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恒温和变温模式下不同施肥黄壤有机碳矿化特征及其影响因素

朱鑫宇 卢韦 李渝 肖琼 王妍 邬磊 张文菊

植物营养与肥料学报2023,Vol.29Issue(12):2208-2218,11.
植物营养与肥料学报2023,Vol.29Issue(12):2208-2218,11.DOI:10.11674/zwyf.2023196

恒温和变温模式下不同施肥黄壤有机碳矿化特征及其影响因素

Characteristics and controlling factors of yellow soil organic carbon mineralization in different fertilization treatments under constant and variable temperature regimes

朱鑫宇 1卢韦 2李渝 3肖琼 2王妍 2邬磊 2张文菊2

作者信息

  • 1. 青岛农业大学资源与环境学院,山东青岛 266000||中国农业科学院农业资源与农业区划研究所/北方干旱半干旱耕地高效利用全国重点实验室/农业农村部耕地质量监测与评价重点实验室,北京 100081
  • 2. 中国农业科学院农业资源与农业区划研究所/北方干旱半干旱耕地高效利用全国重点实验室/农业农村部耕地质量监测与评价重点实验室,北京 100081
  • 3. 农业农村部贵州耕地保育与农业环境科学观测实验站,贵州贵阳 550006
  • 折叠

摘要

Abstract

[Objectives]Soil organic carbon(SOC)mineralization is an important process of carbon cycle in terrestrial ecosystems,and temperature changes significantly affect the characteristics of SOC mineralization.We investigated the SOC mineralization in response to constant and variable temperatures under different long-term fertilization management,so as to provide a theoretical basis for mitigating the impact of agricultural production on climate change through optimized farmland carbon management.[Methods]The soil samples were collected from the yellow soil long-term fertilization experiment at Guizhou Academy of Agricultural Sciences,with the following four treatments:no fertilizer(CK),chemical fertilizer(NPK),organic fertilizer(M),and combined organic and inorganic fertilizer(NPKM).The soil samples were incubated at constant temperature(15℃),and variable temperature(the incubation temperature changed from 10℃→15℃→20℃→15℃→10℃ at interval of 6 hours,and the cycle repeated every 24 hours)for 32 days.The CO2 effluxes were determined by NaOH absorption method,and soil physicochemical and biological properties were analyzed,in order to elucidate the characteristics of SOC mineralization and its main driving factors under different temperature modes.[Results]Under constant temperature,compared with CK treatment(201 mg/kg),the cumulative CO2 emission significantly increased by 30.6%and 13.3%in M and NPKM treatments(262 and 228 mg/kg,respectively),and decreased by 12.7%in NPK treatment(175 mg/kg).Under variable temperature condition,cumulative CO2 emission significantly increased by 30%in the M treatment relative to the CK treatment,while there was no significant difference among the CK,NPK,and NPKM treatments.Compared to constant temperature condition,cumulative CO2 emission increased by 16.2%and 25.6%for the CK and NPK treatments,respectively,under variable temperature condition.However,there was little difference in cumulative CO2 emission under constant and variable temperature conditions for the M and NPKM treatments.The cumulative CO2 emissions were significantly and positively correlated with soil pH,SOC,total nitrogen,and microbial biomass carbon(MBC)and nitrogen(MBN)among fertilization treatments under both constant and variable temperature conditions.The changes in CO2 emission induced by temperature modes were negatively correlated with soil MBC,MBN,microbial respiratory quotient,and enzyme activities related to carbon,nitrogen and phosphorus cycling.[Conclusions]Long-term application of organic fertilizer could significantly increase SOC mineralization by increasing substrate availability and microbial biomass,and mitigate the positive effects of variable temperature on SOC mineralization via changing soil microbial respiratory quotient and enzyme activities related to carbon,nitrogen,and phosphorous cycling.

关键词

土壤有机碳/矿化/温度变化/CO2累积排放量/黄壤

Key words

soil organic carbon/mineralization/temperature change/cumulative CO2 emission/yellow soil

引用本文复制引用

朱鑫宇,卢韦,李渝,肖琼,王妍,邬磊,张文菊..恒温和变温模式下不同施肥黄壤有机碳矿化特征及其影响因素[J].植物营养与肥料学报,2023,29(12):2208-2218,11.

基金项目

科技部基础资源调查专项(2021FY100501) (2021FY100501)

中央级公益性科研院所基本科研业务费专项(Y2023LM03). (Y2023LM03)

植物营养与肥料学报

OA北大核心CSCDCSTPCD

1008-505X

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