首页|麦玉轮作长期秸秆还田下土壤呼吸及有机碳库对温度变化的响应

麦玉轮作长期秸秆还田下土壤呼吸及有机碳库对温度变化的响应

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为探明华北麦玉轮作区长期秸秆还田下增温对土壤呼吸及土壤碳库的影响,本试验基于 41 年不同秸秆还田水平(分别为0 kg/hm2(S1)、2 250 kg/hm2(S2)、4 500 kg/hm2(S3)和9 000 kg/hm2(S4))田间定位试验,采集土壤样品后分别在 15、25 和 35℃下进行 125 d的室内恒温培养,针对土壤呼吸速率及有机碳组分含量进行监测。结果表明:在整个培养期间,土壤呼吸速率呈现先下降后平稳的变化趋势,秸秆还田量与温度显著影响土壤呼吸速率和呼吸累积释放量。各处理间土壤呼吸速率和呼吸累积释放量整体为 35℃>25℃>15℃,S4>S3>S2>S1。秸秆还田量和温度显著影响土壤有机碳及各组分含量,培养后S4 处理土壤有机碳含量显著高于其他处理,S3 和S4 处理土壤颗粒有机碳和微生物量碳含量显著高于其他处理,随培养温度的提高土壤有机碳组分呈降低趋势。土壤呼吸与土壤有机碳、颗粒有机碳、微生物量碳含量呈显著正相关。S3 和S4 处理较S1和S2 处理可以显著降低土壤呼吸温度敏感性(Q10)。总的来看,华北麦玉轮作区长期中量和高量秸秆还田可以提高土壤有机碳库,降低土壤呼吸温度敏感性,减缓CO2 的释放,且 4 500 kg/hm2 还田量具有更高的固碳潜力与空间。
Responses of soil respiration and soil organic carbon pools to temperature under long-term different straw returning amounts in wheat-maize rotation system
Soil samples were collected from 41-year experimental fields that have been continuously returning straws with different amounts including 0 kg/hm2(S1),2 250 kg/hm2(S2),4 500 kg/hm2(S3),and 9 000 kg/hm2(S4)and were incubated at 15,25 and 35℃for 125 d to investigate the responses of soil respiration and soil carbon pools in the wheat and maize rotation area of North China.The results showed that soil respiration rate showed a decreasing and then stable trend during the whole incubation period.The straw returning amount and temperature significantly affected the soil respiration rate and the cumulative soil respiration.Soil respiration rate and the cumulative soil respiration among treatments are generally exhibited on 35℃>25℃>15℃,S4>S3>S2>S1.The straw returning amount and temperature significantly affected soil organic carbon and its fractions.Soil organic carbon content in S4 treatment was significantly higher than that of other treatments.The contents of soil particulate organic carbon and microbial organic carbon in S3 and S4 treatments were significantly higher than that of other treatments.With the increase of incubation temperature,soil organic carbon and its fractions showed a decreasing trend.Soil respiration rate was positively correlated with soil organic carbon,particulate organic carbon,and microbial carbon content.Compared with S1 and S2,temperature sensitivity(Q10)significantly decreased in S3 and S4.In conclusion,long-term medium and high straw returning can improve soil organic carbon pool,decrease the temperature sensitivity of soil respiration,and lower the release of CO2 in wheat and maize rotation system in North China,and the medium straw returning has a higher potential and space for carbon sequestration under global warming conditions.

straw returningwarmingsoil respirationtemperature sensitivitysoil organic carbon fractions

李旭、付鑫、杨晓楠、李敬宇、翟英芳

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河北省农田生态环境重点实验室,河北 保定 071001

河北农业大学 国土资源学院,河北 保定 071001

华北作物改良与调控国家重点实验室,河北 保定 071001

河北省山区研究所,河北 保定 071001

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秸秆还田 增温 土壤呼吸 温度敏感性 土壤有机碳组分

国家自然科学青年基金项目河北省重点研发计划项目河北省自然科学基金项目

4220740421326402DD2020204012

2024

河北农业大学学报
河北农业大学

河北农业大学学报

CSTPCD北大核心
影响因子:0.475
ISSN:1000-1573
年,卷(期):2024.47(2)
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