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Impacts of land-use history on the recovery of ecosystems after agricultural abandonment

机译:农业废弃后土地利用历史对生态系统恢复的影响

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Land-use changes have been shown to have large effects on climate and biogeochemical cycles, but so far most studies have focused on the effects of conversion of natural vegetation to croplands and pastures. By contrast, relatively little is known about the long-term influence of past agriculture on vegetation regrowth and carbon sequestration following land abandonment. We used the LPJ-GUESS dynamic vegetation model to study the legacy effects of different land-use histories (in terms of type and duration) across a range of ecosystems. To this end, we performed six idealized simulations for Europe and Africa in which we made a transition from natural vegetation to either pasture or cropland, followed by a transition back to natural vegetation after?20, 60?or 100?years. The simulations identified substantial differences in recovery trajectories of four key variables (vegetation composition, vegetation carbon, soil carbon, net biome productivity) after agricultural cessation. Vegetation carbon and composition typically recovered faster than soil carbon in subtropical, temperate and boreal regions, and vice versa in the tropics. While the effects of different land-use histories on recovery periods of soil carbon stocks often differed by centuries across our simulations, differences in recovery times across simulations were typically small for net biome productivity (a few decades) and modest for vegetation carbon and composition (several decades). Spatially, we found the greatest sensitivity of recovery times to prior land use in boreal forests and subtropical grasslands, where post-agricultural productivity was strongly affected by prior land management. Our results suggest that land-use history is a relevant factor affecting ecosystems long after agricultural cessation, and it should be considered not only when assessing historical or future changes in simulations of the terrestrial carbon cycle but also when establishing long-term monitoring networks and interpreting data derived therefrom, including analysis of a broad range of ecosystem properties or local climate effects related to land cover changes.
机译:土地用途的变化已显示出对气候和生物地球化学循环有很大影响,但是到目前为止,大多数研究都集中在将自然植被转化为农田和牧场的影响上。相比之下,对过去农业对土地废弃后对植被再生和碳固存的长期影响的了解知之甚少。我们使用LPJ-GUESS动态植被模型研究了一系列生态系统中不同土地利用历史(在类型和持续时间方面)的遗留效应。为此,我们对欧洲和非洲进行了六次理想化的模拟,其中我们从自然植被过渡到牧场或农田,然后在20、60或100年后又过渡到自然植被。模拟确定了农业停止后四个关键变量(植被组成,植被碳,土壤碳,净生物群落生产力)的恢复轨迹存在显着差异。在亚热带,温带和北方地区,植被碳和组成的恢复速度通常比土壤碳快,在热带地区,反之亦然。尽管在我们的模拟中不同土地利用历史对土壤碳储量恢复期的影响通常相差几个世纪,但对于净生物群落生产力(几十年)而言,模拟中恢复时间的差异通常较小,而植被碳和组成的适度变化则较小(几十年)。在空间上,我们发现北方森林和亚热带草原的恢复时间对先前土地使用的敏感性最高,因为先前土地管理极大地影响了农业后生产力。我们的结果表明,土地使用历史是影响农业停产后很长时间影响生态系统的一个相关因素,不仅在评估陆地碳循环模拟的历史或未来变化时,而且在建立长期监测网络和解释时,都应考虑土地使用历史从中得出的数据,包括对与土地覆被变化有关的广泛生态系统特性或当地气候影响的分析。

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