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Impacts of conversion of tropical peat swamp forest to oil palm plantation on peat organic chemistry, physical properties and carbon stocks

机译:热带泥炭沼泽森林向油棕种植的转化对泥炭有机化学,物理性质和碳储量的影响

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摘要

Ecosystem services provided by tropical peat swamp forests, such as carbon (C) storage and water regulation, are under threat due to encroachment and replacement of these natural forests by drainage-based agriculture, commonly oil palm plantation. This study aims to quantify how the chemical and physical properties of peat change during land conversion to oil palm. This will be addressed by comparing four separate stages of conversion; namely, secondary peat swamp forests, recently deeply drained secondary forests, cleared and recently planted oil palm, and mature oil palm plantation in North Selangor, Malaysia. Results indicate accelerated peat decomposition in surface peats of mature oil palm plantations due to the lowered water table and altered litter inputs associated with this land-use change. Surface organic matter content and peat C stocks at secondary forest sites were higher than at mature oil palm sites (e.g. C stocks were 975 ± 151 and 497 ± 157 Mg ha− 1 at secondary forest and mature oil palm sites, respectively). Land conversion altered peat physical properties such as shear strength, bulk density and porosity, with mirrored changes above and below the water table. Our findings suggest close links between the organic matter and C content and peat physical properties through the entire depth of the peat profile. We have demonstrated that conversion from secondary peat swamp forest to mature oil palm plantation may seriously compromise C storage and, through its impact on peat physical properties, the water holding capacity in these peatlands.
机译:由热带泥炭沼泽森林提供的生态系统服务(例如碳(C)储存和水调节)受到威胁,这是由于以排水为基础的农业(通常是油棕种植)对这些天然森林的侵占和替代。这项研究旨在量化泥炭在土地转化为油棕期间的化学和物理特性如何变化。这将通过比较四个单独的转换阶段来解决。分别是马来西亚北部雪兰莪州的次生泥炭沼泽森林,近来严重枯竭的次生森林,已清理和近期种植的油棕以及成熟的油棕人工林。结果表明,由于地下水位降低和与此土地利用变化相关的垫料输入量的变化,成熟的油棕种植园表层泥炭加速了泥炭分解。次生林站点的地表有机质含量和泥炭C储量高于成熟油棕站点(例如,次生林和成熟油棕站点的C储量分别为975±151和497±157 Mg ha-1)。土地转化改变了泥炭的物理特性,例如抗剪强度,堆积密度和孔隙率,并且在地下水位的上方和下方都反映出变化。我们的发现表明,在整个泥炭剖面深度中,有机物与C含量和泥炭物理性质之间存在密切联系。我们已经证明,从次生泥炭沼泽森林到成熟的油棕人工林的转化可能会严重损害碳储量,并通过其对泥炭物理性质的影响,影响这些泥炭地的持水能力。

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