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黄河下游典型湿地土壤养分及生态化学计量特征

[Nutrients and Ecological Stoichiometry Characteristics of Typical Wetland Soils in the Lower Yellow River].

作者信息

Wang Chuan-Ying, Wang Kai-Yue, Wang Hao-Ran, Zhang Meng-di, Zhou Yun-Kai

机构信息

College of Geography and Environmental Science, Henan University, Kaifeng 475004, China.

Key Laboratory of Geospatial Technology for the Middle and Lower Yellow River Regions, Ministry of Education, Henan University, Kaifeng 475004, China.

出版信息

Huan Jing Ke Xue. 2024 Mar 8;45(3):1674-1683. doi: 10.13227/j.hjkx.202304064.

Abstract

Carbon, nitrogen, phosphorus, and potassium in the soil are the necessary nutrient elements for plant growth, and their contents and ecological stoichiometry can reflect the status of soil quality and nutrient limitation. The Huayuankou Yellow River Floating Bridge Wetland in the lower Yellow River was selected as the research object. The methods of ANOVA, redundancy analysis, and linear regression fitting were used to study the contents of organic carbon (SOC), total nitrogen (TN), total phosphorus (TP), total potassium (TK), alkaline nitrogen (AN), available phosphorus (AP), available potassium (AK), and their ecological stoichiometric ratios as well as the limiting elements of soil nutrients, and the key physicochemical properties that affect soil nutrients and their ecological stoichiometry in the wetland were revealed. The results showed that the mean values of (SOC), (TN), (TP), (TK), (AN), (AP), and (AK) in wetland soil were 5.46 g·kg, 0.60 g·kg, 0.28 g·kg, 17.06 g·kg, 13.75 mg·kg, 6.54 mg·kg, and 158.56 mg·kg, respectively, which showed an increasing trend from the river bank to the shoaly land and were generally higher at the high vegetation coverage areas than at the low vegetation coverage areas. There were significant correlations among SOC, TN, TP, and TK. Soil C/P, C/K, N/P, and N/K showed a consistent trend with soil nutrients, whereas C/N showed the opposite. The coefficients of variation of SOC, TN, AN, N/P, and N/K in the soil exceeded 50.00%, with significant spatial differences. The average value of C/N in wetland soil was 11.882, which was close to the average level of soils in China, whereas the average values of C/P and N/P were 49.119 and 4.516, respectively, both of which were lower than the average level of soils in China, and the N/P of soil was far less than 14, which indicated that N was limited in the soil. The proportion of clay and electrical conductivity combined to explain 61.4% and 43.9% of the variation in the soil nutrients and their ecological stoichiometry, respectively, which were the dominant soil physicochemical properties affecting the soil nutrients and their ecological stoichiometry of Huayuankou Yellow River Floating Bridge Wetland. The research results are helpful to improve our knowledge of nutrients and their influencing factors in the wetland soil of the lower Yellow River and provide an important scientific basis for the ecological restoration and management of the wetland in the lower Yellow River.

摘要

土壤中的碳、氮、磷和钾是植物生长必需的营养元素,其含量及生态化学计量比能够反映土壤质量状况和养分限制情况。选取黄河下游的花园口黄河浮桥湿地作为研究对象,采用方差分析、冗余分析和线性回归拟合等方法,研究了有机碳(SOC)、全氮(TN)、全磷(TP)、全钾(TK)、碱解氮(AN)、有效磷(AP)、速效钾(AK)的含量及其生态化学计量比以及土壤养分限制元素,揭示了湿地中影响土壤养分及其生态化学计量比的关键理化性质。结果表明,湿地土壤中(SOC)、(TN)、(TP)、(TK)、(AN)、(AP)和(AK)的平均值分别为5.46 g·kg、0.60 g·kg、0.28 g·kg、17.06 g·kg、13.75 mg·kg、6.54 mg·kg和158.56 mg·kg,呈现出从河岸向浅滩陆地递增的趋势,且在高植被覆盖区域总体高于低植被覆盖区域。SOC、TN、TP和TK之间存在显著相关性。土壤C/P、C/K、N/P和N/K与土壤养分呈现一致趋势,而C/N则相反。土壤中SOC、TN、AN、N/P和N/K的变异系数超过50.00%,存在显著的空间差异。湿地土壤C/N的平均值为11.882,接近中国土壤的平均水平,而C/P和N/P的平均值分别为49.119和4.516,均低于中国土壤的平均水平,且土壤N/P远小于14,表明土壤中氮素受限。黏粒比例和电导率分别解释了土壤养分及其生态化学计量比变异的61.4%和43.9%,是影响花园口黄河浮桥湿地土壤养分及其生态化学计量比的主要土壤理化性质。研究结果有助于增进我们对黄河下游湿地土壤养分及其影响因素的认识,为黄河下游湿地的生态恢复与管理提供重要的科学依据。

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