Human induced soil erosion and the implications on crop yield in a small mountainous Mediterranean catchment (SW-Turkey)

被引:20
|
作者
Van Loo, Maarten [1 ]
Dusar, Bert [1 ,2 ]
Verstraeten, Gert [1 ,2 ]
Renssen, Hans [3 ]
Notebaert, Bastiaan [1 ]
D'Haen, Koen [1 ]
Bakker, Johan [1 ,2 ]
机构
[1] Katholieke Univ Leuven, Dept Earth & Environm Sci, Div Geog & Tourism, Celestijnenlaan 200E,Box 2409, B-3001 Leuven, Belgium
[2] Katholieke Univ Leuven, Ctr Archaeol Sci, Celestijnenlaan 200E,Box 2409, B-3001 Leuven, Belgium
[3] Vrije Univ Amsterdam, Fac Earth & Life Sci, Dept Earth Sci, NL-1081 HV Amsterdam, Netherlands
关键词
Geomorphic modeling; Soil depletion; Crop yield; Human impact; Land use change; Climate; HOLOCENE ENVIRONMENTAL-CHANGE; LAND-USE; SEDIMENT YIELD; SPATIAL-PATTERNS; COMBINING FIELD; HUMAN IMPACT; LANDSCAPE; HISTORY; CLIMATE; WATER;
D O I
10.1016/j.catena.2016.08.023
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Many hillslopes in the limestone dominated Taurus Mountain Range (SW Turkey) are characterized by severely depleted soils, while a significant amount of sediment is being stored in the valley bottoms. The same holds true for the 11.4 km(2) endorheic Gravgaz basin in the vicinity of the Hellenistic-Roman city of Sagalassos in SW Turkey. Previous palaeo-environmental research in this basin already yielded both detailed sedimentological and palynological information on sedimentation in the valley bottom and vegetation changes that took place during the last several millennia. An adapted WATEM/SEDEM geomorphic model version was used to simulate the impact of the observed changes in vegetation cover, climate and hillslope soil properties on hillslope soil erosion and valley bottom sediment deposition over the last 4000 years. The calibrated WATEM/SEDEM model is able to reconstruct the temporal changes of sedimentation in the valley bottom reasonably well. To simulate the impact of historic soil erosion on crop productivity a simple crop yield model was coupled to the reconstructed soil thickness maps. The main outcomes are that soil erosion was mainly driven by deforestation and hence anthropogenic activity, but the resulting soil erosion did not cause a complete collapse of crop yields. On the contrary, we were able to quantify that the sediment accumulation in the lower lying valley bottoms compensated at least a part of the loss in crop yield from the hillslopes: potential crop yield value changed from 2.80 t ha(-1) a(-1) before widespread deforestation to 258 t ha(-1) a(-1) during Roman-Imperial times and 2.19 t ha(-1) a(-1) at present. These model approaches are tools that allow us to quantify human impact in the past, going beyond traditional qualitative descriptions, which will ultimately lead to a better understanding of human-environment interactions in the past (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:493 / 506
页数:14
相关论文
共 19 条