模拟高温-降水对培肥土壤CO2排放及可溶性有机质的影响
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1.四川农业大学资源学院;2.四川省烟草公司攀枝花市公司

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四川省科技厅项目(2025YFHZ0142,25NSFJQ0002)、四川省大学生创新训练计划项目(S202410626058)和国家重点研发计划项目(2022YFD1901605)共同资助


Effects of Simulated High Temperature and Precipitation on CO2 Emissions and Dissolved Organic Matter in Fertilized Soil
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Affiliation:

1.College of Resources, Sichuan Agricultural University;2.Sichuan tobacco company Panzhihua city company;3.Southwest University College of Resources and Environment

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Supported by the Natural Science Foundation of Sichuan Province(Nos. 2025YFHZ0142,25NSFJQ0002), Innovation Training Program for College Students in Sichuan Province(No.S202410626058)and the National Key Research and Development Program of China(No.2022YFD1901605)

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    摘要:

    有机培肥是维持农业土壤肥力水平最主要的措施之一,然而土壤培肥的同时能否有效应对复合极端天气事件,维持土壤有机碳(Soil Organic Carbon,SOC)稳定性,尚不清楚。土壤可溶性有机质(Dissolved Organic Matter,DOM)作为衡量SOC动态变化的重要指标,是SOC积累及稳定过程的核心参与者。本研究以稻田土壤为对象,基于短期模拟培养试验,采用顶空定期采气-气相色谱法、紫外-可见吸收和荧光光谱方法,对比分析模拟高温(32℃)-降水对不同培肥稻田土壤(施用磷钾化肥,PK;施用氮磷钾化肥,NPK;低量有机培肥,LOM;高量有机培肥,HOM)的CO2排放速率及累计排放量,可溶性有机质含量及光谱特征的影响。结果表明:(1)在高温培养或降水后高温培养期间,有机培肥(LOM和HOM)处理土壤CO2累计排放量变幅较小,仅为8.92%~14.17%,有效增加了有机培肥土壤应对外界高温-降水事件影响的韧性;(2)与高温培养第1天(Day1)相比,培肥处理在高温培养第14天(Day14)时土壤DOM含量均增加,尤其是有机培肥(LOM和HOM)处理显著增加了7.81~14.74 mg·kg-1(P<0.05),但HOM处理显著降低了土壤DOM芳香性(SUVA254)、疏水性(SUVA260)以及各类荧光物质的含量,表明在高温胁迫下,有机培肥只改变了土壤DOM的结构组成,并未促进CO2的排放;(3)与Day14相比,降水后高温培养(Day28)显著降低了土壤DOM含量,降幅达64.05%~80.44%(P<0.05),然而有机培肥较其他处理显著增加了土壤DOM的SUVA254、SUVA260指数,提高了腐殖化程度(HIX),从而减少了CO2排放,而有机肥自身造成的类蛋白物质(荧光峰B和T)的增加,并不能引起土壤CO2排放的增加。总体上,在本研究条件下,有机培肥尤其是有机替代25%~50%氮肥,均能够提高土壤有机碳稳定性,增强其抵御极端天气事件的农业适应能力,为气候变化背景下优化农业施肥模式提供了科学依据。

    Abstract:

    【Objective】Organic fertilization is one of the most important measures to maintain the fertility level of agricultural soil. However, it is still unclear whether soil fertilization can effectively cope with the frequent occurrence of compound extreme weather events and maintain the stability of soil organic carbon (SOC). Moreover, soil dissolved organic matter (DOM) is an important indicator to measure the dynamic changes of SOC and also a core participant in the process of SOC accumulation and stability. Nevertheless, it is still unclear how extreme weather events may affect DOM and consequently its contribution to SOC accumulation and stability. 【Method】A short-term simulation experiment was conducted using rice paddy soils, and headspace gas sampling, gas chromatography, ultraviolet-visible absorption and fluorescence spectroscopy were applied to compare the effects of high temperature (32 ℃)-precipitation on the emission of CO2 and spectral characteristics of soil DOM in different fertilized soils (PK: phosphorus-potassium fertilizer; NPK: nitrogen-phosphorus-potassium fertilizer, LOM: low-volume organic manure; and HOM: high-volume organic manure). 【Result】The results revealed that (1) the variation range of cumulative soil CO2 emissions in the organic fertilization treatments (LOM and HOM) was relatively small, ranging from 8.92% to 14.17% during high-temperature or high-temperature after precipitation incubations. This effectively increased the resilience of organically fertilized soil in response to external high temperature-precipitation events. (2) Compared with the first day (Day 1) of high-temperature incubation, the soil DOM content in LOM and HOM treatments significantly increased by 7.81-14.74 mg·kg-1 (P<0.05). However, the HOM treatment significantly reduced the soil DOM aromaticity (SUVA254), hydrophobicity (SUVA260), and various fluorescent substances, indicating that under high temperature stress, organic fertilization only changed the structural composition of soil DOM and did not promote the emission of CO2. (3) High temperature incubation after precipitation (Day 28) significantly reduced the soil DOM content by 64.05%-80.44% (P<0.05) when compared with Day 14. Also, organic fertilization significantly increased the SUVA254 and SUVA260 indices of soil DOM and the humification index (HIX) compared with other treatments, thereby reducing CO2 emissions. The increase in protein-like substances (fluorescence peaks B and T) caused by organic fertilizer itself did not lead to an increase in soil CO2 emissions.【Conclusion】Overall, organic fertilization, especially the organic substitution of 25%-50% nitrogen fertilizer, can improve the stability of soil organic carbon, enhance its agricultural adaptability in extreme weather events under the conditions of this study. The findings of this study provide a scientific basis for optimizing agricultural fertilization models, and promoting sustainable agricultural development.

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王森辕,李星宇,熊维亮,黄玉珠,王昌全,李 冰,黄 容.模拟高温-降水对培肥土壤CO2排放及可溶性有机质的影响[J].土壤学报,2026,63(1). DOI:10.11766/trxb202502100053 WANG Senyuan, LI Xingyu, XIONG Weiliang, HUANG Yuzhu, WANG Changquan, LI Bing, HUANG Rong. Effects of Simulated High Temperature and Precipitation on CO2 Emissions and Dissolved Organic Matter in Fertilized Soil[J]. Acta Pedologica Sinica,2026,63(1).

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  • 收稿日期:2025-02-10
  • 最后修改日期:2025-07-07
  • 录用日期:2025-07-22
  • 在线发布日期: 2025-07-28
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