Luminescence chronology of late Holocene extreme hydrological events in the upper Penner River basin, South India

2007 ◽  
Vol 22 (8) ◽  
pp. 747-753 ◽  
Author(s):  
Puthusserry J. Thomas ◽  
Navin Juyal ◽  
Vishwas S. Kale ◽  
Ashok K. Singhvi
Author(s):  
Upasana S. Banerji ◽  
Jithu Shaji ◽  
P. Arulbalaji ◽  
K. Maya ◽  
S. Vishnu Mohan ◽  
...  

2010 ◽  
Vol 177 (2) ◽  
pp. 160-170 ◽  
Author(s):  
JEAN-PHILIPPE VENOT ◽  
LUNA BHARATI ◽  
MARK GIORDANO ◽  
FRANÇOIS MOLLE

2003 ◽  
Vol 48 (7) ◽  
pp. 57-63 ◽  
Author(s):  
M.C. Sekhar ◽  
Ch. Indira

Chloride discharge relationships at several monitoring stations on the River Krishna in South India are investigated, both qualitatively and quantitatively, to identify probable source contributions. The chloride behaviour along the waterway is studied in detail to assess the source contributions at various monitoring stations falling within the study area. Seasonal variations in the intensity of rainfall cause wide variations in the quality of the River Krishna. As there is strong seasonal dependence between the flow in the river and chlorides, seasonal models are developed for prediction of concentrations and loads. Linear regression analysis is carried out to determine the model parameters. The predicted concentrations and loads are in agreement with the observed values within the uncertainty of data. As the area is characterized by distinct dry and wet seasons (based on rainfall distribution over the year), mass balances are used to differentiate between point and non-point source contributions to the river. In large river basins, monitoring all individual sources is difficult and/or impossible and expensive; hence the presented approach based on receiving water quality and flow serves as an alternative for modeling chlorides in the river basin. Results of the study can be used to emphasise water pollution control strategies.


Antiquity ◽  
2008 ◽  
Vol 82 (317) ◽  
pp. 560-570 ◽  
Author(s):  
César A. Méndez M. ◽  
Omar R. Reyes B.

How early did steppe dwellers penetrate the forests? The authors compare and contrast settlement on the steppe, in the forest and on the steep sea coast of western Patagonia, finding that the steppe is occupied first, from 11400 calendar years BP. But around 2800 calendar years BP settlements enter the forest almost simultaneously for a brief period along the length of the Cisnes river valley. Within a few centuries the experiment appears to be abandoned, and the focus of prehistoric peoples returns to the steppe.


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