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关中平原麦玉轮作体系作物秸秆不同还田模式下土壤有机碳和无机碳库变化特征
引用本文:李雨诺,樊媛媛,曹彬彬,田霄鸿,师江澜. 关中平原麦玉轮作体系作物秸秆不同还田模式下土壤有机碳和无机碳库变化特征[J]. 应用生态学报, 2021, 32(8): 2703-2712. DOI: 10.13287/j.1001-9332.202108.030
作者姓名:李雨诺  樊媛媛  曹彬彬  田霄鸿  师江澜
作者单位:1.西北农林科技大学资源环境学院, 陕西杨凌 712100;2.农业部西北植物营养与农业环境重点实验室, 陕西杨凌 712100;3.农业部合阳农业环境与耕地保育科学观测实验站, 陕西合阳 715300
基金项目:国家重点研发计划项目(2016YFD0200308)、陕西省重点研发计划项目(2019ZDLNY01-05-01)和国家科技支撑计划项目(2012BAD14B11)资助
摘    要:为探究不同秸秆还田模式对土壤碳库的影响,以陕西关中平原连续11年麦玉秸秆还田定位试验为基础,选择5种还田模式,即秸秆均不还田(CK)、小麦高留茬-玉米秸秆粉碎还田(WH-MC)、小麦玉米秸秆均粉碎还田(WC-MC)、小麦高留茬-玉米秸秆不还田(WH-MN)和小麦秸秆粉碎还田-玉米秸秆不还田(WC-MN),测定不同模式土...

关 键 词:秸秆还田模式  土壤有机碳  土壤无机碳  土壤碳固持
收稿时间:2021-01-07

Soil organic and inorganic carbon pools as affected by straw return modes under a wheat-maize rotation system in the Guanzhong Plain,Northwest China
LI Yu-nuo,FAN Yuan-yuan,CAO Bin-bin,TIAN Xiao-hong,SHI Jiang-lan. Soil organic and inorganic carbon pools as affected by straw return modes under a wheat-maize rotation system in the Guanzhong Plain,Northwest China[J]. The journal of applied ecology, 2021, 32(8): 2703-2712. DOI: 10.13287/j.1001-9332.202108.030
Authors:LI Yu-nuo  FAN Yuan-yuan  CAO Bin-bin  TIAN Xiao-hong  SHI Jiang-lan
Affiliation:1.College of Natural Resources and Environment, Northwest A&F University, Yangling 712100, Shaanxi, China;2.Key Laboratory of Plant Nutrition and Agro-environment in Northwest China, Ministry of Agriculture, Yangling 712100, Shaanxi, China;3.Scientific Observing and Experimental Station of Arable Land Conservation (Heyang), Ministry of Agriculture, Heyang 715300, Shaanxi, China
Abstract:To understand the effects of straw return modes on soil carbon pools, we investigated total soil organic carbon (SOC), labile organic carbon fractions, and inorganic carbon (SIC) in different straw return modes at a depth of 0-40 cm under a maize-wheat cropping system in the Guanzhong Plain, Shaanxi, based on an 11-year field experiment. There were five straw return modes, i.e., no return of straw of both wheat and maize (CK), the retention of high wheat stubble plus the return of chopped maize straw (WH-MC), the return of both chopped wheat and maize straw (WC-MC), the retention of high wheat stubble and no return of maize straw (WH-MN), and the return of chopped wheat straw and no return of maize straw (WC-MN). The proportions of SOC storage were significantly higher under the WH-MC and WC-MC treatments than that under the CK by 28.1% and 22.2%, respectively. The proportions of SIC storage were increased by 20.4% and 17.3%, respectively. Compared with the initial value, the increases of sequestered SOC and SIC ranged from -0.84 t·hm-2 to 6.55 t·hm-2, respectively, and from -0.26 t·hm-2 to 8.61 t·hm-2, respectively. The efficiency of sequestration of SOC was 7.5%. To maintain the basic SOC level, the minimum carbon input from straw was 4.65 t·hm-2·a-1. The contents of labile carbon fractions at the 0-20 cm layer increased significantly under the WH-MC and WC-MC treatments compared with those of the control. Results of principal component analysis showed that the changes in soil carbon pools were primarily affected by the amount of straw return. Additionally, the increases in SIC storage could be ascribed to the Ca2+ and Mg2+ ions derived from irrigation water and plant residues that could coprecipitate with the CO2 from SOC mineralization to form CaCO3. In conclusion, our results indicated that the straw return mode that utilized the retention of high wheat stubble and chopped maize straw was sufficient to maintain soil carbon storage and would be the optimal straw-returning strategy for the region.
Keywords:straw return mode  soil organic carbon (SOC)  soil inorganic carbon (SIC)  soil carbon sequestration  
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