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关中地区农田土壤有机碳固存速率及影响因素:以陕西武功县为例
引用本文:张晓伟,许明祥.关中地区农田土壤有机碳固存速率及影响因素:以陕西武功县为例[J].环境科学,2013,34(7):2793-2799.
作者姓名:张晓伟  许明祥
作者单位:1. 西北农林科技大学资源环境学院,杨凌,712100
2. 中国科学院水利部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,杨凌,712100
基金项目:中国科学院战略性先导科技专项(XDA05050504); 中国科学院知识创新工程重要方向项目(KZCX2-YW-443); 国家自然科学基金项目(41171422)
摘    要:以武功县为例,通过计算农田土壤碳储量及固碳速率,明确关中地区农田土壤有机碳动态变化的规律,进而揭示农田土壤有机碳与自然因素、人为因素的关系.结果表明:①80%的样点0~20 cm农田土壤有机碳含量在8.0~12.0 g.kg-1之间,总体上呈现正态分布.②武功县2011年0~20 cm农田土壤有机碳密度为26.3 t.hm-2,低于全国农田耕层土壤有机碳密度平均水平(33.45 t.hm-2).近30年农田土壤固碳速率为71.3 kg.(hm2.a)-1,近5年农田土壤固碳速率为480 kg.(hm2.a)-1,近期固碳速率高于全国农田耕层土壤平均固碳速率380.78 kg.(hm2.a)-1].③在半湿润平原地区,土壤有机碳含量主要受土壤类型、地貌类型、有机肥投入的影响,其中土壤类型可解释30.2%的有机碳变异性,地貌类型可解释37.7%,有机肥可解释32.1%.综合分析表明,武功县农田土壤有机碳密度在过去30 a间呈增加趋势,这可能与化肥的施用和秸秆还田有关,具体有多大的影响程度还需进一步研究.

关 键 词:关中地区  农田  有机碳  固存速率  影响因素
收稿时间:2012/10/30 0:00:00
修稿时间:2012/12/28 0:00:00

Soil Organic Carbon Sequestration Rate and Its Influencing Factors in Farmland of Guanzhong Plain: A Case Study in Wugong County, Shannxi Province
ZHANG Xiao-wei and XU Ming-xiang.Soil Organic Carbon Sequestration Rate and Its Influencing Factors in Farmland of Guanzhong Plain: A Case Study in Wugong County, Shannxi Province[J].Chinese Journal of Environmental Science,2013,34(7):2793-2799.
Authors:ZHANG Xiao-wei and XU Ming-xiang
Institution:College of Resource and Environment, Northwest A&F University, Yangling 712100, China;State Key Laboratory of Soil Erosion and Dry land Farming on Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resource, Yangling 712100, China
Abstract:Take Wugong County as an example, soil carbon storage and soil carbon sequestration rate were calculated, the change law of farmland soil organic carbon was explored, and the relationship of farmland soil organic carbon and natural factors, human factors was further revealed. The results of the study showed that: 1The soil organic carbon contents in 80% of the sampling sites were in the range of 8.0-12.0 g·kg-1, and the organic carbon contents in 0-20 cm soils showed a normal distribution. 2In 2011, the organic carbon density of the 0-20 cm farmland soil was 26.3 t·hm-2, below the national average soil organic carbon density (33.45 t·hm-2) of the arable layer. In the last 30 years, the soil carbon sequestration rate in the 0-20 cm layer was 71.3 kg·(hm2·a)-1, and in the past five years, the carbon sequestration rate was 480 kg·(hm2·a)-1. The recent carbon sequestration rate was higher than the national average soil carbon sequestration rate of the arable layer380.78 kg·(hm2·a)-1 ]. 3In the semi-humid plain region, soil organic carbon was mainly affected by soil types, landform types, organic fertilizer. Soil types accounted for 30.2% of the organic carbon variability; the landform types and the organic fertilizer could explain 37.7% and 32.1%, respectively. The results of the comprehensive analysis showed that the farmland soil organic carbon density of Wugong County in the past 30 years is increasing, and this probably relies on the utilization of chemical fertilizer and the returning straw. Further study should be conducted on the impact of the chemical fertilizer and returning straw.
Keywords:Guanzhong Plain  farmland  soil organic carbon  sequestration rate  influencing factors
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