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Effects of soil salinity on the content, composition, and ion binding capacity of glomalin-related soil protein (GRSP)

机译:土壤盐分对gloomalin相关土壤蛋白(GRSP)的含量,组成和离子结合能力的影响

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Soil aggregation, an ecosystem function correlated with the concentration of glomalin-related soil protein (GRSP), is highly disturbed in saline soil. However, few studies have focused on differences in amount, composition, and ion binding capacity of GRSP in typical sodic-saline soils. In this study, a field study was performed in Songnen Plain. Combined indicators of soil salinity (Q value) were significant negatively correlated with GRSP concentration by Principal Component Analysis. Multiple linear regression models showed that soil salinity might account for 46%, 25% and 44% variation in total GRSP (T-GRSP), easily-extractable GRSP (EE-GRSP) and dif-ficultly-extractable GRSP (DE-GRSP), respectively. Soil bulk density had most important impact on GRSP concentration, followed by the pH, soil EC had the weak influence. Comparative analysis was carried out between low-salinity and high-salinity soil. Purified T-GRSP of high-saline soil contained higher N content (13.13%), lower C content (43.41%) and lower functional groups relative content (e.g. C-O and Si-O-Si). Purified T-GRSP of high-salinity soil had a greater binding capacity with calcium and phosphorus, the binding capacity could compensate the GRSP loss about 29.8% and 14.1%, respectively. Our findings suggested that sodic salinlzation of the soil led to a decrease in GRSP concentration and a change in the component percentages. This change in composition might be related to adaptation of fungi-plant systems to varied environments. The calcium and phosphorus binding capacity had a positive dependent of soil salinization, which was possible to develop ecological management or recovery technology in the future.
机译:土壤聚集是一种与胶草蛋白相关的土壤蛋白质(GRSP)浓度相关的生态系统功能,在盐渍土壤中受到严重干扰。但是,很少有研究集中在典型的钠盐土壤中GRSP的数量,组成和离子结合能力方面的差异。在这项研究中,在松嫩平原进行了实地研究。通过主成分分析,土壤盐分的综合指标(Q值)与GRSP浓度显着负相关。多元线性回归模型表明,土壤盐分可能占总GRSP(T-GRSP),易提取GRSP(EE-GRSP)和难提取GRSP(DE-GRSP)的46%,25%和44% , 分别。土壤容重对GRSP浓度影响最大,其次是pH值,土壤EC影响较弱。在低盐度和高盐度土壤之间进行了比较分析。高盐度土壤的纯化T-GRSP含有较高的N含量(13.13%),较低的C含量(43.41%)和较低的官能团相对含量(例如C-O和Si-O-Si)。高盐度土壤纯化的T-GRSP与钙和磷的结合能力更大,结合能力可以分别补偿GRSP的29.8%和14.1%的损失。我们的发现表明,土壤的钠盐碱化导致GRSP浓度降低和组分百分比变化。这种成分变化可能与真菌植物系统适应各种环境有关。钙磷结合能力与土壤盐渍化呈正相关关系,将来有可能发展生态管理或恢复技术。

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