生态环境学报 ›› 2023, Vol. 32 ›› Issue (9): 1552-1562.DOI: 10.16258/j.cnki.1674-5906.2023.09.002
唐志伟1(), 翁颖1, 朱夏童1, 蔡洪梅1, 代雯慈1, 王捧娜1, 郑宝强1, 李金才1,2,*(
), 陈翔1,*(
)
收稿日期:
2023-07-27
出版日期:
2023-09-18
发布日期:
2023-12-11
通讯作者:
李金才。E-mail: ljc5122423@126.com作者简介:
唐志伟(2000年生),男,硕士研究生,研究方向为作物生理生态。E-mail: tzw13866538069@126.com
基金资助:
TANG Zhiwei1(), WENG Ying1, ZHU Xiatong1, CAI Hongmei1, DAI Wenci1, WANG Pengna1, ZHENG Baoqiang1, LI Jincai1,2,*(
), CHEN Xiang1,*(
)
Received:
2023-07-27
Online:
2023-09-18
Published:
2023-12-11
摘要:
秸秆还田能改变农田土壤微生物生物量碳(Soil Microbial Biomass Carbon,SMBC)含量,分析秸秆还田条件下SMBC含量变化及其相关影响因素,对理解秸秆还田下土壤养分周转与碳循环机制具有重要意义。基于中国知网和Web of Science数据库2001-2022年公开发表的68篇文献,建立了839组包含秸秆还田和秸秆不还田下SMBC含量的数据库,按照气候类型、种植方式、耕作方式、秸秆种类、施氮量、秸秆还田量进行分组,采用Meta分析对秸秆还田条件下SMBC含量变化的特征进行综合分析。结果表明,与秸秆不还田相比,1)秸秆还田显著提升SMBC含量(51.4%,置信区间为0.373-0.654),且对不同土层SMBC含量的提升效果不同,浅层和深层SMBC含量分别提升47.9%和42.7%。2)秸秆还田下温带季风气候区和亚热带季风气候区SMBC含量分别增加71.0%和35.8%,但在温带大陆气候区对SMBC含量影响表现出显著负效应,降低幅度为35.6%。3)不同耕作方式下旋耕(99.2%)对SMBC含量的增幅影响最为明显,约为常规耕作和免耕下的2.4倍和4倍。4)旱地秸秆还田SMBC含量的增幅明显高于稻田。玉米秸秆对SMBC含量的响应度最高,增幅达到99.5%,水稻秸秆次之,增幅为30.8%;小麦秸秆最低,降低幅度为5.8%。5)施氮量对SMBC含量增幅在−34.5%-183.9%之间,0-100 kghm−2和101-225 kghm−2施氮量下秸秆还田可显著提升SMBC含量,而在226-325 kghm−2和326-425 kghm−2施氮量下秸秆还田对SMBC含量的影响表现出显著的负效应;6)对于秸秆还田量而言,当秸秆还田量 <4500 kghm−2时增幅52.60%,4500-9000 kghm−2时增幅47.7%,>9000 kghm−2时增幅44.2%,但SMBC含量的增幅表现出随着秸秆还田量的增加呈递减趋势。由此可见,不同的气候类型、种植方式、耕作方式、秸秆种类、施氮量、秸秆还田量等条件下,秸秆还田对中国农田SMBC含量的影响存在显著差异。
中图分类号:
唐志伟, 翁颖, 朱夏童, 蔡洪梅, 代雯慈, 王捧娜, 郑宝强, 李金才, 陈翔. 秸秆还田下中国农田土壤微生物生物量碳变化及其影响因素的Meta分析[J]. 生态环境学报, 2023, 32(9): 1552-1562.
TANG Zhiwei, WENG Ying, ZHU Xiatong, CAI Hongmei, DAI Wenci, WANG Pengna, ZHENG Baoqiang, LI Jincai, CHEN Xiang. Meta-analysis of Soil Microbial Mass Carbon and Its Influencing Factors in Farmland in China under Straw Return[J]. Ecology and Environment, 2023, 32(9): 1552-1562.
土壤深度 | 气候类型 | 种植方式 | 耕作方式 | 秸秆种类 | 施氮量 | 秸秆还田量 |
---|---|---|---|---|---|---|
总体 (839) | 温带大陆气候 (54) | 稻田 (324) | 旋耕 (247) | 玉米 (355) | 0−100 (143) | <4500 (251) |
浅层0−20 (747) | 温带季风气候 (439) | 旱地 (515) | 深耕 (23) | 小麦 (90) | 101−225 (345) | 4500−9000 (226) |
深层>20 (92) | 亚热带季风气候 (301) | 免耕 (44) | 水稻 (218) | 226−325 (172) | >9000 (47) |
表1 数据分组情况
Table 1 Data grouping
土壤深度 | 气候类型 | 种植方式 | 耕作方式 | 秸秆种类 | 施氮量 | 秸秆还田量 |
---|---|---|---|---|---|---|
总体 (839) | 温带大陆气候 (54) | 稻田 (324) | 旋耕 (247) | 玉米 (355) | 0−100 (143) | <4500 (251) |
浅层0−20 (747) | 温带季风气候 (439) | 旱地 (515) | 深耕 (23) | 小麦 (90) | 101−225 (345) | 4500−9000 (226) |
深层>20 (92) | 亚热带季风气候 (301) | 免耕 (44) | 水稻 (218) | 226−325 (172) | >9000 (47) |
图1 不同土层SMBC对秸秆还田的响应 点和误差线分别代表增幅及95%的置信区间,如果95%的置信区间没有跨越零线表示处理与对照存在显著差异;若在某一分组下95%置信区间的横线之间无重叠,可认为所研究因素之间存在差异显著的统计学关联。*表示显著影响。下同
Figure 1 Response of SMBC in different soil layers to straw return to field
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