I am a geochemist, primarily interested in low-temperature geochemical processes to understand better the past evolution of climate/hydrology/vegetation and their interactions. Recently, I graduated from the Earth and Climate Science Department of the Indian Institute of Science Education and Research (IISER) Pune. My Ph.D. research focused on the impact of climate on land surface processes at different time scales, ranging from seasonal to kilo-year. I frequently use geochemical and isotopic signatures of marine and terrestrial sediments and river water samples to answer some of these questions.
Currently, I am working as a postdoctoral researcher at the IBS Center for Climate Physics (ICCP). Here, I am focusing on two major aspects: (i) local hydrological dynamics, mainly the infiltration process at the karst system, and (ii) long-term atmospheric circulation, that is the dust supply, using trace-elemental and isotopic compositions of speleothem samples collected from different parts of the world. I am also involved in a cave system monitoring program to understand how the karstic zone influences speleothem chemical compositions. To address my research objective, I established an analytical protocol of one laser ablation (193 nm ArF Excimer) system coupled with a mass spectrometer (LA-ICP-MS) at ICCP for analyzing speleothem trace elemental compositions.
I have a great interest in understanding climate-erosion linkage, as well as paleoceanographic processes and depositional environment (redox state) using sediment geochemistry. (read more)
Appointments
Postdoctoral Fellow | IBS Center for Climate Physics | 2023 - Present
Research Associate | CCCR, IITM Pune | 2022 - 2023
Mining Geologist | Hindustan Zinc Limited | 2015 - 2016
Contact
IBS Center for Climate Physics
Pusan National University
Busan, 46241, Republic of Korea
Education
Ph.D. | Geochemistry | Indian Institute of Science Education and Research, Pune
Advisor: Prof. Gyana Ranjan Tripathy
M.Sc. | Applied Geology | Jadavpur University, Kolkata
B.Sc. | Geological Sciences | Jadavpur University, Kolkata
Geochemical investigation of a sediment core, (age: 0.8 - 7.2 kyr BP) from the eastern Arabian Sea, was carried out to reconstruct erosional changes across the Meghalayan stage boundary (∼4.2 kyr BP).
Key findings
Provenance and chemical weathering show the minimal change between 7.2 and 2.6 kyr BP.
Changes in weathering patterns were observed during the Roman Warm Period.
A transition from oxic to reduced bottom water condition was observed since ∼4.2 kyr BP.
Surface water chemistry (major ions and silica concentrations) of two mining-influenced rivers (Damodar and Subarnarekha) from India has been investigated to estimate their sulfide oxidation fluxes and to assess their impact on the long-term carbon cycle.
Key findings
Elevated dissolved sulfate concentrations are observed in mining-dominated regions.
Oxidation of sulfides supplies one-third of SO4 in the coal-rich, upper Damodar basin.
CO2 consumption rate in these tropical rivers is 2-3 times higher than the global average value.
Our research and lab
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