未来温度升高对福建省耕地土壤有机碳的影响研究
Imapcts of Atmospheric Temperature on Organic Carbon Dynamic Change of Cropland in Fujian Province
未来气温升高对耕地土壤有机碳收支平衡有重要的影响。本研究运用生物地球化学模型DNDC(DeNitrification-DeComposition, 9.5版本)和我国典型亚热带地区-福建省不同地理位置的闽侯、浦城、同安、武平、永定5个县2008年15948个耕地地力调查样点数据建成的1:5万土壤数据库,利用尺度上推的方法分析了未来温度上升2℃和4℃对福建省耕地土壤有机碳的影响。结果表明,在正常温度变化、温度上升2℃和4℃的3种情景分析下福建省耕地2011-2040年分别固碳7.04 Tg、5.62 Tg和4.27 Tg,年均有机碳变化量分别为175.94 kg/hm2、140.54 kg/hm2和106.81 kg/hm2。从不同土类来看,温度上升2℃和4℃情景对潮土土类的影响最大,年均有机碳变化量分别比正常温度变化处理低51.00 kg/hm2和80.69 kg/hm2,而对滨海盐土土类的影响最小,年均有机碳变化量分别比正常温度变化处理低22.54 kg/hm2和54.25 kg/hm2。从土壤亚类来看,温度上升2℃和4℃情景处理下受影响最大的分别是灰潮土和潜育水稻土,年均有机碳变化量分别比正常温度变化处理低51.00 kg/hm2和102.17 kg/hm2,而受影响最小的都是淹育水稻土,年均有机碳变化量分别比正常温度变化处理低20.20 kg/hm2和42.14 kg/hm2。可见,未来温度升高将明显的降低福建省耕地土壤有机碳的"碳汇"能力。因此,通过制定合理的农业措施来减弱将来温度升高所造成的"碳源"效应是非常重要的。
Future temperature increased had significant impact to balance of Payments of cropland. The study utilized biogeochemical model DNDC (DeNitrification-DeComposition, 9.5),with the database of 1:50000 for soil database according to the measure values of 15,948 sampling point in year 2008, took five typical county (Tong,an, Pucheng, Wuping, Yongding, and Minhou) in different geographic locations from Fujian Province in subtropical regions as the study area, analyzed the change rule of soil organic carbon in Fujian province and explored the "cardon source/sink" effect of 3 possible atmospheric temperature scenario in soils of Fujian province from 2011 to 2040 . The main research conclusions were as follows: According to the verification result at the regional scale, the results indicated that DNDC model has a good performance on simulating the SOC dynamics for the soils of Fujian province. carbon fixation of soil in Fujian province of temperature increased 2℃ and 4℃ 2 scenarios was 5.62 Tg and 4.27 Tg respectively, the dSOC of cropland were 175.94 kg/hm2,140.54 kg/hm2 and 106.81 kg/hm2. Compared with conventional temperature scenario, the temperature increased 2℃ and 4 ℃ scenario, the fluvo-aquic soils organic carbon decreased 51.00 kg/hm2 and 80.69 kg/hm2 each year respectively. The variable quantity was the greatest change in all soil groups. The coastal soloncharks organic carbon decreased 22.54 kg/hm2 and 54.25 kg/hm2 every year respectively. The variable quantity was the smallest change in all soil groups. The analysis from the soil subgroups. Compared with conventional temperature scenario, the temperature increased 2℃ and 4℃ scenario, grey fluvo-aquic soils and gley paddy soils organic carbon decreased 51.00 kg/hm2 and 102.17 kg/hm2 each year and it is the greatest change in all soil subgroups. Submergenic paddy soils organic carbon decreased 20.20 kg/hm2 and 42.14 kg/hm2 each year in two scenario, and it is the smallest change in all soil subgroups. Temperature increased significantly decreased the "cardon source" capacity of Fujian province cropland. It is important to take reasonable agriculture measures to reduce "cardon sink" effect which caused by temperature increased.
邱壑、陈霖、张黎明、陈小梅、位佳、邢世和、黄琳斌
农业科学研究环境科学基础理论环境污染、环境污染防治
NDC模型耕地有机碳温度变化
NDC model cropland organic carbon atmospheric temperature
邱壑,陈霖,张黎明,陈小梅,位佳,邢世和,黄琳斌.未来温度升高对福建省耕地土壤有机碳的影响研究[EB/OL].(2014-05-14)[2025-08-11].http://www.paper.edu.cn/releasepaper/content/201405-217.点此复制
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