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生物炭和水炭的施用影响盐碱土中的土壤氨挥发和溶解有机物。

Biochar and hydrochar application influence soil ammonia volatilization and the dissolved organic matter in salt-affected soils.

作者信息

Ma Yaxin, Xie Wenping, Yao Rongjiang, Feng Yanfang, Wang Xiangping, Xie Huifang, Feng Yuanyuan, Yang Jingsong

机构信息

Jiangsu Key Laboratory of Chemical Pollution Control and Resources Reuse, School of Environmental and Biological Engineering, Nanjing University of Science and Technology, Nanjing 210094, China.

State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, CAS, Nanjing 210008, China.

出版信息

Sci Total Environ. 2024 May 20;926:171845. doi: 10.1016/j.scitotenv.2024.171845. Epub 2024 Mar 21.

Abstract

Biochar, which including pyrochar (PBC) and hydrochar (HBC), has been tested as a soil enhancer to improve saline soils. However, the effects of PBC and HBC application on ammonia (NH) volatilization and dissolved organic matter (DOM) in saline paddy soils are poorly understood. In this research, marsh moss-derived PBC and HBC biochar types were applied to paddy saline soils at 0.5 % (w/w) and 1.5 % (w/w) rates to assess their impact on soil NH volatilization and DOM using a soil column experiment. The results revealed that soil NH volatilization significantly increased by 56.1 % in the treatment with 1.5 % (w/w) HBC compared to the control without PBC or HBC. Conversely, PBC and the lower application rate of HBC led to decrease in NH volatilization ranging from 2.4 % to 12.1 %. Floodwater EC is a dominant factor in NH emission. Furthermore, the fluorescence intensities of the four fractions (all humic substances) were found to be significantly higher in the 1.5 % (w/w) HBC treatment applied compared to the other treatments, as indicated by parallel factor analysis modeling. This study highlights the potential for soil NH losses and DOM leaching in saline paddy soils due to the high application rate of HBC. These findings offer valuable insights into the effects of PBC and HBC on rice paddy saline soil ecosystems.

摘要

生物炭,包括热解炭(PBC)和水热炭(HBC),已被作为一种土壤改良剂进行测试,以改善盐碱地。然而,PBC和HBC施用于盐碱稻田土壤对氨(NH)挥发和溶解有机物(DOM)的影响却鲜为人知。在本研究中,将沼苔衍生的PBC和HBC生物炭类型以0.5%(w/w)和1.5%(w/w)的比例施用于稻田盐碱土,通过土柱试验评估它们对土壤NH挥发和DOM的影响。结果表明,与不添加PBC或HBC的对照相比,1.5%(w/w)HBC处理的土壤NH挥发显著增加了56.1%。相反,PBC和较低施用量的HBC导致NH挥发减少了2.4%至12.1%。淹水EC是NH排放的主导因素。此外,平行因子分析模型表明,与其他处理相比,1.5%(w/w)HBC处理中四个组分(所有腐殖物质)的荧光强度显著更高。本研究强调了由于HBC的高施用量,盐碱稻田土壤中存在土壤NH损失和DOM淋溶的可能性。这些发现为PBC和HBC对稻田盐碱土生态系统的影响提供了有价值的见解。

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