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基于长期有机质实验中大规模生物学特性的淋溶土特征分析

Characterisation of Luvisols Based on Wide-Scale Biological Properties in a Long-Term Organic Matter Experiment.

作者信息

Kotroczó Zsolt, Fekete István, Juhos Katalin, Prettl Nándor, Nugroho Priyo Adi, Várbíró Gábor, Biró Borbála, Kocsis Tamás

机构信息

Department of Agro-Environmental Studies, Hungarian University of Agriculture and Life Sciences, H-1118 Budapest, Hungary.

Institute of Environmental Science, University of Nyíregyháza, H-4400 Nyíregyháza, Hungary.

出版信息

Biology (Basel). 2023 Jun 25;12(7):909. doi: 10.3390/biology12070909.

Abstract

Soil organic matter is a biological system that functions as an integrated whole. These assemblies have different properties, functions, and decomposition times. SOM is one of the main determinants of soil productivity. Our studies were carried out in a temperate deciduous oak forest on Luvisols soil. In the DIRT Project (Detritus Input and Removal Treatments), the following treatments were applied: Double Litter, Double Wood, Control, No Litter, No Root and No Input. Our objective was to compare the effect of withdrawal or doubling of organic matter on the protein pattern of the soil and the biological activity and changes in labile C (permanganate-oxidizable carbon) content in a long-term organic matter manipulation experiment. Patterns of thermostable proteins, soil dehydrogenase enzyme activity, CO emission, and POXC content were measured at the most biologically active soil depth of 0-5 cm after 23 years of treatment. Our results show that the enzyme activities of the litter removal treatments were significantly reduced compared to the doubling treatments, as were the values of soil respiration. The same significant difference was also detected in the C content of the soils of the treatments. Based on cluster analysis of the protein profile of the soil samples, the No Litter and No Input treatments were significantly different from the other treatments. This shows that specific organic matter is needed to enhance soil biological activity and the associated POXC content.

摘要

土壤有机质是一个作为整体发挥功能的生物系统。这些组合具有不同的性质、功能和分解时间。土壤有机质是土壤生产力的主要决定因素之一。我们的研究在淋溶土上的温带落叶栎林中进行。在“碎屑输入与去除处理”(DIRT项目)中,采用了以下处理方式:双倍凋落物、双倍木材、对照、无凋落物、无根和无输入。我们的目标是在一项长期的有机质操纵实验中,比较去除或加倍有机质对土壤蛋白质模式、生物活性以及不稳定碳(高锰酸盐可氧化碳)含量变化的影响。在处理23年后,于最具生物活性的0至5厘米土壤深度处测量了热稳定蛋白质模式、土壤脱氢酶活性、二氧化碳排放和高锰酸盐可氧化碳含量。我们的结果表明,与加倍处理相比,去除凋落物处理的酶活性显著降低,土壤呼吸值也是如此。在各处理土壤的碳含量中也检测到了同样的显著差异。基于对土壤样品蛋白质谱的聚类分析,无凋落物和无输入处理与其他处理有显著差异。这表明需要特定的有机质来提高土壤生物活性和相关的高锰酸盐可氧化碳含量。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8fa7/10376200/e2f00853dca3/biology-12-00909-g001.jpg

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