中文关键词计量土壤学土壤养分底土土壤剖面土壤发生分类土壤环境因子 英文关键词pedometricssoil nutrientssubsoilsoil profilesoil classificationsoil-environmental factor

作者	单位	E-mail
宋佳龄	湖南农业大学资源环境学院, 长沙 410128	songjialing17@stu.hunau.edu.cn
盛浩	湖南农业大学土壤研究所, 长沙 410128	shenghao82@hunau.edu.cn
周萍	中国科学院亚热带农业生态研究所亚热带农业生态过程重点实验室, 长沙 410125
段良霞	湖南农业大学资源环境学院, 长沙 410128
周清	湖南农业大学资源环境学院, 长沙 410128
张杨珠	湖南农业大学土壤研究所, 长沙 410128

中文摘要 为了解稻田土壤中是否存在稳定的土壤有机碳（C）、氮（N）和磷（P）比值，基于亚热带区110个水稻土剖面和587个发生层的土壤调查数据库，在区域尺度上分析了典型水稻土C：N：P比值的生态化学计量学特征，并应用相关分析和冗余分析，研究水稻土C：N：P比值与土壤-环境因子（地形和母质、土壤发生层、土壤类型和土壤理化性质）的关系.结果显示，亚热带区稻田土壤C：N、C：P和N：P的剖面加权平均值分别为12.6、49和3.9，C：N：P为38：3.2：1.不同母质起源、不同土壤亚类和不同发生层的水稻土C：N变异相对较小；但C：P和N：P的变异很大，两者均值也远低于全球（186和13.1）和中国土壤（136和9.3）的C：P和N：P的平均水平.尽管稻田土壤剖面的C：N：P相对不稳定，但由于稻田表土生物与环境相互作用强烈，表土C：N相对稳定（14.2）.这反映长期水耕熟化作用下，稻田表土中C和N仍存在紧密的耦合作用.然而，在稻田土壤剖面上，C：P和N：P并不稳定，SOC与全P含量、全N与全P含量也无显著相关性，表明环境变化可能导致土壤C：N：P解耦.地形、土壤质地、氧化铁和容重是调控稻田土壤剖面C：N：P的关键土壤环境因子. 英文摘要 This study aims to understand the existence of stable soil organic carbon (C), nitrogen (N), and phosphorus (P) ratios in paddy soil. Based on a field soil survey database, the ecological stoichiometry of the C:N:P ratio of 110 subtropical paddy soil profiles and 587 genetic horizons were analyzed at a regional scale. Relevant analysis and redundancy analysis (RDA) are used to study the relationships between C:N:P ratios and soil-environmental factors (topography, parent materials, soil genetic horizons, soil groups, soil physical, and chemical properties). The results showed that the weighted averages of C:N, C:P, and N:P in paddy soils of subtropical regions were 12.6, 49, and 3.9, respectively, and C:N:P was 38:3.2:1. The C:N of paddy soil did not vary significantly with parent materials, soil groups, or genetic horizons. However, the C:P and N:P variations were significantly different, and the mean values of the two were much lower than global ratios (186 and 13.1) and average levels of C:P and N:P in Chinese soils (136 and 9.3). Although the C:N:P ratio in the paddy soil profile was relatively unstable, the topsoil C:N (14.2) was relatively stable due to the strong interaction between the topsoil and the environment. This reflects the close coupling of C and N in the topsoil of paddy fields under long-term anthrostagnic maturation. However, in the paddy soil profile, C:P and N:P were not stable, and there was no significant correlation between soil organic carbon (SOC) and total P content, total N, or total P content, which suggests that environmental changes may lead to soil C:N:P decoupling. It was found that topography, soil texture, iron oxide, and bulk density are all key soil-environmental factors that regulate the soil profile of rice paddy C:N:P.

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