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Volume 37 Issue 5
Oct.  2018
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DENG Yan, JIANG Zhongcheng, XU Ye, YUE Xiangfei, LI Xuyao, LIANG Jintao. Redistribution of precipitation by vegetation and its ecohydrological effects in a typical epikarst spring catchment[J]. CARSOLOGICA SINICA, 2018, 37(5): 714-721. doi: 10.11932/karst20180509
Citation: DENG Yan, JIANG Zhongcheng, XU Ye, YUE Xiangfei, LI Xuyao, LIANG Jintao. Redistribution of precipitation by vegetation and its ecohydrological effects in a typical epikarst spring catchment[J]. CARSOLOGICA SINICA, 2018, 37(5): 714-721. doi: 10.11932/karst20180509

Redistribution of precipitation by vegetation and its ecohydrological effects in a typical epikarst spring catchment

doi: 10.11932/karst20180509
  • Publish Date: 2018-10-25
  • Study of precipitation redistribution by vegetation and its effects on epi-karst water in southwest of China could guide the ecological protection and comprehensive development and utilization of karst water resources. Based on the analysis of the characteristics of two typical plants, this paper presents a study on this issue in a typical epikarst spring catchment, Southwest China. The results show that the through rainfall in Toona sinensis (S1) vegetation is 1,861.83 mm, accounting for 59.65% of the total precipitation. Through rainfall in Caesalpinia decapetala (S2) vegetation is 1,626.42 mm, accounting for 52.11% of the total precipitation. The through rainfall rate decreases with increasing precipitation. Stem flow in S1 is 89.4 mm, accounted for 2.86% of total precipitation. Stem flow in S2 was 27.79 mm, accounted for 0.89% of total precipitation. Interception storage in S1 and S2 are 1,169.97 mm and 1,466.99 mm, accounting for 37.48% and 47.01% of total rainfall, respectively. Using the water balance method, annual evapotransipiration in the Yaji typical epikarst spring catchment is 1,623.81 mm, accounting for 52.03% of the precipitation, and runoff depth is 1,497.39 mm, accounting for 47.97% of the precipitation. Canopy could change the precipitation recharge pattern and quantity to epi-karst zone. Precipitation is intercepted by canopy and partitioned into through rainfall and stem flow, while through rainfall supplements the epi-karst zone in a continuous wave-like manner. The vegetation interception can reduce the total supply of rainfall to the epi-karst zone, but increases the effective supply. Compared with Caesalpinia decapetala, Toona sinensis vegetation would increase the effective recharge to epikarst zone.

     

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