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Effects of land use change and management on the European cropland carbon balance

机译:土地利用变化和管理对欧洲农田碳平衡的影响

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We model the carbon balance of European croplands between 1901 and 2000 in response to land use and management changes. The process-based ORCHIDEE-STICS model is applied here in a spatially explicit framework. We reconstructed land cover changes, together with an idealized history of agro-technology. These management parameters include the treatment of straw and stubble residues, application of mineral fertilizers, improvement of cultivar species and tillage. The model is integrated for wheat and maize during the period 1901-2000 forced by climate each 1/2-hour, and by atmospheric CO2, land cover change and agro-technology each year. Several tests are performed to identify the most sensitive agro-technological parameters that control the net biome productivity (NBP) in the 1990s, with NBP equaling for croplands the soil C balance. The current NBP is a small sink of 0.16 t C ha-1 yr-1. The value of NBP per unit area reflects past and current management, and to a minor extent the shrinking areas of arable land consecutive to abandonment during the 20th Century. The uncertainty associated with NBP is large, with a 1-sigma error of 0.18 t C ha-1 yr-1 obtained from a qualitative, but comprehensive budget of various error terms. The NBP uncertainty is dominated by unknown historical agro-technology changes (47%) and model structure (27%), with error in climate forcing playing a minor role. A major improvement to the framework would consist in using a larger number of representative crops. The uncertainty of historical land-use change derived from three different reconstructions, has a surprisingly small effect on NBP (0.01 t C ha-1 yr-1) because cropland area remained stable during the past 20 years in all the tested land use forcing datasets. Regional cross-validation of modeled NBP against soil C inventory measurements shows that our results are consistent with observations, within the uncertainties of both inventories and model. Our estimation of cropland NBP is however likely to be biased towards a sink, given that inventory data from different regions consistently indicate a small source whereas we model a small sink.
机译:我们对1901年到2000年之间欧洲土地的碳平衡进行了建模,以响应土地使用和管理方式的变化。在此,基于过程的ORCHIDEE-STICS模型在空间明确的框架中应用。我们重建了土地覆被变化以及理想化的农业技术历史。这些管理参数包括秸秆和残茬的处理,矿物肥料的使用,改良品种和耕作。该模型针对1901-2000年期间的小麦和玉米进行了集成,该模型受气候每1/2小时,每年的大气CO2,土地覆盖变化和农业技术的强迫。进行了几次测试,以确定最敏感的农业技术参数,这些参数控制着1990年代的净生物群落生产力(NBP),其中NBP等于农田的土壤碳平衡。当前的NBP是一个0.16 t C ha-1 yr-1的小汇。每单位面积的NBP值反映了过去和当前的管理方式,在较小程度上反映了20世纪连续废弃的耕地面积的缩小。与NBP相关的不确定性很大,从各种误差项的定性但综合预算中获得的1-sigma误差为0.18 t C ha-1 yr-1。 NBP的不确定性主要由未知的历史农业技术变化(47%)和模型结构(27%)决定,气候强迫误差起着较小的作用。该框架的一项重大改进将包括使用大量代表性作物。来自三种不同重建方法的历史土地利用变化的不确定性,对NBP(0.01 t C ha-1 yr-1)的影响极小,因为在所有测试的土地利用强迫数据集中,过去20年中耕地面积保持稳定。建模的NBP对土壤C清单测量的区域交叉验证表明,在清单和模型的不确定性范围内,我们的结果与观测结果一致。但是,考虑到来自不同地区的库存数据始终表明来源较小,而我们模拟的是较小的汇区,因此我们对农田NBP的估计可能会偏向汇区。

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