...
首页> 外文期刊>Geomorphology >Changes in the channel-bed level of the eastern Carpathian rivers: Climatic vs. human control over the last 50 years
【24h】

Changes in the channel-bed level of the eastern Carpathian rivers: Climatic vs. human control over the last 50 years

机译:喀尔巴阡山脉东部河流河床水位的变化:过去50年的气候与人类控制

获取原文
获取原文并翻译 | 示例

摘要

This paper is focused on the changes over the past 50 years in the channel beds of seven major rivers that are part of the Siret drainage basin located in eastern Romania. Each river has been subjected to various degrees of human intervention, assessed based on the morphological quality index (MQI): two rivers (Siret and Bistrita) have undergone complex human interventions on 40 and 60%, respectively, of their channel lengths, two rivers (Suceava and Moldova) are 30% artificial, and the remaining three rivers (Trotus, Putna, and Buzau) have a good or moderate MQI. The changes occurring in channel beds and data on water discharge (Q_w) and sediment load (Q_s were assessed simultaneously for the last 50 years. The bedload was indirectly evaluated as ranging between 5 and 15% of the total sediment load. It was determined that incision was prevalent among the processes acting on the channel-bed sections under investigation (representing 62% of the altered area and changing bed level by between —0.25 and —2.70 m), with aggradation accounting for the remaining 38% (causing changes ranging from +0.15 to +1.25 m). The magnitude of the processes (incision or aggradation) for sections with an MQI < 0.3 was four times higher than for sections with a moderate or good MQI (>0.3). The pattern of change in the channel-bed processes between 1960 and 2010 for all river categories was as follows: a low rate of incision from 1960 to 1979, followed by a higher rate of incision from 1980 to 1989, and finally a tendency of recovery toward the river's initial state, characterised by a decrease in the incision rate or slight aggradation after 1990. The variable that exhibited the strongest response to climate conditions was water discharge (Q_w), whereas the sediment load (Q_s) was highly responsive to both climatic signals and anthropogenic factors. The sediment load has been instrumental in the adjustments of the channel beds by maintaining a balance between the two controlling factors, nature and man.
机译:本文着眼于过去50年中罗马尼亚东部Siret流域一部分的7条主要河流的河床变化。根据形态质量指数(MQI)评估,每条河流都受到了不同程度的人工干预:两条河流(Siret和Bistrita)分别对其河道长度的40%和60%进行了复杂的人工干预,两条河流(苏恰瓦河和摩尔多瓦)有30%是人工河道,其余三河(特罗托斯河,普特纳河和布扎河)的MQI都中等或中等。在过去的50年中,同时评估了河床的变化以及排水量(Q_w)和沉积物负荷(Q_s)的数据,间接评估了床体负荷在总沉积物负荷的5%至15%之间。在研究中作用于河床床段的过程中,切口普遍存在(占改变面积的62%,床层高度在-0.25至-2.70 m之间变化),其余38%由凝结作用(造成的变化范围为+0.15至+1.25 m)。MQI <0.3的断面的幅度(切开或凝结)是MQI中等或良好(> 0.3)的断面的四倍。 1960年至2010年之间所有河流类别的河床过程如下:1960年至1979年的切口率较低,其后1980年至1989年的切口率较高,最终有恢复到河流初始状态的趋势c 1990年以后,切口率降低或略微积水使人遭受伤害。对气候条件表现出最强响应的变量是排水量(Q_w),而泥沙负荷(Q_s)对气候信号和人为因素均具有高度响应性。通过保持自然和人为两个控制因素之间的平衡,沉积物负荷在调整河床中起到了重要作用。

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