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首页> 外文期刊>Erdkunde >THE EFFECTS OF LAND USE CHANGE ON ATMOSPHERIC NUTRIENT DEPOSITION IN CENTRAL SULAWESI
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THE EFFECTS OF LAND USE CHANGE ON ATMOSPHERIC NUTRIENT DEPOSITION IN CENTRAL SULAWESI

机译:苏拉威西中部土地利用变化对大气营养素沉积的影响

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摘要

Deposition rates in remote areas due to anthropogenic emissions are increasing in Asian countries and elsewhere. The burning of biomass in slash-and-burn activities, in addition to burning fossil fuel result in higher rates of atmospheric deposition at forest and agricultural sites. An investigation of bulk depositions in Central Sulawesi was conducted at 13 field sites along a land use cover gradient that included natural and unused sites, slash-and-burn sites, and consolidated agricultural systemsaround and in the Lore Lindu National Park, an area of more than 2310 km~2. Bulk depositions rates were measured with passive ion exchange collectors. Our results show that Central Sulawesi generally experiences low deposition rates. Depositions that originate mainly from anthropogenic sources, such as nitrate, are very low, i.e. between 0.1 and 0.8 kg ha~(-1)a~(-1), but increase to 2.4 nitrate kg ha~(-1) a~(-1) near slash-and-burn areas. Similar patterns were found for elements such as potassium and calcium. Indeterminate depositions were found for geogenic elements such as iron, manganese and aluminium and in some cases phosphorus. A principal component analysis allowed differentiation between the contributions of different sources and different element to the total deposition impact in most cases. Specific deposition rates were recorded for different land use systems. The main factor that generated different deposition patterns was biomass burning resulting from slash-and-burn activities. The latter determined the composition of atmospheric depositions of nearby sites, but the more distant sites inside the national park do not appear to be influenced by these anthropogenic activities yet.
机译:在亚洲国家和其他地方,由于人为排放造成的偏远地区的沉积率正在上升。除燃烧化石燃料外,在砍伐和燃烧活动中燃烧生物质还导致森林和农业场所的大气沉积率更高。在苏拉威西中部沿土地利用覆盖梯度的13个田间地点进行了大块沉积物调查,包括自然和未使用的地点,砍伐和烧毁的地点以及合并的农业系统,以及在Lore Lindu国家公园附近。比2310 km〜2。用无源离子交换收集器测量本体沉积速率。我们的结果表明,苏拉威西中部地区沉积速率普遍较低。主要来自人为来源(例如硝酸盐)的沉积物非常低,即介于0.1和0.8 kg ha〜(-1)a〜(-1)之间,但增加到2.4硝酸盐kg ha〜(-1)a〜( -1)在刀耕火种的地区附近。对于钾和钙等元素也发现了类似的模式。已发现铁,锰和铝等地质元素的不确定沉积,某些情况下还发现了磷。主成分分析可以区分大多数情况下不同来源和不同元素对总沉积影响的贡献。记录了不同土地利用系统的特定沉积速率。产生不同沉积模式的主要因素是刀耕火种活动导致的生物质燃烧。后者决定了附近地点的大气沉积物组成,但国家公园内较远的地点似乎尚未受到这些人为活动的影响。

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