ZHAO Meng-jie, CHEN Yun-ming, AI Ze-min, et al. Distribution Characteristics of Soil Organic Carbon and Their Affecting Factors of Typical Plantations in Loess Hilly Region[J]. Bulletin of Soiland Water Conservation, 2013, 32(2): 270-275.
ZHAO Meng-jie, CHEN Yun-ming, AI Ze-min, et al. Distribution Characteristics of Soil Organic Carbon and Their Affecting Factors of Typical Plantations in Loess Hilly Region[J]. Bulletin of Soiland Water Conservation, 2013, 32(2): 270-275.DOI:
In order to understand the effects of different plantation types on soil organic carbon accumulation
we conducted a comparative analysis on the variations in the total amount and distribution characteristics ofsoil organic content in the 0-60cm soil layers of typical plantations of Robinia pseudoacacia
Hippophaerhamnoides
Caragana intermediain the loess hilly region.The results showed that the plantations playedpositive roles in soil organic carbon accumulation.After reaching their stable growth stages
the plantationsshowed replenishment effects on the soil organic carbon pool.The replenishment ability of the plantationscould be ranked in a decending order as Hippophae rhamnoides>Robinia pseudoacada>Caragana intermedia
with average annual replenishment rates of 0.854
0.004and 0.003g
respectively.Owing to thedifferences in root growth distribution
the replenishment rates varied vertically for different plantations.Under the plantation of Hippophae rhamnoides
the increase of soil carbon mainly occurred at the 20-40cmlayer with an annual replenishment rate of 0.357g
while for Robinia pseudoacada and Caragana intermedia
the increases were found at the layers of 40-60cm with rates of 0.010and 0.005g/kg
respectively.Moreover
the results also indicated significant correlation between soil physical properties and soil organiccontent(p<0.01);the soil organic content decreased with increasing soil bulk density and increased with aggregate stability.This suggested that the soil organic carbon storage capacity was affected by the soil physical properties
which in turn could be changed by vegetation root activities.