巴丹吉林沙漠腹地盐湖碳酸盐同位素特征及其环境意义

doi:10.12118/j.issn.1000-6060.2024.288

Abstract

Abstract:

The formation of lake carbonate is closely associated with the physical and chemical properties of lake water and the climatic environment, serving as an essential carrier of lake environmental information. This study examines two types of carbonates (tufa and lake sediment carbonate) from six lakes in the hinterland of the Badain Jaran Desert, Inner Mongolia, China. The precipitation processes of these carbonates and their environmental implications were analyzed using stable carbon, oxygen, and clumped isotope (Δ₄₇) indices. The results indicate the following: (1) The carbon and oxygen isotope characteristics of tufas and lake sediment carbonates from the six lakes differ significantly, with the oxygen isotope values of tufa deposits being notably more negative than those of lake sediment carbonates. (2) The clumped isotope temperatures [T(Δ₄₇)] of lake sediment carbonates are consistent and approximate the regional summer temperature, whereas the T(Δ₄₇) of tufas are lower. (3) Based on oxygen isotope values and T(Δ₄₇), the estimated δ¹⁸O composition of the water in which the tufas precipitated suggests that the tufas capture a mixed signal from spring water and lake water. These findings provide preliminary insights into the environmental significance of salt lake carbonates in the hinterland of the Badain Jaran Desert and offer data to support long-term investigations into the hydrological evolution of desert lakes.

Key words: lake sediment carbonate, tufa, clumped isotope, Badain Jaran Desert

LI Quancong, LEI Guoliang, ZHAO Hui, ZHU Yun, SUN Wanting, YU Yuan, JIANG Geping. Isotopic characteristics of carbonate in salt lakes in the hinterland of Badain Jaran Desert and its environmental significance[J].Arid Land Geography, 2025, 48(2): 247-256.

Figures/Tables 7

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湖泊名称	经度/°E	纬度/°N	面积/km²	湖水pH值	地下水pH值	湖泊最大深度/m	水化学类型
呼都格吉林	102.37^[20]	39.82^[20]	0.43^[20]	9.63	7.11^[26]	6.30^[24]	Na-CO₃-Cl^[27]
呼和吉林	102.46^[20]	39.88^[20]	0.93^[20]	9.50	7.68^[28]	12.20^[24]	Na-CO₃-Cl^[27]
必鲁图	102.49^[20]	39.84^[20]	0.33^[20]	9.48	-	-	Na-CO₃-Cl^[27]
布尔特	102.27^[20]	39.84^[20]	0.24^[20]	9.61	9.19^[29]	-	Na-CO₃-Cl^[27]
苏木吉林	102.43^[20]	39.81^[20]	0.62^[20]	9.57	7.80^[23]	5.80^[24]	Na-CO₃-Cl^[27]
车日格勒	102.25^[20]	39.89^[20]	1.06^[20]	9.52	7.93^[26]	8.00^[24]	Na-CO₃-Cl^[27]

碳酸盐类型	湖泊名称	样品编号	测试加样量/mg	δ¹³C/‰	δ¹⁸O/‰	Δ₄₇/‰	Δ₄₇±1SE/‰	T(Δ₄₇)/℃	T(Δ₄₇)±1SE/℃	N
钙华	呼都格吉林	HDGJL-T	15	-7.81	-3.68	0.726	0.007	17.5	1.9	3
	呼和吉林	HHJL-T	15	-2.71	-1.53	0.725	0.002	17.7	0.6	3
	必鲁图	BLT-T	20	-1.54	-0.91	0.713	0.012	21.2	3.3	3
	布尔特	BET-T	15	0.45	-1.21	0.713	0.010	21.2	2.9	8
	苏木吉林	SMJL-T	20	-0.15	-0.45	0.714	0.011	20.8	3.1	7
	车日格勒	CRGL-T	12	1.68	-0.86	0.710	0.005	22.0	1.5	3
湖泊沉积物碳酸盐	呼都格吉林	HDGJL-S	77	-2.24	-1.42	0.672	0.005	33.9	1.6	4
	呼和吉林	HHJL-S	80	-0.38	-0.64	0.688	0.006	28.7	1.9	3
	必鲁图	BLT-S	65	-0.75	-0.18	0.686	0.023	29.3	7.0	3
	布尔特	BET-S	70	0.57	-0.16	0.697	0.015	25.9	4.5	4
	苏木吉林	SMJL-S	70	-1.41	0.47	0.697	0.007	25.8	2.2	3
	车日格勒	CRGL-S	95	-0.70	-0.65	0.704	0.005	23.8	1.5	4

Isotopic characteristics of carbonate in salt lakes in the hinterland of Badain Jaran Desert and its environmental significance

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