【24h】

Vegetation - soils relationships in a wetland area of the Orinoco delta plain (Venezuela)

机译:植被-奥里诺科三角洲平原(委内瑞拉)湿地地区的土壤关系

获取原文
获取原文并翻译 | 示例

摘要

The Orinoco Delta is one of the world's last great river deltas with pristine ecosystems. But it is also an important oil and gas reservoir area. Currently, little scientific and factual knowledge is available to assess the effect of oil exploitation activities. Understanding vegetation and soils relationships is fundamental to delineate conservation strategies to maintain species richness, essential ecological processes and life support systems. To meet these needs, our research objectives were to characterize soil conditions supporting different vegetation units of the Lower Orinoco Plain and to relate soil characteristics with vegetation assemblages. For these purposes, surface and bottom soil samples were taken in 227 sites, which were distributed proportionally to each vegetation unit coverage. Samples were analysed for salinity, chlorides, carbonates, pH, organic carbon, exchangeable acidity, aluminium, hydrogen, calcium, potassium and sodium. Average thickness of the surface organic layer was 2.32 m, reaching 6 m in some places. Organic carbon content did not differ significantly among soils from different vegetation units. Lowest surface pH values were found in forests and meadows (< 4.5). Bottom pH was less variable and almost neutral. The highest salinity values were found in mangrove soils (1.80per thousand ± 0.12), the lowest in palm forests (0.06per thousand ± 0.02). Main differences among soil samples were related with cation exchange capacity (68.3 meq/100g ± 81.5), percent base saturation (91.9% ± 11.0), and acidity (2.30 meq/100g ± 3.46). Our results indicated that content of salts and cations and soil acidification were the main factors in determining vegetation arrangements.
机译:奥里诺科三角洲是世界上最后一个拥有原始生态系统的伟大三角洲之一。但这也是重要的油气储集区。当前,很少有科学和事实知识可用来评估石油开采活动的效果。了解植被和土壤之间的关系对于描述保护策略以维持物种丰富性,必要的生态过程和生命支持系统至关重要。为了满足这些需求,我们的研究目标是表征支持下奥里诺科平原不同植被单元的土壤条件,并将土壤特征与植被组合联系起来。为此,在227个地点采集了表层和底层土壤样本,这些样本与每个植被单元的覆盖率成正比分布。分析样品的盐度,氯化物,碳酸盐,pH,有机碳,可交换酸度,铝,氢,钙,钾和钠。表面有机层的平均厚度为2.32 m,在某些地方达到6 m。不同植被单位的土壤中有机碳含量没有显着差异。在森林和草地中发现最低的表面pH值(<4.5)。底部pH值变化较小,几乎是中性的。在红树林土壤中发现最高的盐度值(每千1.80±0.12),在棕榈树林中发现最低的盐度(每千±0.06±0.02)。土壤样品之间的主要差异与阳离子交换容量(68.3 meq / 100g±81.5),碱基饱和百分比(91.9%±11.0)和酸度(2.30 meq / 100g±3.46)有关。我们的结果表明,盐和阳离子的含量以及土壤酸化是决定植被排列的主要因素。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号