青稞连作对根际土壤理化性质及酶活性的影响OA
Effects of continuous cropping of highland barley on physio-chemical properties and enzyme activities of rhizosphere soil
[目的]分析不同连作年限下青稞根际土壤理化性质与酶活性变化,以期揭示连作对青稞根际土壤微环境的影响机制并探索青稞连作障碍的科学治理途径,明确连作对土壤微环境的调控规律.[方法]设置连作2年(CCY02)、5年(CCY05)和10年(CCY10)3个处理,采集根际土壤样品,测定其理化指标与关键酶活性,并运用相关性分析等方法解析各指标间内在联系.[结果]随连作年限延长,青稞根际土壤碳、氮养分含量持续下降,其中有机质较连作2年下降76.77%,土壤基础肥力耗竭明显;速效钾异常积累,养分输入与作物吸收的比例严重失衡;土壤容重下降,孔隙状况改变、电导率显著升高,可溶性盐分累计风险增加;pH始终维持中性偏碱(8.06~8.91),且各年限之间无显著差异;生态化学计量中C/P、C/K、N/P、N/K下降,C/N上升,微生物代谢所需养分协调性被破坏.连作10年后,过氧化氢酶、磷酸酶及转化酶活性整体降低,其中转化酶活性显著下降39.72%,土壤酶系统功能受到抑制.相关性分析表明,土壤碳、氮养分与速效钾呈显著负相关,且转化酶活性与碳氮含量呈极显著正相关,可作为反映连作土壤养分变化的关键生物指标.[结论]长期连作导致青稞根际土壤碳氮养分缺失、钾素积累、磷素波动及养分比例失衡,同时显著抑制关键土壤酶活性,土壤理化性质与酶活性的协同劣变是青稞连作障碍形成的重要机制.
[Objective]The present paper analyzed the changes in physico-chemical properties and enzyme activities in the rhizosphere soil of highland barley under different continuous cropping years,aiming to reveal the impact mechanism of continuous cropping on the rhizosphere soil micro-environment,explore scientific approaches to mitigate continuous cropping obstacles,and clarify the regulatory patterns of continu-ous cropping on the soil micro-environment.[Method]Three treatments were established including continuous cropping for 2 years(CCY02),5 years(CCY05)and 10 years(CCY10).Rhizosphere soil samples were collected to determine physio-chemical indicators and key enzyme activities.Correlation analysis and other methods were employed to examine the relationships among these parameters.[Result]With the ex-tension of continuous cropping years,the carbon and nitrogen nutrient contents in the rhizosphere soil of highland barley continued to decline.Specifically,compared with CCY02,the soil organic matter decreased by 76.77%,indicating a significant depletion of soil basic fertility.A-vailable potassium accumulated abnormally,suggesting a severe imbalance between nutrient input and crop uptake.Soil bulk density de-creased,leading to altered porosity,while electrical conductivity increased significantly,raising the risk of soluble salt accumulation.The soil pH remained neutral to slightly alkaline(ranging from 8.06 to 8.91)with no significant differences observed among different cropping years.Regarding ecological stoichiometry,the ratios of C/P,C/K,N/P and N/K decreased,whereas the C/N ratio increased,indicating a dis-ruption in the coordination of nutrients required for microbial metabolism.After 10 years of continuous cropping,the activities of catalase,phosphatase and invertase generally decreased.Notably,invertase activity significantly declined by 39.72%,suggesting that the functionality of the soil enzyme system was inhibited.Correlation analysis revealed a significant negative correlation between soil carbon and nitrogen nutri-ents and available potassium.Furthermore,invertase activity showed an extremely significant positive correlation with carbon and nitrogen con-tents,establishing it as a key biological indicator for reflecting nutrient changes in continuously cropped soil.[Conclusion]Long-term continu-ous cropping of highland barley leads to depletion of carbon and nitrogen,accumulation of potassium,fluctuation in phosphorus availability,and disruption of nutrient balances in the rhizosphere soil.It also significantly suppresses key soil enzyme activities.The coordinated deterio-ration of soil physio-chemical properties and enzyme activity is a critical mechanism underlying the formation of continuous cropping obstacles in highland barley.
陈加利;胡体龙;李宏英;许艺菲;李霞;赵媛
青海大学生态环境工程学院,西宁 810016青海大学生态环境工程学院,西宁 810016青海大学生态环境工程学院,西宁 810016青海大学生态环境工程学院,西宁 810016青海大学生态环境工程学院,西宁 810016青海大学生态环境工程学院,西宁 810016
农业科技
青稞连作根际土壤土壤酶活性土壤理化性质
Highland barleyContinuous croppingRhizosphere soilSoil enzyme activitySoil physio-chemical properties
《西南农业学报》 2026 (5)
1013-1023,11
国家自然科学基金项目(2024-NSFC-32460474)青海省"昆仑英才-高端创新创业人才项目"
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