Luo You-lin, Li Qi-quan, Wang Chang-quan, Zhang Wei, Zhang Hao, Li Lin-xian, Chen Jun-wei, Ma Yu
Ying Yong Sheng Tai Xue Bao. 2015 Jan;26(1):177-85.
Spatial distribution characteristics of soil C/N ratio and its affecting factors at a county scale in hilly area of Middle Sichuan Basin were analyzed based on field sampling. Result indicated that soil C/N ranged from 4.84 to 21.79, with a mean value of 11.93. The coefficient of variation was 26.3%; which suggested soil C/N had moderate variability in this study area. The ratio of nugget to sill was 73.0%, which suggested the spatial variability of soil C/N was determined by both structural and random factors, and the random factors played a more important role. The soil C/N was higher in northeast and southwest while the central part of the study area was characterized by relatively lower values of soil C/N. The soil C/N ranged from 10.0 to 13.5 in most parts of the study area. Parent material, soil type, topographic factors and land use type had significant impacts on soil C/N (P<0.05). Soil C/N showed a significant positive correlation with elevation and slope (P<0.05). The soil parent materials were able to explain 8.7% of soil C/N spatial variability. The explanatory power of soil group, subgroup and soil genus were 3.8%, 5.0%, 8.7%, respectively. Topographic factors showed the lowest explanatory power of only 0. 8%. However, land use type could explain 23.9% of the spatial variability, which suggested that land use type was the dominant factor in controlling the spatial variability of soil C/N.
基于野外采样,分析了四川盆地中部丘陵区某县域尺度土壤碳氮比的空间分布特征及其影响因素。结果表明,土壤碳氮比范围为4.84至21.79,平均值为11.93。变异系数为26.3%,表明该研究区域土壤碳氮比具有中等变异性。块金值与基台值之比为73.0%,表明土壤碳氮比的空间变异性由结构因素和随机因素共同决定,且随机因素起更重要作用。研究区域东北部和西南部土壤碳氮比更高,而中部土壤碳氮比相对较低。研究区域大部分地区土壤碳氮比在10.0至13.5之间。成土母质、土壤类型、地形因素和土地利用类型对土壤碳氮比有显著影响(P<0.05)。土壤碳氮比与海拔和坡度呈显著正相关(P<0.05)。土壤母质能够解释土壤碳氮比空间变异性的8.7%。土类、亚类和土属的解释力分别为3.8%、5.0%、8.7%。地形因素的解释力最低,仅为0.8%。然而,土地利用类型能够解释23.9%的空间变异性,表明土地利用类型是控制土壤碳氮比空间变异性的主导因素。