Changes of Soil Organic Carbon in Various Stages of Vegetation Restoration in Ziwuling Mountain
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Changes of Soil Organic Carbon in Various Stages of Vegetation Restoration in Ziwuling Mountain
Bulletin of Soiland Water ConservationVol. 30, Issue 3, Pages: 94-98(2011)
作者机构:
1. 中国科学院 水利部水土保持研究所,陕西 杨凌,712100
2. 西北农林科技大学水土保持研究所,陕西 杨凌 7121003
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Published:2011
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MA Shuai, ZHAO Shi-wei, LI Ting, et al. Changes of Soil Organic Carbon in Various Stages of Vegetation Restoration in Ziwuling Mountain[J]. Bulletin of Soiland Water Conservation, 2011, 30(3): 94-98.
DOI:
MA Shuai, ZHAO Shi-wei, LI Ting, et al. Changes of Soil Organic Carbon in Various Stages of Vegetation Restoration in Ziwuling Mountain[J]. Bulletin of Soiland Water Conservation, 2011, 30(3): 94-98.DOI:
Changes of Soil Organic Carbon in Various Stages of Vegetation Restoration in Ziwuling Mountain
and organic carbon contribution rates of variously sized soil aggregates were studied during vegetation restoration in Ziwuling Mountain. The results show that the weighted mean of SOC was 3. 54 g/kg for the 0-100cm soil profile of sloped cropland
while the weighted means of SOC of 0-100cm soil profiles of abandoned land
grassland
shrub and arbor phases were 6.8%
36.6%
41.5% and 73.6%
respectively
higher than that of slop cropland. T he increasing magnitudes of SOC contents of 0-20 cm soil layer were higher than those of soil layers below following vegetation restoration.The SOC contents of aggregates of all sizes in the 0-5 and 5-10cm soil layers increased gradually and the SOC enriched in the macroaggregates(>2mm) over time along with vegetation restoration. No clear change of SOC contents in the 10-20 cm soil layer for aggregates of all sizes. The SOC contribution rates of>5
5~ 2 and 2~ 1mm aggregates in 0-20 cm soil layer of abandoned land
grassland
shrub and arbor were higher than that of sloped cropland
indicating that the increased part of SOC in 0-20 cm soil layer were stored mainly in>1mm aggregates during vegetation restoration.