...
首页> 外文期刊>Lakes & Reservoirs >Spatial variations in sedimentary organic matter in surficial lake sediments of Nyanza Gulf (Lake Victoria, Kenya) after invasion of water hyacinth
【24h】

Spatial variations in sedimentary organic matter in surficial lake sediments of Nyanza Gulf (Lake Victoria, Kenya) after invasion of water hyacinth

机译:风信子入侵后,Nyanza湾(肯尼亚维多利亚湖)表层湖泊沉积物中沉积有机质的空间变化

获取原文
获取原文并翻译 | 示例

摘要

No detailed studies have been conducted on the spatial distribution of sediment characteristics within Nyanza Gulf of Lake Victoria, especially after the invasion of water hyacinth. Accordingly, a rapid, inexpensive method was used to determine the spatial sediment organic matter variations, expressed as loss on ignition (LOI). Surficial sediments were collected during different survey periods from about thirty-two sampling sites between 1994 and 2012, in order to characterize the sediments. Although the deeper (>40m) depositional areas are located in the open lake, visual observations indicate that most of the offshore sediments consist of muddy deposits, plus significant shell remains, with a more sandy type of sediments located in some areas off the inflowing river mouths. The surficial sediments were characterized by a relatively high water content, with over 89% of the samples containing water contents greater than 75%. The sediment organic matter contents from the 2012 survey were more variable, ranging from 1.90% to 33.47%. The sediment organic carbon contents varied spatially, although there were no significant variations between the different sampling periods. Evaluating the SOM at different heating durations at a constant temperature (550°C) and a very high temperatures (950°C) did not identify any significant differences. High primary production and greater settling in the deeper areas contribute to the nature of sediments deposited, also being reflected in the relatively high OC contents. Spatially, it is thought that detritus from water hyacinth and terrestrial external loads are important sources of organic matter deposited on the lake bottom within the gulf and may support its growth because of enrichment of nutrient elements. The importance of sediments in adsorption of contaminant substances and influencing geochemical processes within the lake is also emphasized.
机译:尚未对维多利亚湖Nyanza海湾内的沉积物特征的空间分布进行详细研究,尤其是在风信子入侵之后。因此,使用一种快速,廉价的方法来确定空间沉积物有机物的变化,表示为灼烧损失(LOI)。为了表征沉积物,在1994年至2012年的不同调查期间,从大约32个采样点收集了表面沉积物。尽管更深的沉积区域(> 40m)位于开阔的湖泊中,但肉眼观察表明,大多数近海沉积物由泥泞的沉积物组成,外加大量的贝壳残留物,在入流河外的某些区域则有更多的沙质沉积物。嘴巴表层沉积物的特征是含水量相对较高,超过89%的样品含水量大于75%。 2012年调查的沉积物有机质含量变化更大,范围从1.90%到33.47%。沉积物有机碳含量在空间上变化,尽管在不同采样周期之间没有显着变化。在恒定温度(550°C)和非常高的温度(950°C)下,在不同的加热持续时间下评估SOM并未发现任何显着差异。较高的初级产量和在更深区域的更大沉降量有助于沉积物的沉积,这也反映在较高的OC含量中。在空间上,人们认为水葫芦碎屑和地面外部负荷是沉积在海湾内湖底的有机物的重要来源,并且由于营养元素的富集而可能支持其生长。还强调了沉积物在吸附污染物和影响湖泊内地球化学过程中的重要性。

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