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土壤改良剂对盐碱地稻田土壤有机质形态和稳定性的影响。

Effects of soil amendments on fractions and stability of soil organic matter in saline-alkaline paddy.

机构信息

College of Global Change and Earth System Science, Beijing Normal University, Beijing, 100875, China.

College of Global Change and Earth System Science, Beijing Normal University, Beijing, 100875, China; China (Shanghai) Pilot Free Trade Zone Lin-gang Special Area Administration, Shang Hai, 201306, China.

出版信息

J Environ Manage. 2021 Sep 15;294:112993. doi: 10.1016/j.jenvman.2021.112993. Epub 2021 Jun 10.

Abstract

Soil amelioration is an effective practice to alleviate the adverse effects of soil salinization. However, increasing the fertility of salt-affected soils has been challenging, particularly in coastal saline-alkaline paddy soils. Here, we carried out a 45-day incubation experiment to evaluate the impacts of soil amendments on fractions and stability of soil organic matter (SOM) in a saline-alkaline paddy. The experiment simulates the flooding-draining practice and consists of CaCO, gypsum and biochar amendments using different fertility soils. We measured dissolved organic carbon (DOC) and nitrogen (DON) in supernatant liquids, water-soluble cations, water extractable organic carbon (WEOC) and nitrogen (WEON), and microbial biomass carbon (MBC) and nitrogen (MBN) in soils after the incubation. Results showed that water soluble sodium (Na) was significantly decreased under all amendments (by 17%-32%), except in high fertility soil. We found a significant decrease in DOC (by 36%-47%) under gypsum treatment, but in DON (by 18%-59%) under biochar treatment. However, there was no significant effect on DOC or DON under CaCO treatment. Gypsum treatment led to decreased WEOC content (by 0.067%-5.4%), but increased MBC (by 0.16%-44%) and MBN (by 8.3%-37%) in all soils. Biochar treatment caused a decrease in the ratios of WEOC to soil organic carbon (SOC) and WEON to total nitrogen (TN), and an increase in MBC:SOC and MBN:TN ratios. These results suggest that gypsum and biochar amendments can enhance SOM stability in the saline-alkaline paddy. However, SOM stability was not enhanced under CaCO treatment, probably due to the presence of a large amount of Na in these soils. Our study highlights that soil amelioration has different effects on soil carbon and nitrogen cycles in the saline-alkaline paddy soils, which is associated with water-logged condition.

摘要

土壤改良是缓解土壤盐渍化不利影响的有效措施。然而,提高盐渍土壤的肥力一直具有挑战性,特别是在沿海盐碱性稻田土壤中。在这里,我们进行了为期 45 天的孵化实验,以评估土壤改良剂对盐碱性稻田土壤有机质(SOM)的形态和稳定性的影响。该实验模拟了淹水-排水过程,包括使用不同肥力土壤的碳酸钙、石膏和生物炭改良剂。我们测量了孵化后土壤中上清液中的溶解有机碳(DOC)和氮(DON)、水溶性阳离子、水可提取有机碳(WEOC)和氮(WEON)以及微生物生物量碳(MBC)和氮(MBN)。结果表明,除高肥力土壤外,所有改良剂均显著降低了水溶性钠(Na)(减少 17%-32%)。我们发现石膏处理下 DOC 显著减少(减少 36%-47%),但生物炭处理下 DON 显著减少(减少 18%-59%)。然而,碳酸钙处理对 DOC 或 DON 没有显著影响。石膏处理导致 WEOC 含量降低(降低 0.067%-5.4%),但所有土壤中的 MBC(增加 0.16%-44%)和 MBN(增加 8.3%-37%)均增加。生物炭处理导致 WEOC 与土壤有机碳(SOC)和 WEON 与总氮(TN)的比例降低,MBC:SOC 和 MBN:TN 比例增加。这些结果表明,石膏和生物炭改良剂可以增强盐碱性稻田土壤中 SOM 的稳定性。然而,碳酸钙处理并未增强 SOM 稳定性,这可能是由于这些土壤中存在大量的 Na。我们的研究强调了土壤改良对盐碱性稻田土壤碳氮循环的不同影响,这与淹水条件有关。

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