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长期施用石灰和秸秆还田条件下酸性红壤 pH 对土壤有机碳的调节作用。

Soil organic carbon regulation by pH in acidic red soil subjected to long-term liming and straw incorporation.

机构信息

State Key Laboratory of Efficient Utilization of Arid and Semi-arid Arable Land in Northern China, Institute of Agricultural Resources and Regional Planning, Chinese Academy of Agricultural Sciences, Beijing, 100081, China.

School of Agricultural Sciences, Zhengzhou University, Zhengzhou, 450001, China.

出版信息

J Environ Manage. 2024 Sep;367:122063. doi: 10.1016/j.jenvman.2024.122063. Epub 2024 Aug 3.

Abstract

The manipulation of soil pH through liming and straw incorporation plays a pivotal role in influencing soil organic carbon (SOC) dynamics in acidic red soil. This study aimed to assess the impact of these practices on SOC and elucidate the relationship between SOC and pH. Over a 31-year field experiment, seven different fertilization treatments were implemented: unfertilized (CK), nitrogen and potassium fertilizers (NK), NK with lime (NKCa), nitrogen, phosphorous, and potassium fertilizers (NPK), NPK with lime (NPKCa), NPK with straw (NPKS), and NPKS with lime (NPKSCa). Results revealed that liming and straw incorporation significantly elevated soil pH by 0.13-0.73 units. Lime application boosted SOC and mineral-associated organic carbon (MAOC) by 20.2% and 28.7%, respectively, in NK treatment, whereas its impact on SOC in NPK and NPKS treatments were negligible. SOC witnessed a 17.1% increase with NPKS and a 15.2% increase with NPKSCa compared to NPK alone. Notably, NPKS and NPKSCa led to a significant surge in particulate organic carbon (POC) by 19.7% and 37.7%, respectively, albeit NPKSCa reduced MAOC by 14.9% relative to NPK. Linear regression analysis unveiled a positive correlation between POC and soil pH, while SOC and MAOC exhibited an initial rise at lower pH levels followed by stabilization as pH continuously increasing. A partial least squares path model showed two pathways through which pH influenced SOC: firstly, by positively affecting SOC through increasing Fe and Al oxides contents and enhanced aggregate stability, and secondly, by negatively influencing SOC through altered ratios of fungi/bacteria and Gram-positive bacteria/Gram-negative bacteria. In conclusion, the long-term effects of lime and straw application on SOC and MAOC were contingent upon soil pH, with more pronounced positive effects observed at lower pH levels. These findings underscore the importance of considering soil pH when implementing lime and straw strategies to mitigate acidification and regulate SOC in acidic red soil.

摘要

通过石灰和秸秆混合施用来调节土壤 pH 值,对酸性红壤中土壤有机碳(SOC)动态变化具有重要影响。本研究旨在评估这些措施对 SOC 的影响,并阐明 SOC 与 pH 值之间的关系。在一项为期 31 年的田间试验中,实施了 7 种不同施肥处理:不施肥(CK)、氮钾肥料(NK)、氮钾加石灰(NKCa)、氮磷钾肥料(NPK)、氮磷钾加石灰(NPKCa)、氮磷钾加秸秆(NPKS)和氮磷钾加秸秆加石灰(NPKSCa)。结果表明,石灰和秸秆混合施用使土壤 pH 值分别提高了 0.13-0.73 个单位。石灰的应用使 NK 处理中的 SOC 和矿物结合有机碳(MAOC)分别增加了 20.2%和 28.7%,而对 NPK 和 NPKS 处理中的 SOC 影响可以忽略不计。与单独使用 NPK 相比,NPKS 和 NPKSCa 使 SOC 分别增加了 17.1%和 15.2%。值得注意的是,NPKS 和 NPKSCa 使颗粒有机碳(POC)分别增加了 19.7%和 37.7%,而 NPKSCa 使 MAOC 相对于 NPK 减少了 14.9%。线性回归分析表明,POC 与土壤 pH 值呈正相关,而 SOC 和 MAOC 在较低的 pH 值水平下先升高,然后随着 pH 值的持续升高而稳定。偏最小二乘路径模型显示了 pH 值影响 SOC 的两种途径:首先,通过增加 Fe 和 Al 氧化物含量和增强团聚体稳定性来正向影响 SOC;其次,通过改变真菌/细菌和革兰氏阳性菌/革兰氏阴性菌的比例来负向影响 SOC。综上所述,石灰和秸秆施用对 SOC 和 MAOC 的长期影响取决于土壤 pH 值,在较低的 pH 值水平下观察到更明显的积极影响。这些发现强调了在实施石灰和秸秆策略以减轻酸化和调节酸性红壤中的 SOC 时,考虑土壤 pH 值的重要性。

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