LIU Weiyi, FAN Shaohui, LIU Xizhen, et al. Spatiotemporal Changes of Soil Water Content Under Different Types of Phyllostachys Edulis Forests in Northern Fujian Province[J]. Bulletin of Soiland Water Conservation, 2015, 35(4): 59-63.
DOI:
LIU Weiyi, FAN Shaohui, LIU Xizhen, et al. Spatiotemporal Changes of Soil Water Content Under Different Types of Phyllostachys Edulis Forests in Northern Fujian Province[J]. Bulletin of Soiland Water Conservation, 2015, 35(4): 59-63. DOI: 10.13961/j.cnki.stbctb.2015.04.013.
Spatiotemporal Changes of Soil Water Content Under Different Types of Phyllostachys Edulis Forests in Northern Fujian Province
[Objective] The temporal and spatial variation of soil moisture was revealed under different bamboo forest stands in order to provide the scientific basis for the sustainable management of Phyllostachys edulis forests. [Methods] Based on the field test
three typical P. edulis forests(P. edulis and Cunninghamia lanceolata mixed forest
P. edulis pure forest and P. edulis and broad-leaved tree mixed forest) in northern Fujian Province were investigated in comparison with C. lanceolata pure forest and evergreen broadleaved forest. [Results] The seasonal changes of soil moisture content were consistent with the rainfall and evaporation. Monthly average soil moisture content ranged from 22.98% to 37.88%
and broad-leaved tree mixed forest had the largest mean annual soil moisture content of 31.95%
and followed by P. edulis and C. lanceolata mixed forest
P. edulis and broad-leaved tree mixed forest
C. lanceolata pure forest and P. edulis pure forest(30.46%
30.10%
29.78
and 29.31%
respectively). The moisture contents of different soil layers of evergreen broadleaved forest had significant differences(p<0.01) in the soil profiles
and the soil moisture contents decreased with soil depth
however
the moisture contents of other forest types had no significant differences in the soil profile. [Conclusion] The impacts of forest types and soil depth on soil moisture contents were different
but did not reach significant levels
and the precipitation in the forest canopy was the direct factor influencing soil moisture contents.
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Related Institution
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