...
首页> 外文期刊>Journal of Maps >Spatial distribution of sediment storage types in two glacier landsystems (Pasterze & Obersulzbachkees, Hohe Tauern, Austria)
【24h】

Spatial distribution of sediment storage types in two glacier landsystems (Pasterze & Obersulzbachkees, Hohe Tauern, Austria)

机译:两个冰川土地系统(Pasterze&Obersulzbachkees,奥地利陶恩山)的沉积物存储类型的空间分布

获取原文
   

获取外文期刊封面封底 >>

       

摘要

For the first time, geomorphological maps of the Obersulzbachkees (ca. 28?km~(2)) and the Pasterze (ca. 39.7?km~(2)) glacier landsystem at the catchment scale (1:10,000 and 1:12,500) are presented and the distribution of sediment storage types and (sub)recent sediment transfer processes are quantified and discussed. Special attention is drawn to the activity and function of sediment storages within the sediment cascade and on process (de)coupling of the sediment transfer systems. Glaciers cover ca. 50% of the landsystems and have retreated more than 1?km within the last six decades. The spatial distribution of sediment storage types delivers a record of the historical activity of the glaciers and the degree of sediment storage activity gives insights into the state of paraglacial landform adjustment. A typical landform assemblage is found in both landsystems. Moraine deposits are the dominant sediment storage type (coverage of ca. 3?km~(2) in both landsystems) and a significant source of (sub)recent sediment transfer. Deposits of reworked till account for ca. 4% of the total sediment coverage and paraglacial reworking is the main evolutionary factor for drift-mantled slopes with high activity in ice marginal and proximal locations (gully densities up to 3.7 per 100 metres of slope). With increasing distances from the glacier, the importance of paraglacial reworking decreases (gully density of 0.5 to 0.6). However, the contribution of paraglacial reworking to the overall sediment output is insignificant due to decoupling effects and till and debris are currently stored in both landsystems. The glacifluvial transport system is supply limited at the Obersulzbachkees and transport limited at the Pasterze. We consider the proglacial zone as a key control on sediment delivery from the glacier to the downstream fluvial system and hypothesize that the majority of sediment output from both landsystems is suspended load.
机译:流域规模(1:10,000和1:12,500)的Obersulzbachkees(约28?km〜(2))和Pasterze(约39.7?km〜(2))冰川土地系统的地貌图首次出现。介绍了沉积物的存储类型和(近)沉积物转移过程的分布,并进行了讨论。特别注意沉积物级联内的沉积物存储的活动和功能,以及沉积物传输系统的过程(去耦合)。冰川覆盖约在过去的十年中,有50%的土地系统已经退缩了1多公里。沉积物存储类型的空间分布提供了冰川历史活动的记录,而沉积物存储活动的程度则可以洞悉冰川期地貌调整的状态。在两个土地系统中都发现了典型的地貌组合。冰a沉积物是主要的沉积物存储类型(在两个土地系统中覆盖率约为3?km〜(2)),并且是(近)近期沉积物转移的重要来源。返工的存款占约在冰边缘和近端位置具有高活动性的漂移覆盖斜坡(总密度最高为每100米3.7的沟壑),其总沉积物覆盖率的4%是冰川覆盖的斜坡的主要演化因素。随着距冰川距离的增加,冰川下返工的重要性降低(河谷密度为0.5至0.6)。然而,由于解耦效应,冰川下返工对沉积物总产出的贡献微不足道,并且目前在这两个土地系统中都存储了耕作和碎片。冰川河水运输系统在Obersulzbachkees的供应有限,在Pasterze的运输受到限制。我们认为,冰河带是控制从冰川到下游河流系统的泥沙输送的关键控制,并假设这两个陆地系统的大部分泥沙输出都是悬浮负荷。

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