Effect of dry spells and soil cracking on runoff generation in a semiarid micro watershed under land use change

2016 ◽  
Vol 541 ◽  
pp. 1057-1066 ◽  
Author(s):  
Julio Cesar Neves dos Santos ◽  
Eunice Maia de Andrade ◽  
Maria João Simas Guerreiro ◽  
Pedro Henrique Augusto Medeiros ◽  
Helba Araújo de Queiroz Palácio ◽  
...  
2009 ◽  
Vol 208 (1-2) ◽  
pp. 121-128 ◽  
Author(s):  
Ying Chen ◽  
Youpeng Xu ◽  
Yixing Yin

2013 ◽  
Vol 18 (11) ◽  
pp. 1464-1470 ◽  
Author(s):  
Qiongfang Li ◽  
Tao Cai ◽  
Meixiu Yu ◽  
Guobin Lu ◽  
Wei Xie ◽  
...  

GeoScape ◽  
2021 ◽  
Vol 15 (1) ◽  
pp. 19-29
Author(s):  
Monoj Kumar Jaiswal ◽  
Nurul Amin

Abstract Alteration of land-use land cover pattern causes severe consequences on the hydrological system by modifying the rainfall-runoff pattern in a region. The study aimed to investigate the impact of land-use land-cover dynamics on runoff generation in different geomorphic divisions of Panchnoi River basin. The study used the Soil Conservation Service-Curve Number method to estimate runoff generation in the Panchnoi River basin in a GIS platform. This study observed that the conversion of the land-use pattern in the geomorphic zones significantly enhances runoff. The Piedmont experience highest land-use change, where 64.17 km2 forest cover lost to cropland and built-up lands, leads to a notable increase in runoff generation, i.e. from 1 076 mm (52.82% of rainfall) in 1990 to 1 467 mm (70.46% of rainfall) in 2015. The Flood plain and New alluvial plain generates high runoff in the basin as it mostly occupied by human-induced land-uses, i.e. 1 444 mm (72.72% of rainfall) and 1 360 mm (71.70% of rainfall) respectively in 1990, which increase to 1588 mm (79.20%) and 1507 mm (78.69%) runoff respectively in 2015, due to alteration of cropland to built-up lands. In the Old alluvial plain, a marginal land-use change observed resulted in moderate growth in runoff from 1 272 mm (62.35%) to 1 404 mm (66.79%). The study indicates land-use land-cover change invokes to increase runoff generation can give rise severe environmental and economic problems in the river basin, through the occurrence of flashflood and soil erosion. Highlights for public administration, management and planning: • Evaluation of the impact of land-use land cover dynamics on runoff is essential for containing flash flood and water resource management on a basin scale. • Alteration of natural land covers has severe implications in the form of flood, soil erosion, and loss of biodiversity. • Enhanced runoff due to land-use dynamics reduces groundwater recharge rate that may cause drinking water scarcity in the dry season shortly.


CATENA ◽  
2015 ◽  
Vol 135 ◽  
pp. 263-270 ◽  
Author(s):  
Nur Algeet-Abarquero ◽  
Miguel Marchamalo ◽  
Javier Bonatti ◽  
Jesús Fernández-Moya ◽  
Roger Moussa

2014 ◽  
Vol 71 (2) ◽  
pp. 289-295 ◽  
Author(s):  
Leihua Dong ◽  
Lihua Xiong ◽  
Upmanu Lall ◽  
Jiwu Wang

The principles and degrees to which land use change and climate change affect direct runoff generation are distinctive. In this paper, based on the MODIS data of land use in 1992 and 2003, the impacts of land use and climate change are explored using the Soil Conservation Service Curve Number (SCS-CN) method under two defined scenarios. In the first scenario, the precipitation is assumed to be constant, and thus the consequence of land use change could be evaluated. In the second scenario, the condition of land use is assumed to be constant, so the influence only induced by climate change could be assessed. Combining the conclusions of two scenarios, the effects of land use and climate change on direct runoff volume can be separated. At last, it is concluded: for the study basin, the land use types which have the greatest effect on direct runoff generation are agricultural land and water body. For the big sub basins, the effect of land use change is generally larger than that of climate change; for middle and small sub basins, most of them suffer more from land use change than from climate change.


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