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枣树弃耕时间对黄土高原土壤剖面性质和酶活性的影响。

Effect of jujube orchard abandonment time on soil properties and enzyme activities at soil profile in the Loess Plateau.

机构信息

College of Resources and Environment, Shanxi Agricultural University, Tailuo Ave 12, Taigu, 030801, China.

State Key Laboratory of Black Soils Conservation and Utilization, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, 4888 Shengbei Street, Changchun, 130012, China.

出版信息

Sci Rep. 2024 Aug 15;14(1):18943. doi: 10.1038/s41598-024-69794-6.

Abstract

In the Loess Plateau, the impact of abandoned farmland on soil properties and enzyme activity, along with its temporal variations and potential driving factors, remains a mystery. This study was designed to systematically and comprehensively examine the variations in soil enzyme activities, particle size distribution, and stability of soil aggregates at different stages of ecological recovery in the Loess Plateau. Our findings reveal a nuanced temporal pattern: with the progression of cropland abandonment, there is a notable decrease in soil bulk density. Concurrently, a dynamic trend in enzyme activities is observed-initially exhibiting a decline, followed by an increase over extended periods of recovery. Notably, prolonged abandonment leads to marked enhancements in soil structure. Parameters such as the mean weight diameter (MWD) and geometric mean diameter (GMD) of soil aggregates show an overall increasing trend. In terms of the Relative Dissipation Index (RSI), our data indicate a sequence of control > 2 years of abandonment > 4 years > 6 years > 14 years. From this, it can be seen that fallowing may be an effective natural restoration strategy for improving the physical structure of soils in the Loess Plateau and restoring soil nutrients. However, positive changes may take a long time to become evident.

摘要

在黄土高原,废弃农田对土壤性质和酶活性的影响及其时间变化和潜在驱动因素仍然是一个谜。本研究旨在系统全面地研究黄土高原生态恢复不同阶段土壤酶活性、粒径分布和土壤团聚体稳定性的变化。我们的研究结果揭示了一个微妙的时间模式:随着耕地的废弃,土壤容重明显下降。同时,酶活性呈现出动态趋势——最初下降,然后在较长时间的恢复过程中增加。值得注意的是,长时间的废弃导致土壤结构明显增强。土壤团聚体的平均重量直径(MWD)和几何平均直径(GMD)等参数表现出总体增加的趋势。就相对耗散指数(RSI)而言,我们的数据表明依次为对照>2 年撂荒>4 年>6 年>14 年。由此可见,休耕可能是改善黄土高原土壤物理结构和恢复土壤养分的有效自然恢复策略。然而,积极的变化可能需要很长时间才能显现出来。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/08c4/11327241/33e1a40f1b13/41598_2024_69794_Fig1_HTML.jpg

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