Study on surface water and groundwater interaction of Shaliu River Basin in Qinghai Lake in different periods

Yi-zhen LEI; Sheng-kui CAO; Guang-chao CAO; Yu-fan YANG; Yao LAN; Yu-tong JI; Hua-fei LI

doi:10.31497/zrzyxb.20201017

Journal of Natural Resources, Volume. 35, Issue 10, 2528(2020)

Study on surface water and groundwater interaction of Shaliu River Basin in Qinghai Lake in different periods

Yi-zhen LEI^1,2, Sheng-kui CAO^1,2、*, Guang-chao CAO^1,2, Yu-fan YANG^1,2, Yao LAN^1,2, Yu-tong JI^1,2, and Hua-fei LI^1,2

Author Affiliations

¹College of Geographical Sciences, Qinghai Normal University, Xining 810008, China

²Qinghai Provincial Key Laboratory of Physical Geography and Environmental Processes, Xining 810008, China

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Figures & Tables(7)

Fig. 1. The stratigraphic distribution and sampling point distribution of the Shaliu River Basin

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Fig. 2. The variations of monthly average air temperature, precipitation and runoff in Shaliu River Basin in 2018

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Fig. 3. The relationships between δD and δ¹⁸O of different water bodies in Shaliu River Basin in different periods

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Fig. 4. The relationships of recharge between surface water and groundwater in Shaliu River Basin in different periods

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Table 1. The δD and δ¹⁸O values of different water bodies of alpine steppe zone in Shaliu River Basin in different periods

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Table 1. The δD and δ¹⁸O values of different water bodies of alpine steppe zone in Shaliu River Basin in different periods

水体	月份	n	δD/‰			δ¹⁸O/‰
水体	月份	n	min	mean/SE	max	min	mean/SE	max
降水	4月	4	-64.40	-37.94/23.10	-8.84	-10.78	-6.96/2.73	-4.30
	8月	5	-77.34	-69.95/7.36	-59.46	-11.62	-10.52/0.91	-9.46
	11月	5	-129.59	-100.59/17.00	-87.41	-18.14	-15.13/1.75	-13.79
河水	4月	12	-43.59	-37.85/3.02	-34.67	-7.27	-6.34/0.45	-5.83
	8月	15	-54.80	-45.12/3.99	-40.36	-9.63	-8.78/0.60	-6.68
	11月	14	-48.96	-44.03/2.20	-41.52	-8.13	-7.46/038	-7.02
地下水	4月	21	-45.30	-39.70/4.43	-23.91	-7.15	-6.46/0.49	-5.07
	8月	23	-50.34	-40.93/3.31	-36.68	-7.96	-6.61/0.48	-5.84
	11月	25	-55.53	-45.83/5.37	-36.18	-10.21	-8.27/1.47	-6.07

Table 2. The δD and δ¹⁸O values of different water bodies of alpine meadow zone in Shaliu River Basin in different periods

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Table 2. The δD and δ¹⁸O values of different water bodies of alpine meadow zone in Shaliu River Basin in different periods

水体	月份	n	δD/‰			δ¹⁸O/‰
水体	月份	n	min	mean/SE	max	min	mean/SE	max
降水	4月	2	-18.21	-13.84/6.19	-9.46	-4.37	-4.15/0.32	-3.92
	8月	3	-81.83	-76.18/6.31	-69.36	-12.79	-11.60/1.06	-10.78
	11月	2	-100.31	-95.01/7.50	-89.70	-15.38	-14.64/1.06	-13.89
河水	4月	22	-59.37	-41.86/6.35	-26.78	-9.47	-7.01/1.27	-5.28
	8月	21	-57.06	-48.10/4.04	-40.12	-9.47	-7.88/0.81	-6.74
	11月	21	-53.15	-46.87/4.00	-35.30	-8.79	-7.97/0.71	-6.46
地下水	4月	19	-50.38	-41.09/4.29	-34.37	-8.26	-6.82/0.69	-5.90
	8月	18	-47.71	-40.54/3.85	-33.86	-7.86	-6.63/0.63	-5.80
	11月	20	-51.11	-42.66/4.53	-35.83	-8.34	-7.11/0.70	-5.93

Table 3. The proportions of recharge between surface water and groundwater (%)

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Table 3. The proportions of recharge between surface water and groundwater (%)

时期	区域	地表水补给地下水		地下水补给地表水
时期	区域	比例	不确定性	比例	不确定性
消融期	高山草原带	80.65	24.29	—	—
消融期	高山草甸带	93.36	130.14	—	—
多雨期	高山草原带	—	—	44.50	19.61
多雨期	高山草甸带	—	—	74.85	18.50
冰冻期	高山草原带	89.44	16.09	—	—
冰冻期	高山草甸带	—	—	88.58	24.07

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Yi-zhen LEI, Sheng-kui CAO, Guang-chao CAO, Yu-fan YANG, Yao LAN, Yu-tong JI, Hua-fei LI. Study on surface water and groundwater interaction of Shaliu River Basin in Qinghai Lake in different periods[J]. Journal of Natural Resources, 2020, 35(10): 2528

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Paper Information

Received: Apr. 20, 2019

Accepted: --

Published Online: Apr. 21, 2021

The Author Email: CAO Sheng-kui (caoshengkui@163.com)

DOI:10.31497/zrzyxb.20201017

Topics

Resource Economy

Research Articles

Table 1. The δD and δ18O values of different water bodies of alpine steppe zone in Shaliu River Basin in different periods

Table 1. The δD and δ18O values of different water bodies of alpine steppe zone in Shaliu River Basin in different periods

Table 2. The δD and δ18O values of different water bodies of alpine meadow zone in Shaliu River Basin in different periods

Table 2. The δD and δ18O values of different water bodies of alpine meadow zone in Shaliu River Basin in different periods

Table 3. The proportions of recharge between surface water and groundwater (%)

Table 3. The proportions of recharge between surface water and groundwater (%)

Table 1. The δD and δ¹⁸O values of different water bodies of alpine steppe zone in Shaliu River Basin in different periods

Table 1. The δD and δ¹⁸O values of different water bodies of alpine steppe zone in Shaliu River Basin in different periods

Table 2. The δD and δ¹⁸O values of different water bodies of alpine meadow zone in Shaliu River Basin in different periods

Table 2. The δD and δ¹⁸O values of different water bodies of alpine meadow zone in Shaliu River Basin in different periods