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长期施肥红壤矿物颗粒结合有机碳储量及其固定速率
引用本文:佟小刚,;王伯仁,;徐明岗,;张文菊.长期施肥红壤矿物颗粒结合有机碳储量及其固定速率[J].农业环境保护,2009(12):2584-2589.
作者姓名:佟小刚  ;王伯仁  ;徐明岗  ;张文菊
作者单位:[1]中国农业科学院农业资源与农业区划研究所/农业部作物营养与施肥重点开放实验室,北京100081; [2]西北农林科技大学资源环境学院,陕西杨凌712100
基金项目:国家自然科学基金(40871148);“十一五”国家重点科技支撑计划项目(2006BAD02A14,2006BAD05809);中央级公益性科研院所基本科研业务费专项资金(2009-17)
摘    要:采用物理分组方法分析了长期不同施肥模式下红壤耕层(0—20cm)不同大小矿物颗粒结合态有机碳储量差异及其固定速率。结果表明,与不施肥相比,长期施肥均显著增加了耕层土壤砂粒、粗粉粒、细粉粒及粗黏粒结合有机碳的储量,且以配施有机肥(M、NPKM和1.5NPKM)效果最显著,固碳速率分别达到0.13-0.24、0.19-0.23、0.05-0.16及0.12~0.36Mg·hm^-2.a^-1;施化肥(NPK、NP、N)和秸秆还田(NPKS)有利于增加细黏粒有机碳储量,且固碳速率高于配施有机肥,分别达到0.08~0.13和0.11Mg·hm^-2·a^-1。17a有机肥配施有利于增加固存于粗粉粒(30.5%)和粗黏粒(30.7%)中的有机碳;而秸秆还田(NPKS)和化肥施用下,有利于增加固存于粗粉粒(32.9%)和细黏粒(42.9%)中的有机碳,说明无论化肥配施还是有机无机配施,红壤粗粉粒是固定新增有机碳的主要组分,而长期配施有机肥是提升红壤各级颗粒有机碳库的较好施肥模式。

关 键 词:长期施肥  有机碳  储量  土壤颗粒  红壤

Change Characteristics of Organic Carbon Stocks and Sequestration Rate of Particle-size Fractions in Red Soil Under Long-term Fertilizations
Institution:TONG Xiao-gang, WANG Bo-ren, XU Ming-gang, ZHANG Wen-ju( 1.Key Laboratory of Crop Nutrition and Fertilization, Ministry of Agriculture/Institute of Agricuhural Resources and Regional Planning , CAAS, Beijing 100081, China, 2.College of Resource and Environment, Northwest Sci-Tech University of Agriculture and Forestry, Yangling 712100, China)
Abstract:The density fractionation scheme was used to study change characteristics of organic carbon stocks and sequestration rate of particle-size fractions in red soil under long-term fertilization. Our results showed that compared to non-fertilization (CK), long-term fertilization significantly increased the organic carbon stock that combined with sand( S ), coarse silt( CS ), fine silt( FS ), and coarse clay( CC ). Especially, applications with manure( M, NPKM, 1.5NPKM) showed highest carbon sequestration rate in S-OC(0.13-0.24 Mg·hm^-2·a^-1), CS(0.19-0.23 Mg·hm^-2·a^-1 ), FS ( 0.05-0.16 Mg·hm^-2·a^-1 ), and CC (0.12-0.36 Mg·hm^-2·a^-1 ), respectively. Applications of chemical fertilizers ( NPK, NP, N ) and straw incorporation were more effective to increase organic carbon in FC and the carbon sequestration rate were 0.08-0.13 and 0.11 Mg·hm^-2·a^-1 respectively, which were higher than the rates of applications with manure,. Applications with manure were apt to sequester more organic carbon in the CS( 30.5% ) and CC (30.7%) particles. However, application of straw incorporation (NPKS) and chemical fertilizers sequenstered more organic carbon in CS( 32.9% ) and FC(42.9% ) particles. Therefore, CS was the main carbon pool that sequestrated organic carbon in red soil under long-term fertilization. Moreover, long-term application with manure was helpful fertilization practices to increase Organic carbon in all particle-size fractions of red soil.
Keywords:long-term fertilization  organic carbon  reserves  particle-size fractions  red soil
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