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氮磷添加下黄土丘陵区退耕草地土壤呼吸速率日变化特征
引用本文:陈阳,周俊杰,陈志飞,简春霞,赖帅彬,徐炳成. 氮磷添加下黄土丘陵区退耕草地土壤呼吸速率日变化特征[J]. 中国环境科学, 2021, 41(12): 5779-5792
作者姓名:陈阳  周俊杰  陈志飞  简春霞  赖帅彬  徐炳成
作者单位:1. 西北农林科技大学水土保持研究所, 黄土高原土壤侵蚀与旱地农业国家重点实验室, 陕西 杨凌 712100;2. 中国科学院水利部水土保持研究所, 陕西 杨凌 712100
基金项目:国家重点研发计划(2016YFC0501703);国家自然科学基金资助项目(41771553)
摘    要:为探究黄土丘陵区退耕草地土壤呼吸及其组分日变化对氮磷添加的响应,采用裂区试验设计,主区施氮[0,50和100kg N/(hm2·a)]和副区施磷[0,40和80kgP2O5/(hm2·a)],于2019年5~8月每月测定各处理下土壤呼吸速率、异养呼吸速率及土壤温度和含水量日变化.结果表明,土壤呼吸速率及其组分日变化均呈...

关 键 词:土壤呼吸  自养呼吸  异养呼吸  氮磷添加  温度敏感性
收稿时间:2021-05-10

Effects of nitrogen and phosphorus addition on diurnal variations of soil respiration rate in the grassland and farm withdrawing cultivation on Loess Hilly-gully Region
CHEN Yang,ZHOU Jun-jie,CHEN Zhi-fei,JIAN Chun-xia,LAI Shuai-bin,XU Bing-cheng. Effects of nitrogen and phosphorus addition on diurnal variations of soil respiration rate in the grassland and farm withdrawing cultivation on Loess Hilly-gully Region[J]. China Environmental Science, 2021, 41(12): 5779-5792
Authors:CHEN Yang  ZHOU Jun-jie  CHEN Zhi-fei  JIAN Chun-xia  LAI Shuai-bin  XU Bing-cheng
Affiliation:1. State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, China;2. Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling 712100, China
Abstract:In order to explore the response characteristics of soil respiration (Rs) and its components (heterotrophic respiration, Rh; and autotrophic respiration, Ra) to N and P additions in the grassland and farm withdrawing cultivation, a field split-plot experiment was performed including: [main-plots with 0, 50, and 100kg N/(hm2·a)]; and [subplots: with 0, 40 and 80kg P2O5/(hm2·a)]. Such treatments were made every month from May to August in 2019 and for each treatment, these treatments were made: diurnal variations of Rs and Rhand Ra, soil temperature (Ts) and soil water content. Results showed that the diurnal variations of Rs and its two components (i.e. Rh and Ra) showed single-peak curves across all N and P addition treatments, and all reached the maximum values between 12:00~14:00. Compared with no fertilization treatment (CK), Rs, Rh and Ra increased significantly under N addition by 7.31%~13.13%, 1.12%~12.43% and 7.64%~46.26%, respectively, and increased significantly under P addition by 16.84%~18.42%, 11.48%~14.22% and 17.15%~29.59% respectively. N and P combined addition increased Rs, Rh and Ra by 24.17%~27.30%, 21.94%~32.43% and 34.05%~41.26%, respectively. The daytime proportions of whole day carbon emissions from Rs, Rh and Ra under different N and P addition treatments accounted for 52.68%~61.37%, 50.92%~58.70% and 51.39%~76.35%, respectively. The cumulative CO2emission was the highest at 2012g/m2 under a treatment of 50kg N/(hm2·a) combined with 80kg P2O5/(hm2·a), and the lowest appeared under no fertilization treatment at 1531g/m2. Rs and its two components (Rh and Ra) were significantly positively correlated with the soil temperature (Ts), and their temperature sensitivity (Q10) ranged from 1.19 to 1.86, 1.08 to 1.81, and 1.11 to 3.67, respectively. N and P decreased the Q10 values of Rh, but increased the Q10 values of Ra. In summary, N and P additions increase the rates of Rs and its two components, but decreased the temperature sensitivity of Rh, and the effect of N and P addition on soil respiration rate were related to N and P addition amounts and their ratios.
Keywords:soil respiration  autotrophic respiration  heterotrophic respiration  nitrogen and phosphorus addition  temperature sensitivity  
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