Ecosystem N:P stoichiometric ratios determine the catchment surface water N:P ratio through subsurface hydrological processes

被引:21
作者
Liu, Ji [1 ,2 ,3 ]
Wang, Yi [1 ,2 ]
Li, Yong [1 ,2 ]
Liu, Xinliang [1 ,2 ]
Jiang, Yuexi [1 ,2 ]
Fu, Yuxi [1 ,2 ,3 ]
Jin, Wenbo [1 ,2 ,4 ]
Wu, Jinshui [1 ,2 ,3 ]
机构
[1] Chinese Acad Sci, Inst Subtrop Agr, Key Lab Agroecol Proc Subtrop Reg, Changsha 410125, Peoples R China
[2] Chinese Acad Sci, Inst Subtrop Agr, Changsha Res Stn Agr & Environm Monitoring, Changsha 410125, Peoples R China
[3] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[4] Shenzhen Municipal Shenshan Management Bur, Ecol Environm Bur, Shenzhen 518200, Peoples R China
基金
中国国家自然科学基金;
关键词
Overland flow; Groundwater; Water quality; Tea plantation; Masson pine forest; subtropical China; SOIL ORGANIC-CARBON; LAND-USE TYPES; RICE AGRICULTURE; OVERLAND-FLOW; GROUNDWATER DISCHARGE; TOTAL NITROGEN; LOESS PLATEAU; NUTRIENT; PHOSPHORUS; LOSSES;
D O I
10.1016/j.catena.2020.104740
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
An imbalanced surface water N:P (nitrogen:phosphorus) stoichiometric ratio degrades aquatic ecological and environmental functions. Although it is known that the N and P balance and hydrological processes in terrestrial ecosystems affect the surface water N:P ratio, how these factors regulate surface water N:P ratios remains unclear. Here, the N:P ratios in the nutrient budgets, soil, overland flow, groundwater, and surface water in two comparable tea and forest ecosystems and catchments were observed during the 2015-2017 period to link the hydrological processes with the surface water N:P ratio. The results suggested that although the N:P ratio of the nutrients released into the soil-water system was 1.84 times greater in the tea ecosystem than in the forest ecosystem, the soil N:P ratio (5 vs. 10 mol mol(-1)) was lower in the tea ecosystem, probably due to soil N and P decoupling processes associated with tea field establishment. The overland flow N:P ratios of the tea and forest ecosystems (30 and 28 mol mol(-1), respectively) were similar and were mainly affected by surface hydrological processes. The groundwater N:P ratios were higher in the tea ecosystem than in the forest ecosystem (245 vs. 86 mol mol(-1)), indicating more intense soil N leaching than P leaching in the tea ecosystem. An ecosystem releases excessive N through the groundwater process, which contributes to the stability of the soil N:P ratio. It is estimated that the groundwater N:P ratio contributed more than the overland flow N:P ratio to the surface water N:P ratio (31.5-58.6% vs. 0.1-0.7%), which highlights the importance of the groundwater N:P ratio and subsurface hydrological processes for regulating the surface water N:P ratio in catchments. Therefore, to reduce the environmental risk posed by an unbalanced surface water N:P ratio in tea-growing regions, NP fertilizer application must be improved, and NP leaching should be minimized.
引用
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页数:10
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