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Stoichiometric patterns of soil carbon, nitrogen, and phosphorus in farmland of the Poyang Lake region in Southern China

机译:中国南方the阳湖区农田土壤碳,氮,磷的化学计量比

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Purpose Previous studies have reported the occurrence of a Redfield-type ratio (e.g., C/N/P, C/N, C/P, or N/P) between C, N, and P concentrations in marine and (in part) terrestrial ecosystems. Herein, we aimed to determine whether a similar Redfield-type ratio can occur in farmland soil, as well as to elucidate how the C, N, and P ratios change with farmland-use types, soil physicochemical properties, and environmental factors. Materials and methods The stoichiometric patterns of soil C, N, and P in farmland were analyzed based on 6150 samples (0-20 cm) collected in 2012 by the Soil Testing and Formulated Fertilization Project in the Poyang Lake region of Southern China. Results and discussion The average soil C/N/P ratio in farmland of the study region was 98.4:16:1, which was slightly lower than the Redfield ratio of 106:16:1. There was no significant correlation between the concentrations of C, N, and P, indicating the absence of Redfield-type C/N/P, C/P, and N/P ratios. In contrast, the correlation between the concentrations of C and N was significant, indicating the presence of a stable Redfield-type C/N ratio in farmland soil. The average soil C/N, C/P, and N/P ratios corresponding to various farmland-use types showed significant differences (p < 0.01). In addition, all three ratios showed significant correlation with the latitude, soil pH, and mean annual precipitation. Conclusions There are no stable Redfield-type C/N/P, C/P, and N/P ratios while a stable Redfield-type C/N ratio exists in farmland soil in the Poyang Lake region. We urgently need to carry out ecological control experiments and field fertilization observations to understand the relationship between the stability of soil elements and fertilizer application in farmland.
机译:目的先前的研究报告了海洋和(部分)海洋中的C,N和P浓度之间存在Redfield型比率(例如C / N / P,C / N,C / P或N / P)。陆地生态系统。本文中,我们旨在确定农田土壤中是否可能出现类似的Redfield型比率,并阐明C,N和P比率如何随农田用途类型,土壤理化性质和环境因素而变化。材料和方法基于2012年南方Testing阳湖地区土壤试验与配方施肥项目收集的6150个样品(0-20厘米),分析了农田土壤C,N和P的化学计量模式。结果与讨论该研究区农田的平均土壤C / N / P比为98.4:16:1,略低于Redfield比值106:16:1。 C,N和P的浓度之间无显着相关性,表明不存在Redfield型C / N / P,C / P和N / P比。相反,C和N浓度之间的相关性很显着,表明农田土壤中存在稳定的Redfield型C / N比。对应于各种农田利用类型的平均土壤碳氮比,碳磷比和氮磷比显示出显着差异(p <0.01)。此外,这三个比率均与纬度,土壤pH和年平均降水量呈显着相关。结论the阳湖地区农田土壤中没有稳定的Redfield型C / N / P,C / P和N / P比,而稳定的Redfield型C / N比却存在。我们迫切需要进行生态控制实验和田间施肥观察,以了解土壤元素的稳定性与农田施肥之间的关系。

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