首页> 外文期刊>Water Research >Long-term changes in water physicochemistry in the Adour-Garonne hydrographic network during the last three decades
【24h】

Long-term changes in water physicochemistry in the Adour-Garonne hydrographic network during the last three decades

机译:最近三十年来Adour-Garonne水文网络中水物理化学的长期变化

获取原文
获取原文并翻译 | 示例
       

摘要

This study details a trend analysis covering a 30-year period (1975-2004), for 19 physicochemical parameters at 45 surface water sites in the Adour-Garonne basin, south-west France. To perform statistical analysis, we used the annual average of each variable. The analysis revealed sites affected by strong patterns of temporal variation and sites with weak or imperceptible changes of water quality. More than half the studied sites were affected by chemical changes. Trends were generally clearest in the River Garonne continuum, but similar tendencies could also be identified in tributaries. The overall trends indicated the onset of an increase of water temperature starting about 20 years ago and partial recovery from eutrophication during the last decade. As expected, the strongest trend affected the temperature regime of the hydrosystems, there being a more significant warming during the second decade of the study (1984-1994). Additionally, at many sites nutrient loads were lower between 1995 and 2004. This confirms a downward trend in eutrophication status resulting from more stringent control of sewage treatment despite the constant increase of anthropic pressure. Sites that did not present any trends are extreme sites located at each end of the river gradient: headwater and downstream sites under tidal influence. Other sites not affected by changes are those strongly perturbed by human activities showing a high level of degradation.
机译:这项研究详细研究了趋势分析,涵盖了法国西南部Adour-Garonne盆地45个地表水站点上19个物理化学参数的30年周期(1975-2004年)。为了进行统计分析,我们使用了每个变量的年度平均值。分析表明,受时间变化强烈模式影响的站点和水质变化较弱或无法察觉的站点。超过一半的研究地点受到化学变化的影响。在加龙河连续体中,趋势通常最明显,但是在支流中也可以发现类似的趋势。总体趋势表明,大约20年前开始出现水温升高,并在过去十年中从富营养化中部分恢复。不出所料,最强烈的趋势影响了水文系统的温度状况,在研究的第二个十年(1984-1994年)中,变暖现象更为明显。此外,在1995年至2004年期间,许多地方的养分含量较低。这证实了富营养化状态的下降趋势是由于尽管人类压力不断增加,但对污水处理的控制更为严格。没有任何趋势的站点是位于河坡两端的极端站点:源头和受潮汐影响的下游站点。其他不受变化影响的地点是那些受到人类活动强烈干扰的地点,其退化程度很高。

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