哥伦比亚东部酸性土壤稀树草原牧场集约化策略对牛群产量和碳足迹影响的动态模拟模型

Raul R. Vera-Infanzón, I. Rao, C. Ramírez-Restrepo
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引用次数: 2

摘要

东哥伦比亚(Llanos)的新热带稀树草原受到与牛肉生产集约化相关的土地利用变化的影响,对这些变化过程的长期影响的了解有限。此外,通过引入播种牧场在农场层面上的时空强化对肉牛群产量、其温室气体(GHG)排放以及在大草原不同景观下产生的碳(C)足迹的影响尚不清楚。本研究旨在评估通过在哥伦比亚排水良好的东部稀树草原的两种截然不同的景观(可耕作的平坦稀树草原和高度分割的牧场)中引入播种的热带牧场,逐步进行系统集约化的后果,包括小牛产量和温室气体排放以及由此产生的碳足迹。开发了一个动态模型来模拟两种类型的热带牧场的逐渐引入,一种是在一个有陡峭的斜坡和有限的可耕地区,牛也可以进入塞尔维亚稀树草原和播种的牧场,另一种是在平原上,随着时间的推移,完全改变了原生牧场。随着时间的推移,畜群数量、动物产量和排放量都发生了显著变化。所有系统的碳足迹随时间而变化,这取决于牧场对土壤有机碳积累的贡献时间长短以及整个农场水平上稀树草原和播种草场之间的平衡。综上所述,集约化系统的动态是显著的,并且依赖于播种牧草资源的时空配置。因此,将整个区域的趋势一概而论会导致不确定性。然而,对模拟原型的检查可能会揭示预期的趋势,并为决策提供指导
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A dynamic simulation model to assess farm-level effects of pasture intensification strategies on beef herd outputs and carbon footprints in acid soil savannas of Eastern Colombia
The neotropical savannas of Eastern Colombia (Llanos) are subjected to changes in land use associated with intensification of beef production and there is limited knowledge on the long-term impacts of these change processes. Furthermore, the effects of spatial and temporal intensification at farm level via the introduction of sown pastures on beef herd outputs, their greenhouse gas (GHG) emissions and the resulting carbon (C) footprints in contrasting savanna landscapes of of the Llanos are unknown. This study was aimed to assess the consequences of gradual system intensification via introduction of sown tropical pastures in two contrasting landscapes, the tillable, flat savannas and the highly dissected rangelands, of the well-drained Eastern savannas of Colombia, in terms of cow-calf production and GHG emissions and the resulting C footprints. A dynamic model was developed to simulate the gradual introduction of two types of tropical pastures in a region with dissected and steep slopes and limited tillable areas where cattle would also have access to Serrania savanna and sown pastures, versus one located in the Plains that are fully transformed over time with the exclusion of native rangelands. Marked changes in herd demography, animal outputs, and emissions were found over time. The C footprint of all systems varied over time depending upon the length of time that pastures contributed to soil organic carbon accumulation and the balance between savanna and sown pasture areas at a whole farm level. In conclusion, the dynamics of the systems subject to intensification were marked and were dependent on the temporal and spatial deployment of sown forage resources. Therefore, generalizing the trends for the region as a whole result in uncertainty. Nevertheless, examination of simulated prototypes may shed light on the expected trends and provides guidance for decision-making
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