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首页> 外文期刊>Agroforestry Systems >Productivity and carbon storage in silvopastoral systems with Pinus ponderosa and Trifolium spp., plantations and pasture on an Andisol in Patagonia, Chile
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Productivity and carbon storage in silvopastoral systems with Pinus ponderosa and Trifolium spp., plantations and pasture on an Andisol in Patagonia, Chile

机译:智利巴塔哥尼亚Andisol上的黄松和白三叶,人工林和牧场的牧草牧系统的生产力和碳储量

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摘要

No information is available about carbon (C) sequestration potentials in ecosystems on Andisols of the Chilean Patagonia. This study was undertaken to measure the size of C stocks in three predominant ecosystems: Pinus ponderosa-based silvopastoral systems (SPS), pine plantations (PPP) and natural pasture (PST), and examine how clover affect tree growth and stocks of soil C. The C contents of trees and pasture were determined by destructive sampling and dry combustion. Soil samples were taken at 0-5, 5-20, 20-40 cm depths in order to determine soil C and N. For PPP and SPS total aboveground tree C was 38.4 and 53.1 kg tree-1 and belowground was 21.3 and 23.4 kg tree-1, respectively. Annual diameter increment at breast height was 1 and 2 cm in PPP and SPS, respectively, and was significantly higher in SPS. Trees in SPS, due to lower density and the presence of leguminous pasture, demonstrated enhanced growth and C sequestration. Soil organic C (SOC) stocks at 0-40 cm depth were 193.76, 177.10 and 149.25 Mg ha-1 in SPS, PST and PPP, respectively. The conversion of PPP to SPS and PST to PPP resulted in an increase of 44.51 Mg ha-1 and a decrease of 27.85 Mg ha-1 in SOC, respectively. Favorable microclimatic conditions in relation to air temperature and soil moisture were observed in SPS as well as a synergy between trees and pasture.
机译:没有有关智利巴塔哥尼亚Andisols生态系统中碳(C)螯合潜力的信息。这项研究的目的是测量三个主要生态系统中的C储量:基于黄松的营林牧草系统(SPS),松树人工林(PPP)和天然牧场(PST),并研究三叶草如何影响树木生长和土壤C储量通过破坏性采样和干烧测定树木和牧场的碳含量。确定土壤C和N的深度为0-5、5-20、20-40 cm,取土样。对于PPP和SPS,地上树的总C为38.4和53.1 kg树 -1 地下分别是21.3和23.4 kg树 -1 。在PPP和SPS中,乳房高度处的年直径增量分别为1和2 cm,在SPS中显着更高。由于密度较低和豆科牧草的存在,SPS中的树木表现出增强的生长和固碳能力。 SPS,PST和PPP中0-40 cm深度的土壤有机碳(SOC)储量分别为193.76、177.10和149.25 Mg ha -1 。 PPP转换为SPS和PST转换为PPP导致SOC分别增加44.51 Mg ha -1 和减少27.85 Mg ha -1 。在SPS中观察到与气温和土壤湿度有关的有利微气候条件,以及树木和牧场之间的协同作用。

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