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应用生态学报 ›› 2022, Vol. 33 ›› Issue (6): 1475-1481.doi: 10.13287/j.1001-9332.202206.013

• 稳定同位素生态学专栏 • 上一篇    下一篇

不同施肥条件下秸秆碳在表层和深层土壤团聚体中的分配与固存

段佳茹1, 王淑颖1, 李小红1, 徐香茹2, 梅秀文1, 安婷婷1*, 汪景宽1   

  1. 1沈阳农业大学土地与环境学院/农业部东北耕地保育重点实验室/土肥资源高效利用国家工程实验室, 沈阳 110866;
    2江苏大学农业工程学院, 江苏镇江 212013
  • 收稿日期:2021-09-06 接受日期:2022-04-05 出版日期:2022-06-15 发布日期:2022-12-15
  • 通讯作者: *E-mail: atting@syau.edu.cn
  • 作者简介:段佳茹, 女, 1997年生, 硕士研究生。主要从事土壤肥力研究。E-mail: duanjiaru163@163.com
  • 基金资助:
    辽宁省科学研究经费(LSNQN202008)、国家自然科学基金项目(41977086)和中国博士后科学基金项目(2021M691316)资助。

Distribution and sequestration of straw carbon in surface and deep soil aggregates under different fertilization treatments

DUAN Jia-ru1, WANG Shu-ying1, LI Xiao-hong1, XU Xiang-ru2, MEI Xiu-wen1, AN Ting-ting1*, WANG Jing-kuan1   

  1. 1College of Land and Environment, Shenyang Agricultural University/Key Laboratory of Northeast Arable Land Conservation, Ministry of Agriculture and Rural Affair/National Engineering Laboratory for Efficient Utilization of Soil and Fertilizer Resources, Shenyang 110866, China;
    2College of Agricultural Engineering, Jiangsu University, Zhenjiang 212013, Jiangsu, China
  • Received:2021-09-06 Accepted:2022-04-05 Online:2022-06-15 Published:2022-12-15

摘要: 长期施肥引起表层和深层土壤水、热、养分和微生物活性的分异,进而影响秸秆碳在土壤中的分解和周转过程。本研究基于沈阳农业大学长期定位实验站,分别将不同施肥处理表层(0~20 cm)和深层(40~60 cm)土壤与13C标记秸秆混合进行田间试验,通过分析团聚体中有机碳含量和δ13C值,对比秸秆碳在表层和深层土壤团聚体中分配的差异,探讨施肥对秸秆碳在土壤团聚体中固定的影响。结果表明: 与施肥(包括单施氮肥和有机肥配施氮肥)处理相比,不施肥处理分别使表层土壤<0.053 mm和深层土壤>0.25 mm团聚体中秸秆碳含量增加了106.7%和34.2%;秸秆碳对深层土壤>0.053 mm团聚体有机碳的贡献率约为表层土壤的2.0倍;秸秆碳分配到表层土壤>0.25 mm和<0.25 mm团聚体的比例平均分别为22.6%和11.4%,分配到深层土壤的相应比例分别为29.4%和8.8%。总之,秸秆添加促进了深层土壤大团聚体碳源的更新和固存,提高了深层土壤的固碳潜力。

关键词: 团聚体, 秸秆碳, 深层土壤, 13C标记, 施肥

Abstract: Long-term fertilization causes the differences in water, heat, nutrients and microbial activities between topsoil and deep soil, with consequences on the decomposition and turnover of straw carbon (C) in soils. At a long-term positioning experimental station in Shenyang Agricultural University, we mixed the topsoil (0-20 cm) and deep soil (40-60 cm) samples from different fertilization treatments with 13C-labeled straw for in-situ incubation. We analyzed the content of organic C and its δ13C value in soil aggregates, compared the difference in the distribution of straw C between topsoil and deep soil aggregates, and explored the effects of fertilization on the sequestration of straw C in soil aggregates. Compared with fertilization treatments (i.e., single chemical nitrogen fertilizer application and combination of organic manure with nitrogen fertilizer application), the treatment without fertilization increased the content of straw C of <0.053 mm aggregate in the topsoil by 106.7% and that of >0.25 mm aggregate in the deep soil by 34.2%. The contribution percentage of straw C to organic C of >0.053 mm aggregate in the deep soil was about two times of that in the topsoil. About 22.6% and 11.4% of straw C was distributed into the >0.25 mm and <0.25 mm aggregates of topsoil, and about 29.4% and 8.8% of straw C was distributed into the >0.25 mm and <0.25 mm aggregates of deep soil, respectively. In conclusion, straw addition promoted the regeneration and sequestration of carbon in deep soil macroaggregates and increased the carbon sequestration potential of deep soil.

Key words: aggregate, straw carbon, deep soil, 13C-labeling, fertilization