Wang Guo-Bing, Zhao Xiao-Long, Wang Ming-Hui, Ruan Hong-Hua, Xu Chang-Bai, Xu Ya-ming
Jiangsu Province Key Laboratory of Forestry and Ecological Engineering, Nanjing Forestry University, Nanjing 210037, China.
Ying Yong Sheng Tai Xue Bao. 2013 Apr;24(4):921-6.
Soil readily oxidizable carbon (ROC) is a sensitive index to indicate the early changes of soil organic carbon (SOC), and has important value to research the stability and dynamics of SOC pool under the backgrounds of human disturbance and global climate change. To further understand the effects of land use change on soil ROC, an investigation was conducted on the soil ROC content and related factors in four different land use types (grassland, farmland, poplar-agriculture system and pure poplar plantation) in a coastal area of northern Jiangsu Province, East China. The soil ROC content was in the order of grassland < farmland <c poplar-agriculture system < pure poplar plantation, and the difference was most significant in 0-10 cm soil layer. The ROC and ROC/SOC ratio decreased with increasing soil depth, and had significant differences between different soil layers in any one of the land use types. The soil ROC in the four different land use types had the same seasonal variation trend, with the maximum in summer, followed by in winter and autumn, and the minimum in spring. The soil ROC was significantly negatively correlated with soil pH and soil bulk density, positively correlated with SOC, soil water soluble organic carbon (WSOC), total nitrogen (TN), C/N ratio, and Mg, but less correlated with soil moisture and soil total phosphorus (TP). The results indicated that land use change had significant effects on the spatial distribution characteristics of soil ROC, and soil bulk density, pH value, TN, and SOC were the main factors inducing the differences of soil ROC content between different land use types.
土壤易氧化有机碳(ROC)是指示土壤有机碳(SOC)早期变化的敏感指标,对于研究人类干扰和全球气候变化背景下SOC库的稳定性及动态变化具有重要价值。为进一步了解土地利用变化对土壤ROC的影响,对中国东部江苏省北部沿海地区四种不同土地利用类型(草地、农田、杨农复合系统和纯杨树人工林)的土壤ROC含量及相关因素进行了调查。土壤ROC含量顺序为草地<农田<杨农复合系统<纯杨树人工林,在0-10厘米土层差异最为显著。ROC及ROC/SOC比值随土壤深度增加而降低,在任何一种土地利用类型的不同土层间均存在显著差异。四种不同土地利用类型的土壤ROC具有相同的季节变化趋势,夏季最高,其次是冬季和秋季,春季最低。土壤ROC与土壤pH值和土壤容重显著负相关,与SOC、土壤水溶性有机碳(WSOC)、全氮(TN)、C/N比及Mg显著正相关,但与土壤湿度和土壤总磷(TP)相关性较小。结果表明,土地利用变化对土壤ROC的空间分布特征有显著影响,土壤容重、pH值、TN和SOC是导致不同土地利用类型土壤ROC含量差异的主要因素。