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Degradation of soil nutrients and slow recovery of biomass following shifting cultivation in the heath forests of Sarawak, Malaysia

机译:马来西亚沙捞越森林栽培之后,土壤养分降解土壤养分及生物质缓慢恢复

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摘要

Heath forests which are tropical forests on sandy soils are widely distributed in Borneo and provide many ecosystem services, such as carbon storage and non-timber forest products. Over the past several decades, such forests have been disturbed by non-traditional shifting cultivation, which is usually conducted in unsuitable land with short fallow duration. Anthropogenic disturbances in forests growing on sandy soils that have low nutrient retention capacities may promote further reductions in soil fertility. Long-term monitoring of soil nutrients and biomass accumulation is rare in degraded tropical rainforests growing on sandy soils despite the known negative effects of non-traditional shifting cultivation practices on soil fertility, vegetation and biomass recovery, and the growth of trees planted to rehabilitate forests. The objective of the current study was therefore to elucidate changes in soil fertility and biomass recovery potential in degraded forests on sandy soils in Borneo. We monitored soil nutrients and chemical properties in fifty-four 12 x 12 m plots located on different topographical positions along upper and lower slopes. Samples were collected in plots aged 7 and 14 years after abandonment of shifting cultivation. The biomass of secondary forest trees in all plots 12 years after the abandonment was also measured to determine the relationship between biomass accumulation and changes in soil nutrients. We found that soil pH and cation exchange capacity, and the concentrations of most nutrients, including nitrogen, magnesium, and phosphorus, had decreased significantly 7-14 years after abandonment; biomass accumulation in the plots was also limited 12 years after abandonment ( & 0.8 Mg ha(-1) year(-1)). These changes in soil traits within the study plots were similar regardless of topographical position, and the changes were not related to the amount of biomass. Soil nutrients in the plots may have leached out as a result of removal of thick root mats in the surface soil, high sand content, and large amounts of rainfall in the area rather than uptake by recovering trees. These results indicate that it may be difficult to recover soil fertility on steep slopes in sandy soil conditions because of high leaching rates and erosion when the soil surface layer is destroyed by shifting cultivation. It is therefore important to carefully manage shifting cultivation practices in tropical forests on sandy soils in Borneo.
机译:在婆罗洲的沙质土壤中是热带森林的荒地森林广泛分布,并提供许多生态系统服务,如碳储存和非木材林产品。在过去的几十年中,这种森林受到非传统转移栽培的干扰,通常在不合适的土地上进行,休眠短。生长在具有低营养保留能力的沙质土壤中的人为干扰可能促进土壤肥力的进一步减少。尽管非传统转移培养实践对土壤肥力,植被和生物量回收的已知负面影响,但在沙质土壤中生长的热带雨林的长期监测是罕见的,但在砂土上生长的热带热带雨林中罕见的是罕见的。植被和生物量回收,树木的生长恢复森林。因此,目前研究的目的是为了阐明婆罗洲沙子土壤中降解森林中土壤肥力和生物质恢复潜力的变化。我们在沿着上下斜坡和下斜坡上监测54个12×12M地位的土壤营养素和化学性质。在放弃移位栽培后7岁和14岁的地块中收集样品。还测量了12年后的所有情节中的次生林树木的生物量,以确定生物质积累与土壤营养素变化之间的关系。我们发现土壤pH和阳离子交换能力,以及大多数营养素(包括氮,镁和磷)的浓度在放弃后7-14岁以下降低了7-14岁;在遗弃后12年(& 0.8 mg ha(-1)年(-1)年(-1)),地块的生物质积累也有限。无论地形位置如何,研究图中的土壤特性的这些变化都是相似的,并且变化与生物质量无关。地块中的土壤营养物可能会在地面土壤,高砂含量和地区的大量降雨中除去厚根垫而不是通过恢复树木。这些结果表明,由于在通过移位栽培破坏土壤表面层时,可能难以恢复含沙土条件下的陡坡土壤肥力。因此,重要的是要仔细管理婆罗洲沙子土壤的热带森林中的转移栽培实践。

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