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砒砂岩区主要造林树种枯落物及林下土壤持水特性

杨振奇 秦富仓 李晓琴 刘力川 牛晓乐

水土保持学报2017,Vol.31Issue(3):118-122,5.
水土保持学报2017,Vol.31Issue(3):118-122,5.DOI:10.13870/j.cnki.stbcxb.2017.03.021

砒砂岩区主要造林树种枯落物及林下土壤持水特性

Water-Holding Characteristics of Litters and Soil Under Major Afforestation Tree Species in the Feldspathic Sandstone Region

杨振奇 1秦富仓 1李晓琴 1刘力川 1牛晓乐1

作者信息

  • 1. 内蒙古农业大学沙漠治理学院,呼和浩特010019
  • 折叠

摘要

Abstract

To investigate the hydrological function of different afforestation tree species in the feldspathic sandstone region,we selected Pinus tabuli formis,Platycladus orientalis,Populus cathayana,Prunus armeniaca,Hippophae rhamnoides and Caragana korshinskii from the area to analyze and compare the waterholding capacity in the litter layer and soil layer of different tree species by the soaking method and ring sampling method.Our results demonstrated that the litter accumulation variation range of the major afforestation tree species in the feldspathic sandstone region was 1.55-7.89 t/hm2,and Populus cathayana forest litter exhibited the highest maximum water holding capacity,i.e.281.26%,followed by Pinus tabuliformis (217.14%),Platycladus orientalis (201.05%),Prunus armeniaca (202.79%),Hippophae rhamnoides (170.96%),Caragana korshinskii (158.08%),and abandoned land (143.88%).For the soil layer under the Pinus tabuliformis forest,the smallest bulk density was 1.46 g/cm3,the maximum porosity and capillary porosity was 43.55% and 36.99%,respectively,with the maximum capillary moisture capacity being 14.50 mm.For the soil under Prunus armeniaca forest,the maximum non-capillary porosity was 13.12%,and the maximum non-capillary moisture capacity was 6.86 mm.The water-holding capacity of both the litter layer of Pinus tabuliformis and the under-forest soil layer was great.Therefore,Pinus tabuliformis is more suitable for vegetation construction in the feldspathic sandstone region.

关键词

砒砂岩区/枯落物/林下土壤/持水特性

Key words

feldspathic sandstone region/litter/soil/water-holding characteristics

分类

农业科技

引用本文复制引用

杨振奇,秦富仓,李晓琴,刘力川,牛晓乐..砒砂岩区主要造林树种枯落物及林下土壤持水特性[J].水土保持学报,2017,31(3):118-122,5.

水土保持学报

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