• ISSN 1008-505X
  • CN 11-3996/S

提高秸秆还田量促进稻麦轮作土壤大团聚体形成协调土壤交换性钾的固存与释放

Increasing straw return promotes macroaggregate formation in rice-wheat rotation soils, thereby coordinating the retention and release of exchangeable potassium

  • 摘要:
    目的 探讨长期秸秆还田对土壤大团聚体分布、大团聚体中交换性钾分配及其与有机碳含量间的耦合机制。
    方法 研究基于湖北省潜江市的水稻-小麦轮作18年的长期定位试验,选取CK (不施化肥,秸秆不还田),−S (秸秆不还田),+0.5S (秸秆半量还田),+S (秸秆全量还田)四个处理,于2023年9月采集土壤样品,通过团聚体密度分级、交换性钾含量及有机碳含量分析,结合固态13C核磁共振技术,揭示秸秆还田对土壤大团聚体分布特征及交换性钾分配的影响。
    结果 1)与CK和−S相比,+0.5S和+S处理显著提高了>0.25 mm团聚体组分的比例。在大团聚体组分中,与−S相比,+S处理大团聚体中惰性碳结合组分M(c)POM的比例提高了21.9%,缓性碳结合组分M-MOM比例显著降低了55.4%;2)长期秸秆还田条件下,>0.25 mm团聚体组分交换性钾含量得到显著提高,主要源于对M(c)POM、M-MOM组分中交换性钾含量的提升。>0.25 mm团聚体组分交换性钾库得到显著提高。相较于−S处理,+0.5S和+S处理下,>2 mm团聚体交换性钾库分别增加了111.1%和242.4%,且大团聚体钾库的增加主要源于M(c)POM组分钾库的提高;3)长期秸秆还田条件下,相比于−S,+0.5S和+S下>2 mm团聚体组分有机碳含量分别增加了17.6%和46.5%,有机碳库分别增加了55.4%和87.8%,且其提升主要源于对M(c)POM组分的提升。相较于−S,+0.5S和+S分别促使大团聚体中M(c)POM组分烷基碳含量增加了38.1%和34.7%,芳香碳含量下降了22.7%和18.2%,烷基碳类活性有机碳的增加,可吸附更多的交换性钾,提高土壤钾素有效性;4) M(c)POM组分中有机碳与交换性钾含量呈极显著正相关,表明秸秆还田通过促进M(c)POM累积,协同提升了土壤碳固存与钾素供应能力。
    结论 长期秸秆还田显著提高了土壤>0.25 mm大团聚体比例及其钾储量和碳储量,M(c)POM组分是影响土壤钾素有效性的关键组分,秸秆还田促进了M(c)POM组分有机碳累积,通过“吸附-络合-团聚体固持”等过程调控钾素的固存与释放,有效提升了土壤钾素供应能力。随着秸秆还田量的提高,土壤钾素供应能力的提升更为显著,即有机碳的输入量直接影响着秸秆还田调控钾的效应。因此,秸秆还田量可通过促进土壤大团聚体形成,协调土壤交换性钾的固存与释放。

     

    Abstract:
    Objective This study investigated the effects of long-term straw return on changes in exchangeable potassium (K) content within different fractions of soil macro-aggregates and its coupling mechanism with organic carbon content.
    Methods This study was based on an 18-year long-term fixed-site experiment of rice-wheat rotation in Qianjiang City, Hubei Province. Four treatments were selected: CK (no chemical fertilizer, no straw return), −S (no straw return), +0.5S (50% straw return), and +S (100% straw return). Soil samples collected in September 2023 were analyzed through aggregate density fractionation, exchangeable potassium content, and organic carbon content analyses. Combined with solid-state 13C nuclear magnetic resonance (NMR) spectroscopy, the research revealed the effects of straw return on the distribution characteristics of soil macroaggregates and exchangeable potassium allocation.
    Results 1) Compared to CK and −S, long-term straw return significantly increased the proportion of >0.25 mm aggregate fractions. Within macroaggregate fractions, the proportion of M(c)POM under +S treatment increased by 21.9%, while that of M-MOM decreased significantly by 55.4% relative to −S. 2) Under long-term straw incorporation, exchangeable potassium content in >0.25 mm aggregates significantly increased, primarily attributable to elevated levels in the M(c)POM and M-MOM fractions. The exchangeable potassium pool in >0.25 mm aggregates was significantly enhanced. Compared with the −S treatment, the potassium pool in >2 mm aggregates increased by 111.1% and 242.4% under +0.5S and +S treatments, respectively, with the augmentation primarily originating from the M(c)POM fraction. 3) Under long-term straw return conditions, compared to the −S treatment, the organic carbon content in the >2 mm aggregate fraction increased by 17.6% and 46.5% under the +0.5S and +S treatments, respectively, while the organic carbon pool increased by 55.4% and 87.8%, respectively. This improvement was primarily attributed to the enhancement of the M(c)POM fraction. Compared to the −S treatment, the +0.5S and +S treatments increased the alkyl carbon content in the M(c)POM fraction of macroaggregates by 38.1% and 34.7%, respectively, while the aromatic carbon content decreased by 22.7% and 18.2%, respectively. The increase in alkyl carbon, a type of active organic carbon, can adsorb more exchangeable potassium, thereby improving soil potassium availability. 4) Correlation analysis demonstrated a highly significant positive relationship between organic carbon and exchangeable potassium content in M(c)POM, indicating that straw return synergistically enhanced soil carbon sequestration and potassium supply by promoting M(c)POM accumulation.
    Conclusion Long-term straw incorporation significantly increases the proportion of soil macroaggregates (>0.25 mm), as well as their potassium and carbon reserves. The M(c)POM (macro-organic matter within macroaggregates or coarse particulate organic matter) component emerged as a key factor influencing soil potassium availability. Straw incorporation promoted the accumulation of organic carbon in the M(c)POM fraction, regulating potassium retention and release through processes such as "adsorption-complexation-aggregate stabilization," thereby effectively enhancing the soil's potassium supply capacity. As the amount of straw incorporated increased, the improvement in soil potassium supply capacity became more pronounced, indicating that the input of organic carbon directly influences the effectiveness of straw incorporation in regulating potassium. Therefore, the amount of straw incorporated can facilitate the formation of soil macroaggregates and coordinate the retention and release of exchangeable potassium in the soil.

     

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