Chronological changes in soil biogeochemical properties of the glacier foreland of Midtre Lovénbreen, Svalbard, attributed to soil-forming factors

Kim, You Jin; Laffly, Dominique; Kim, Se-eun; Nilsen, Lennart; Chi, Junhwa; Nam, Sungjin; Lee, Yong Bok; Jeong, Sujeong; Mishra, Umakant; Lee, Yoo Kyung; Jung, Ji Young

doi:10.1016/j.geoderma.2022.115777

Title: Chronological changes in soil biogeochemical properties of the glacier foreland of Midtre Lovénbreen, Svalbard, attributed to soil-forming factors

Journal Article · 21 February 2022 · Geoderma

DOI: https://doi.org/10.1016/j.geoderma.2022.115777 · OSTI ID:1855800

Kim, You Jin ^[1]; Laffly, Dominique ^[2]; Kim, Se-eun ^[1]; Nilsen, Lennart ^[3]; Chi, Junhwa ^[1]; Nam, Sungjin ^[1]; Lee, Yong Bok ^[4];

^[1]; Mishra, Umakant ^[5]; Lee, Yoo Kyung ^[1]; Jung, Ji Young ^[1]

Korea Polar Research Institute, Incheon (Korea, Republic of)
Univ. of Toulouse (France)
Univ. of Tromso (Norway)
Gyeongsang National Univ., Jinju (Korea, Republic of)
Sandia National Lab. (SNL-CA), Livermore, CA (United States)

We report that Glacier forelands provide an excellent opportunity to investigate vegetation succession and soil development along the chronosequence; however, there are few studies on soil biogeochemical changes from environmental factors, aside from time. This study aimed to investigate soil development and biogeochemical changes in the glacier foreland of Midtre Lovenbreen, Svalbard, by considering various factors, including time. Eighteen vegetation and soil variables were measured at 38 different sampling sites of varying soil age, depth, and glacio-fluvial activity. Soil organic matter (SOM) was quantitatively measured, and the compositional changes in SOM were determined following size-density fractionation. In the topsoil, the soil organic carbon (SOC) and total nitrogen (N) content was found to increase along the soil chronosequence and were highly correlated with vegetation-associated variables. These findings suggest that plant-derived material was the main driver of the light fraction of SOM accumulation in the topsoil. The heavy fractions of SOM were composed of microbially transformed organic compounds, eventually contributing to SOM stabilization within short 90-yr deglaciation under harsh climatic conditions. In addition to time, the soil vertical profiles showed that other environmental parameters, also affected the soil biogeochemical properties. The high total phosphorous (P) content and electrical conductivity in the topsoil were attributed to unweathered subglacial materials and a considerable amount of inorganic ions from subglacial meltwater. The high P and magnesium content in the subsoil were attributed to parent materials, while the high sodium and potassium content in the surface soil were a result of sea-salt deposition. Glacio-fluvial runoff hampered ecosystem development by inhibiting vegetation development and SOM accumulation. This study emphasizes the importance of considering various soil-forming factors, including parent/subglacial materials, aeolian deposition, and glacio-fluvial runoff, as well as soil age, to obtain a comprehensive understanding of the ecosystem development in glacier forelands.

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Research Organization:: Sandia National Laboratories (SNL-CA), Livermore, CA (United States)

Sponsoring Organization:: National Research Foundation of Korea; USDOE; USDOE National Nuclear Security Administration (NNSA); USDOE Office of Science (SC), Biological and Environmental Research (BER)

Grant/Contract Number:: NA0003525

OSTI ID:: 1855800

Report Number(s):: SAND2022-2417J; 703803

Journal Information:: Geoderma, Journal Name: Geoderma Vol. 415; ISSN 0016-7061

Publisher:: ElsevierCopyright Statement

Country of Publication:: United States

Language:: English

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glacio-fluvial runoff
58 GEOSCIENCES
Svalbard
chronosequence
glacier foreland
soil biogeochemical property
soil-forming factors

Title: Chronological changes in soil biogeochemical properties of the glacier foreland of Midtre Lovénbreen, Svalbard, attributed to soil-forming factors

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