| 不同有机肥施用模式下黄壤稻田根际和非根际土壤有机碳的矿化特征 |
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| 引用本文： | 张雅蓉,刘彦伶,黄兴成,杨叶华,朱华清,熊涵,李渝.不同有机肥施用模式下黄壤稻田根际和非根际土壤有机碳的矿化特征[J].植物营养与肥料学报,2023,29(3):449-458. |
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| 作者姓名： | 张雅蓉 刘彦伶 黄兴成 杨叶华 朱华清 熊涵 李渝 |
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| 作者单位： | 1.贵州省土壤肥料研究所，贵州贵阳 550006 |
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| 基金项目： | 黔农科院青年科技基金([2021]12号)；贵州省土壤肥料研究所科技成果培育与人才培养项目(黔土肥技术[2022]4号)；贵州省农业科学院科技创新专项(黔农科院科技创新［2022］09号)；国家农业重大科技项目(NK2022180303)；国家自然科学基金(31860132；32060302)；黔农科院基础性公益专项([2022]05号)；黔农科院青年科技基金([2022]23号)。 |
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| 摘 要： | 【目的】研究长期施用有机肥对土壤有机碳矿化特征的影响，为提高土壤碳库稳定性和培肥土壤提供理论依据。【方法】贵阳黄壤肥力与肥效长期定位试验始于1994年，种植制度为单季水稻。2021年水稻收获后，选取不施肥(CK)，平衡施用化肥(NPK),25%和50%有机肥氮替代化肥氮(0.25MNPK、0.5MNPK)和单施有机肥(M) 5个处理的水稻植株，用抖根法采集根际和非根际土壤样品，分析活性碳组分含量，以采集的土样进行室内培养试验，研究有机碳矿化特征。【结果】1)与NPK相比，3个有机肥处理的根际土壤有机碳(SOC)含量提升了26%～43%，非根际土壤SOC含量提高了24%～32%；根际土壤微生物量碳(MBC)含量提升了16%～31%，且比非根际土壤高148%；非根际土壤易氧化有机碳(LOC)含量显著提升了36%～75%;0.5MNPK处理非根际土壤可溶性有机碳(DOC)含量显著提升了54%，且根际土壤的DOC含量平均高于非根际土壤10%。2)有机肥施用可明显增加黄壤稻田根际及非根际土壤有机碳矿化量，非根际土壤有机碳矿化量和矿化率分别高于根际土壤30%和33%；较CK和NPK处理，有机肥施用...
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| 关 键 词： | 长期施肥 有机肥 黄壤稻田 根际 非根际 有机碳矿化 |
| 收稿时间： | 2022-07-21 |
Organic carbon mineralization characteristics in rhizosphere and bulk soil of rice under organic fertilization modes in yellow paddy fields |
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| ZHANG Ya-rong,LIU Yan-ling,HUANG Xing-cheng,YANG Ye-hua,ZHU Hua-qing,XIONG Han,LI Yu.Organic carbon mineralization characteristics in rhizosphere and bulk soil of rice under organic fertilization modes in yellow paddy fields[J].Plant Nutrition and Fertilizer Science,2023,29(3):449-458. |
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| Authors: | ZHANG Ya-rong LIU Yan-ling HUANG Xing-cheng YANG Ye-hua ZHU Hua-qing XIONG Han LI Yu |
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| Affiliation: | 1.Guizhou Institute of Soil and Fertilizer, Guiyang, Guizhou 550006, China |
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| Abstract: | 【Objectives】 Study of the effects of organic fertilization on soil organic carbon mineralization characteristics could elucidate the soil carbon pool change and stable mechanism of yellow paddy fields. 【Methods】 The long-term experiment of fertility and fertilizer efficiency of Guiyang was established in 1994, with mono-rice planting system. In 2021, rhizosphere and bulk soils of rice were collected from the five treatments for the determination of soil total and active carbon fraction contents. Including the control (no fertilizer, CK), balanced application of chemical fertilizer (NPK), 25% and 50% organic fertilizer nitrogen instead of chemical fertilizer nitrogen (0.25MNPK, 0.5MNPK) and single organic fertilizer (M). A indoor incubation experiment was conducted using the soils for determination of organic carbon mineralization amount and kinetic mineralization parameters. 【Results】 1) Compared with NPK, organic fertilizer treatments (0.25MNPK, 0.5MNPK, M) increased soil organic carbon (SOC) in rhizosphere and bulk soil by 26%?43% and 24%?32%, and microbial biomass carbon (MBC) in rhizosphere soil by 16%?31%, and the MBC in rhizosphere soil was 148% higher than bulk soil. Compared with NPK, contents of liable organic carbon (LOC) in bulk soils was significantly increased by 36%?75% under organic fertilizer treatments. Dissolved organic carbon (DOC) content was significantly increased by 54% in bulk soil under 0.5MNPK treatment, and DOC in rhizosphere soil was 10% higher than that of bulk soil. 2) Organic fertilizer treatments significantly increased SOC mineralization in rhizosphere and bulk soils, and the mineralization amount and rate in bulk soil were 30% and 33% higher than in rhizosphere soil, respectively. Compared with CK and NPK, organic fertilizer treatments significantly increased rhizosphere SOC mineralization by 36%?63%, which was proportional to the application amount of organic fertilizer. NPK treatment recorded lower mineralization amount than CK, but its variation with CK was more pronounced in bulk soil. CK elicited the highest cumulative mineralization rate in bulk soil, which was 19%?28% higher than organic fertilizer treatments. 3) The dynamics of cumulative SOC mineralization amount with incubation time fit the first-order kinetic equation. In rhizosphere soils, treatment M increased the cumulative mineralization of organic carbon (Ct), while 0.25MNPK and 0.5MNPK treatments increased potential mineralizable organic carbon (C0) by 1.44?3.23 times of CK. 0.25MNPK and 0.5MNPK treatments significantly reduced the turnover rate of organic carbon pool per day constant k. Compared with NPK, Ct was significantly increased in bulk soil, C0 was significantly increased by 0.25MNPK treatment, and k value was significantly reduced under 0.25MNPK and 0.5MNPK treatments. 4) Ct was significantly and positively correlated with SOC, LOC, and DOC contents, but both were significantly and negatively correlated with qMB (SMB/SOC) in rhizosphere and bulk soils. 【Conclusions】 In sum, 25% to 50% organic nitrogen substitution are the preferred fertilization modes for carbon pool management and soil fertilization in yellow paddy fields, for it markedly increases the stability of soil organic carbon, carbon storage, and reduces carbon loss. |
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