LI Zhanbin, ZHOU Bo, MA Tiantian, et al. Effects of Ecological Management on Characteristics of Soil Carbon, Nitrogen, Phosphorus and Their Stoichiometry in Loess Hilly Region, China[J]. 2017, 31(6): 312-318.
DOI:
LI Zhanbin, ZHOU Bo, MA Tiantian, et al. Effects of Ecological Management on Characteristics of Soil Carbon, Nitrogen, Phosphorus and Their Stoichiometry in Loess Hilly Region, China[J]. 2017, 31(6): 312-318. DOI: 10.13870/j.cnki.stbcxb.2017.06.049.
Effects of Ecological Management on Characteristics of Soil Carbon, Nitrogen, Phosphorus and Their Stoichiometry in Loess Hilly Region, China
In order to explore the effects of different ecological management measures on soil carbon (C)
nitrogen (N)
phosphorus (P) content and their stoichiometry characteristics
thus to provide scientific evidence for ecological management and vegetation restoration of loess hilly region
by combining the means of field sampling and laboratory analysis
Wangmaogou which was the typical watershed in loess hilly region was taken as an example in this study
and the soil C
N and P contents and their stoichiometry of the 0—100 cm soil layer of 5 kinds of sample plots (sloping farmland
woodland
shrub land
grassland and terrace land) were analyzed. The results showed that: (1) Transformed into woodland
shrub land
grassland and terrace land by ecological management measures
soil C and N contents of sloping farmland respectively increased by 1.27
1.18
1.24
1.14 times and 1.64
1.64
1.76
1.57 times; There were significant positive correlation between soil C and N. The vertical distribution of the soil C and N in the 0—100 cm soil profile of woodland
grassland
shrub land and terrace land were quite consistent
showing the same trend of decreasing with soil depth and both appearing enrichment phenomenon in the 0—20 cm soil layer
while soil P did not change much with soil depth. (2) Soil C∶N mean value of sloping farmland was significantly higher than that of other plots (P<0.05)
while the surface soil C∶P of sloping farmland was significantly lower than that of other plots (P<0.05). Soil C∶N did not change much
while soil C∶P and N∶P showed the trend of decreasing with soil depth. (3) The distribution of soil C
N and P stoichiometry was mainly determined by soil C and N. The correlations of soil C∶P
N∶P and ammonium nitrogen contents
soil clay contents
soil sand contents
soil water-stable aggregates were significant(P<0.05). Soil C
N
P contents and their stoichiometry were not only affected by ecological management and soil depth
but also were relevant to soil physical and chemical properties
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Related Author
CAO Yang
LIU Guangquan
XU Hao
HAN Xinsheng
ZHANG Fen-li
AN Shao-shan
YANG Jian-guo
DU Sheng
Related Institution
College of Forestry, Northwest A&F University, Yangling
China Institute of Water Resources and Hydropower Research, State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin
Institute of Forestry and Grassland Ecology, Ningxia Academy of Agriculture and Forestry Sciences, Ningxia Key Laboratory of Desertification Control and Soil and Water Conservation, Research Center for Ecological Restoration and Multi-Functional Forestry of Ningxia
Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling