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Chinese Journal of Applied Ecology ›› 2021, Vol. 32 ›› Issue (7): 2347-2354.doi: 10.13287/j.1001-9332.202107.023

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Effects of thinning intensity on the understory water-holding capacity of Pinus sylvestris var. mongolica plantation in the Bashang area of north China

WU Xue-ming1, YU Xin-xiao1,2*, CHEN Li-hua1,2, JIA Guo-dong1,2, QIU Yun-xiao1, PENG Xiu-wen1   

  1. 1College of Water and Soil Conservation, Beijing Forestry University, Beijing 100083, China;
    2Key Laboratory of Soil and Water Conservation and Desertification Combating, Ministry of Education, Beijing 100083, China
  • Received:2021-01-01 Revised:2021-03-14 Online:2021-07-15 Published:2022-01-15
  • Contact: *yuxinxiao@bjfu.edu.cn
  • Supported by:
    National Key R&D Program of China (2016Y FC0500802).

Abstract: The complex terrain and poor climatic conditions in Bashang area of Hebei Province result in water and soil loss and geological disasters, which pose a serious threat to ecological safety in North China. In order to improve local environmental quality, barren-resistant and fast-growing tree species such as Pinus sylvestris var. mongolica and Larix gmelinii are planted with large areas. However, unreasonable plantation density will lead to inefficient utilization of rainfall and intensify the conflict between forest and water. In this study, we analyzed the effects of five thinning intensities (0, 20%, 40%, 60%, 80%) of P. sylvestris var. mongolica plantation on herbs, litter, soil and overall water-holding capacity, with the aim to provide scientific basis for management of P. sylvestris var. mongolica. The results showed that water-holding rate of herb varied from 47.7% to 90.7%, and that the water-holding capacity of herb decreased with increasing thinning intensity. When the thinning intensity was less than 40%, water-holding capacity decreased slowly, and then decreased rapidly. With the increase of thinning intensity, natural water-holding rate and maximum water-holding rate of undecomposed layer and semi-decomposed layer decreased gradually, with the effective water-holding rate being 60%>40%>20%>80%>0, and the water-holding capacity of semi-decomposed layer being better than that of undecomposed layer. The water-holding capacity of soil decreased gradually with the increases of thinning intensity. Thinning intensity less than 40% promoted water holding capacity. Under different thinning intensities, the total water-holding rate of understory was 8.3%-14.3%, with an order of 20%>0>40%>60%>80%. In view of understory all layers and overall changes, the thinning intensity at 20% in the study area could effectively improve the understory water-holding capacity and achieve better ecological benefits.

Key words: thinning intensity, Pinus sylvestris var. mongolica, water-holding capacity, understory structure, stand density