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Atindra Sapkota

Biographic Data

ID6570920
NAMEAtindra Sapkota
GIVEN NAMESAtindra
FAMILY NAMESapkota
SIGNATURESAPKOTA A
AFFILIATIONSState Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, China
VERIFIEDNo
TOTAL WORKS3
TOTAL CITATIONS2
WORKS AS AUTHOR3
WORKS AS EDITOR0
FIRST PUBLICATION YEAR2007
LATEST PUBLICATION YEAR2019
H-INDEX1
  • Kyr of atmospheric mineral dust deposition in north-eastern China

    Open Access•Steve Pratte, Kunshan Bao et al.•ARTICLE•The Holocene•2019•Cited by: 1•References: 15

    A multi-proxy record of Holocene and late-Pleistocene aeolian mineral dust is reconstructed using a combination of geochemical (trace elements), mineralogical and grain-size analyses on cores from the Hani peatland in north-eastern (NE) China. The dust record displays a sharp increase in dust deposition during the late Holocene in comparison to the rest of the Holocene. This trend is in line with climatic records from the Chinese dust source regi…

  • Energy, Forest, and Indoor Air Pollution Models for Sagarmatha National Park and Buffer Zone, Nepal

    Open Access•Franco Salerno, Gaetano Viviano et al.•ARTICLE•Mountain Research and Development•2010

    This paper presents the results of management-oriented research on energy, forest, and human health issues in a remote mountain area, the Sagarmatha National Park and Buffer Zone (SNPBZ), Nepal. The research was based on a broader, integrated participatory framework ultimately intended for use in adaptive management. The present study focused on the application of a participatory modeling framework to address problems related to energy demand and…

  • Six millennia of atmospheric dust deposition in southern South America (Isla Navarino, Chile)

    Open Access•Atindra Sapkota, Andriy K Cheburkin et al.•ARTICLE•The Holocene•2007•Cited by: 1•References: 4

    To characterize dust deposition in southern South America for the Holocene, a 542 cm long core from a peat bog in southern Chile (Oreste bog, Isla Navarino) was studied. Peat formation started ~11 160 14 C yr before present (BP). The titanium (Ti) concentration in bulk peat, combined with dry bulk density, and peat accumulation rate, were used to calculate the mineral accumulation rate (MAR) in the Oreste bog. The distribution of calcium (Ca), ma…

  • Kyr of atmospheric mineral dust deposition in north-eastern China

    Open Access•Steve Pratte, Kunshan Bao et al.•ARTICLE•The Holocene•2019•Cited by: 1•References: 15

    A multi-proxy record of Holocene and late-Pleistocene aeolian mineral dust is reconstructed using a combination of geochemical (trace elements), mineralogical and grain-size analyses on cores from the Hani peatland in north-eastern (NE) China. The dust record displays a sharp increase in dust deposition during the late Holocene in comparison to the rest of the Holocene. This trend is in line with climatic records from the Chinese dust source regi…

  • Six millennia of atmospheric dust deposition in southern South America (Isla Navarino, Chile)

    Open Access•Atindra Sapkota, Andriy K Cheburkin et al.•ARTICLE•The Holocene•2007•Cited by: 1•References: 4

    To characterize dust deposition in southern South America for the Holocene, a 542 cm long core from a peat bog in southern Chile (Oreste bog, Isla Navarino) was studied. Peat formation started ~11 160 14 C yr before present (BP). The titanium (Ti) concentration in bulk peat, combined with dry bulk density, and peat accumulation rate, were used to calculate the mineral accumulation rate (MAR) in the Oreste bog. The distribution of calcium (Ca), ma…

  • Six millennia of atmospheric dust deposition in southern South America (Isla Navarino, Chile)

    Open Access•Atindra Sapkota, Andriy K Cheburkin et al.•ARTICLE•The Holocene•2007•Cited by: 1•References: 4

    To characterize dust deposition in southern South America for the Holocene, a 542 cm long core from a peat bog in southern Chile (Oreste bog, Isla Navarino) was studied. Peat formation started ~11 160 14 C yr before present (BP). The titanium (Ti) concentration in bulk peat, combined with dry bulk density, and peat accumulation rate, were used to calculate the mineral accumulation rate (MAR) in the Oreste bog. The distribution of calcium (Ca), ma…

  • Energy, Forest, and Indoor Air Pollution Models for Sagarmatha National Park and Buffer Zone, Nepal

    Open Access•Franco Salerno, Gaetano Viviano et al.•ARTICLE•Mountain Research and Development•2010

    This paper presents the results of management-oriented research on energy, forest, and human health issues in a remote mountain area, the Sagarmatha National Park and Buffer Zone (SNPBZ), Nepal. The research was based on a broader, integrated participatory framework ultimately intended for use in adaptive management. The present study focused on the application of a participatory modeling framework to address problems related to energy demand and…

  • Kyr of atmospheric mineral dust deposition in north-eastern China

    Open Access•Steve Pratte, Kunshan Bao et al.•ARTICLE•The Holocene•2019•Cited by: 1•References: 15

    A multi-proxy record of Holocene and late-Pleistocene aeolian mineral dust is reconstructed using a combination of geochemical (trace elements), mineralogical and grain-size analyses on cores from the Hani peatland in north-eastern (NE) China. The dust record displays a sharp increase in dust deposition during the late Holocene in comparison to the rest of the Holocene. This trend is in line with climatic records from the Chinese dust source regi…

Geography (3 works) · Aeolian processes and effects (2 works) · Geology (2 works) · Geology and Paleoclimatology Research (2 works) · Geomorphology (2 works) · Holocene (2 works) · Mineral dust (2 works) · Oceanography (2 works) · Peat (2 works) · Aeolian processes (1 work)

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