Li (0.33 μg/L), Rb (0.04 μg/L) and Cs (0.03 μg/L), inductively coupled plasma mass spectrometry (ICP-MS) was adopted, with the relative deviation of all tested samples ≤ 20%. For Cl (detection limit: 0.007 mg/L), Br (0.016 mg/L) and SO₄²⁻ (0.018 mg/L), ion chromatography was used, with the relative deviation ≤ 10%. CO₃²⁻ and HCO₃⁻ were determined via hydrochloric acid titration. The measured data are of great significance for clarifying the current reserves of salt lake resources in Tibet, conducting prospective resource assessment and facilitating their development and utilization.




