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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Impact of natural reforestation on floodplain sedimentation in the Dragonja basin, SW Slovenia
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Impact of natural reforestation on floodplain sedimentation in the Dragonja basin, SW Slovenia

机译:斯洛文尼亚西南部Dragonja盆地的天然造林对洪泛区沉积的影响

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Changes in floodplain sediment dynamics have profound effects on riverine habitats and riparian biodiversity. Depopulation due to socio-economic changes in the Dragonja catchment (91 km(2)) in southwestern Slovenia resulted in the abandonment of agricultural fields, followed by natural reforestation since 1945. This profoundly changed the water and sediment supply to the streams, as well as floodplain sediment deposition. This paper presents a reconstruction of the development of the Dragonja floodplain due to these land use changes during the last 60 years. The reconstruction is based on dating of floodplain sediments using Cs-137 profiles, measurement of actual sedimentation rates using artificial grass sedimentation mats, and linking this information to the present-day hydrological behaviour of the river. The sedimentation mats showed that floodplain sedimentation was restricted to peak flows of considerable magnitude. Due to the reforestation, the return period of such high flows increased from 0.31 year in the period 1960-1985 to 0.81 year between 1986 and 2003, with commensurate changes in sedimentation rates. At the 1.5 m river terrace (formed about 60 years ago), Cs-137-based sedimentation rates (1960-1986) were roughly twice the rates inferred from the artificial grass mats (2001-2003). This finding matches the increase in the return period for larger peak events during the 1986-2003 period, which caused fewer major inundations at this level. Conversely, sedimentation rates determined for the lowest terrace at 0.5 m were similar for both techniques (and periods) because the return periods of the peak events responsible for sediment deposition at this lower level did not change much over the period 1986-2003. Copyright (c) 2006 John Wiley & Sons Ltd.
机译:洪泛区沉积物动力学变化对河流生境和河岸生物多样性具有深远的影响。斯洛文尼亚西南部Dragonja集水区(91 km(2))的社会经济变化导致人口减少,导致放弃了农田,随后自1945年以来进行了自然造林。这也深刻改变了溪流的水和沉积物供应作为洪泛区沉积物的沉积。本文介绍了由于过去60年中这些土地用途的变化而对Dragonja洪泛区的发展的重建。重建的基础是使用Cs-137剖面对洪泛区沉积物进行测年,使用人造草皮沉积垫测量实际沉积速率,并将此信息与河流的当前水文行为联系起来。沉积垫表明,洪泛区的沉积仅限于相当大的峰值流量。由于重新造林,如此高流量的返回期从1960-1985年的0.31年增加到1986年至2003年的0.81年,而沉积率也有相应的变化。在约60年前形成的1.5 m河阶地上,基于Cs-137的沉积速率(1960-1986年)大约是从人工草垫(2001-2003年)推断的速率的两倍。这一发现与1986年至2003年期间更大的高峰事件的返还期增加相吻合,在此水平上造成的主要淹没事件减少了。相反,对于两种技术(和时段)而言,在0.5 m处的最低阶地确定的沉积速率是相似的,因为在1986-2003年期间,在该较低水平上造成沉积物沉降的峰值事件的返回周期没有太大变化。版权所有(c)2006 John Wiley&Sons Ltd.

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