Use of Sr isotopes as a tool to decipher the soil weathering processes in a tropical river catchment, southwestern India

2015 ◽  
Vol 63 ◽  
pp. 498-506 ◽  
Author(s):  
G.P. Gurumurthy ◽  
K. Balakrishna ◽  
M. Tripti ◽  
Jean Riotte ◽  
Stéphane Audry ◽  
...  
Author(s):  
Baby Krishnan Nisha ◽  
Keshava Balakrishna ◽  
Harikripa Narayana Udayashankar ◽  
Busnur Rachotappa Manjunatha

AbstractStudies done on small tropical west-flowing river catchments located in the Western Ghats in southwestern India have suggested very intense chemical weathering rates and associated CO2 consumption. Very less studies are reported from these catchments notwithstanding their importance as potential sinks of atmospheric CO2 at the global scale. A total of 156 samples were collected from a small river catchment in the southwestern India, the Payaswini–Chandragiri river Basin, during pre-monsoon, monsoon and post-monsoon seasons in 2016 and 2017, respectively. This river system comprises two small rivers originating at an elevation of 1350 m in the Western Ghats in peninsular India. The catchment area is dominated by biotite sillimanite gneiss. Sodium is the dominant cation, contributing ~ 50% of the total cations, whereas HCO3− contributes ~ 75% of total anions. The average anion concentration in the samples varied in the range HCO3− > Cl− > SO42− > NO3− > F−, whereas major cation concentration varied in the range Na+  > Ca2+  > Mg2+  > K+. The average silicate weathering rate (SWR) was 42 t km−2 y−1 in the year 2016 and 36 t km−2 y−1 in 2017. The average annual carbon dioxide consumption rate (CCR) due to silicate rock weathering was 9.6 × 105 mol km−2y−1 and 8.3 × 105 mol km−2 y−1 for 2016 and 2017, respectively. The CCR in the study area is higher than other large tropical river catchments like Amazon, Congo-Zaire, Orinoco, Parana and Indus because of its unique topography, hot and humid climate and intense rainfall.


Geomorphology ◽  
2020 ◽  
Vol 371 ◽  
pp. 107433
Author(s):  
Markus Egli ◽  
Dennis Dahms ◽  
Mike Dumitrescu ◽  
Farzaneh Derakhshan-Babaei ◽  
Marcus Christl ◽  
...  

CATENA ◽  
2001 ◽  
Vol 43 (1) ◽  
pp. 49-62 ◽  
Author(s):  
Jason A. Rech ◽  
Richard W. Reeves ◽  
David M. Hendricks

2014 ◽  
Vol 73 (1) ◽  
pp. 333-346 ◽  
Author(s):  
G. P. Gurumurthy ◽  
K. Balakrishna ◽  
M. Tripti ◽  
Jean Riotte ◽  
Stéphane Audry ◽  
...  

2012 ◽  
Vol 440 ◽  
pp. 178-185 ◽  
Author(s):  
Louise Camenzuli ◽  
Martin Scheringer ◽  
Caroline Gaus ◽  
Carla A. Ng ◽  
Konrad Hungerbühler

2012 ◽  
Vol 20 (6) ◽  
pp. 4067-4077 ◽  
Author(s):  
M Tripti ◽  
G P Gurumurthy ◽  
K Balakrishna ◽  
M D Chadaga

2021 ◽  
Vol 11 (1) ◽  
Author(s):  
R. L. Mitchell ◽  
P. Davies ◽  
P. Kenrick ◽  
T. Volkenandt ◽  
C. Pleydell-Pearce ◽  
...  

AbstractCorrelative imaging provides a method of investigating complex systems by combining analytical (chemistry) and imaging (tomography) information across dimensions (2D-3D) and scales (centimetres-nanometres). We studied weathering processes in a modern cryptogamic ground cover from Iceland, containing early colonizing, and evolutionary ancient, communities of mosses, lichens, fungi, and bacteria. Targeted multi-scale X-ray Microscopy of a grain in-situ within a soil core revealed networks of surficial and internal features (tunnels) originating from organic-rich surface holes. Further targeted 2D grain characterisation by optical microscopy (OM), scanning electron microscopy (SEM), and energy dispersive X-ray spectroscopy (SEM–EDS), following an intermediate manual correlative preparation step, revealed Fe-rich nodules within the tunnels. Finally, nanotomographic imaging by focussed ion beam microscopy (FIB-SEM) revealed coccoid and filamentous-like structures within subsurface tunnels, as well as accumulations of Fe and S in grain surface crusts, which may represent a biological rock varnish/glaze. We attribute these features to biological processes. This work highlights the advantages and novelty of the correlative imaging approach, across scales, dimensions, and modes, to investigate biological weathering processes. Further, we demonstrate correlative microscopy as a means of identifying fingerprints of biological communities, which could be used in the geologic rock record and on extra-terrestrial bodies.


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