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首页> 外文期刊>Agricultural sciences in China >Profile Distribution and Storage of Soil Organic Carbon in an Aquic Brown Soil as Affected by Land Use
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Profile Distribution and Storage of Soil Organic Carbon in an Aquic Brown Soil as Affected by Land Use

机译:土地利用对棕褐色土层有机碳剖面分布和储量的影响

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摘要

Many attempts have been made to estimate the soil organic carbon (SOC) storage under different land uses, especially from the conversion of forest land or grassland into cultivated field, but limited reports were found on the estimation of this storage after cultivated field converted into woodland or grassland, especially in small scales. This study is aimed to investigate the dynamics of SOC concentration, its storage and carbon itrogen (C/N) ratio in an aquic brown soil at the Shenyang Experimental Station of Ecology, Chinese Academy of Sciences under four land use patterns over 14 years. The four land use patterns were paddy field (PF), maize field (MF), fallow field (FF) and woodland (WL). In each pedon at 0-150 cm depth, soil samples were collected from ten layers. The results showed that the profile distribution of SOC was different under different land uses, indicating the effect of land use on SOC. Soil organic carbon was significantly related with soil total N, and the correlation was slightly closer in nature ecosystems (with R=0.990 and P<0.001 in both WL and FF, n=30) than in agroecosystems (with R~2=0.976 and P<0.001 in PF, and R=0.980 and P<0.001 in MF, n=30). The C/N ratio in the profiles decreased generally with depth under thefour land use patterns, and was comparatively higher in WL and lower in PF. The C/N ratio of the FF was closer to that in the same soil depths of MF than to that of PF. Within 100 cm depth, the annual sequestration of SOC was 4.25, 2.87, and 4.48 t ha~(-1) more in WL than in PF, MF and FF, the annual SOC increasing rate being 6.15, 3.26, and 5.09 % higher, respectively. As a result, the SOC storage was significantly greater in WL than in any of the other three land use patterns, P=0.001, 0.008, and 0.008 as compared with PF, MF, and FF, respectively, while there was no significant difference among the other three land uses. It is suggested that woodland has the potential to make a significant contribution to C storage and environmental quality.
机译:已经进行了许多尝试来估计不同土地利用下土壤有机碳(SOC)的存储量,特别是从林地或草地向耕地的转化方面,但是在将耕地转化为林地后,对这种存储量的估算的报道却很少。或草地,尤其是小规模的草地。这项研究旨在研究中国科学院沉阳生态实验站水生褐土中SOC浓度,其储存和碳/氮(C / N)比在14年内四种土地利用方式下的动态。四种土地利用方式分别是稻田(PF),玉米田(MF),休耕田(FF)和林地(WL)。在0-150 cm深度的每个脚架上,从十层收集土壤样品。结果表明,不同土地利用方式下SOC的分布特征不同,说明土地利用对SOC的影响。土壤有机碳与土壤总氮显着相关,自然生态系统(WL和FF均为R = 0.990,P <0.001,n = 30)与农业生态系统(R〜2 = 0.976和R> 2)之间的相关性更接近。 PF中的P <0.001,MF中的R = 0.980和P <0.001,n = 30)。在四种土地利用方式下,剖面的C / N比通常随深度而降低,WL相对较高,PF较低。在相同土壤深度下,FF的C / N比更接近于PF。在100 cm深度内,WL中的SOC年度隔离量比PF,MF和FF高出4.25、2.87和4.48 t ha〜(-1),年SOC增长率分别高出6.15、3.26和5.09%,分别。结果,与PF,MF和FF相比,WL中的SOC储存量显着大于其他三种土地利用方式中的任何一个,P = 0.001、0.008和0.008,而在两者之间没有显着差异。其他三个土地用途。建议林地有潜力为碳储存和环境质量做出重大贡献。

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