强降雨过程增加蔬菜种植区浅层地下水碳汇能力

高振朋; 肖春艳; 陈昊; 薛天; 曹莹; 范贺凯; 张东

doi:10.3799/dqkx.2023.201

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Gao Zhenpeng, Xiao Chunyan, Chen Hao, Xue Tian, Cao Ying, Fan Hekai, Zhang Dong, 2025. Heavy Rainfall Increasing Carbon Sink in Shallow Groundwater in Vegetable Growing Areas. Earth Science, 50(4): 1545-1558. doi: 10.3799/dqkx.2023.201

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Gao Zhenpeng, Xiao Chunyan, Chen Hao, Xue Tian, Cao Ying, Fan Hekai, Zhang Dong, 2025. Heavy Rainfall Increasing Carbon Sink in Shallow Groundwater in Vegetable Growing Areas. Earth Science, 50(4): 1545-1558. doi: 10.3799/dqkx.2023.201

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Heavy Rainfall Increasing Carbon Sink in Shallow Groundwater in Vegetable Growing Areas

doi: 10.3799/dqkx.2023.201

Gao Zhenpeng^{1
,
,},
Xiao Chunyan¹,
Chen Hao¹,
Xue Tian¹,
Cao Ying¹,
Fan Hekai¹,
Zhang Dong^{2
,
,
,}

1.
School of Resources and Environment, Henan Polytechnic University, Jiaozuo 454001, China
2.
College of Marine Science, Shanghai Ocean University, Shanghai 201306, China

Received Date: 2023-07-21
Available Online: 2025-05-10
Publish Date: 2025-04-25

Abstract

Abstract

In the backdrop of global climate change, the quest for effective methods to sequester atmospheric carbon dioxide (CO₂) is both urgent and indispensable. The acidifying substances generated by artificial inputs such as manure and chemical fertilizers in agricultural areas release more dissolved inorganic carbon (DIC) into shallow groundwater, altering the process of inorganic carbon cycling. However, the influence of heavy rain events on this process remains unclear. Shallow groundwater in a vegetable cultivation area in North Henan Province was selected as the primary research focus, while shallow groundwater samples from grain growing region and local deep groundwater samples were also collected in April and October 2021. The water chemistry composition, hydrogen and oxygen isotope compositions (δD_H₂O and δ¹⁸O_H₂O), and δ¹³C_DIC compositions were analyzed to investigate the influence of rainfall processes on inorganic carbon cycling in shallow groundwater of agricultural areas. The results show that heavy rainfall led to more anthropogenic pollutants entering groundwater under the vegetable cultivation areas during the rainy season, resulting in an increase in mean TDS values from 649 mg/L in April to 1 195 mg/L in October, and a decrease in average δ¹³C_DIC values from －12.25‰ to －14.14‰. The changes of mean TDS values and δ¹³C_DIC values in groundwater under the vegetable cultivation areas were larger than those in groundwater under other sites, displaying more organic matter had entered and decomposed in the shallow groundwater under the vegetable cultivation areas. The average DIC concentrations varied little from 7.78 mmol/L in April to 7.74 mmol/L in October, however, as groundwater table elevated about 11 to 15 m after heavy rainfall, it implied more DIC input and thereby obviously increased carbon sink capacity in shallow groundwater. This study confirms the impact of anthropogenic inputs in vegetable cultivation areas on DIC in shallow groundwater and verifies that heavy rainfall will transport more DIC into shallow groundwater and increasing more dissolved components, elevating carbon sink capability of groundwater.
- vegetable cultivation area,
- shallow groundwater,
- anthropogenic input,
- dissolved inorganic carbon,
- carbon isotope,
- carbon sink effect,
- geochemistry,
- hydrogeology

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Heavy Rainfall Increasing Carbon Sink in Shallow Groundwater in Vegetable Growing Areas

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