Soil development rates from an optically stimulated luminescence-dated beach ridge sequence in Northern Jutland, Denmark

Research output: Contribution to journal › Journal article › Research › peer-review

Standard

Soil development rates from an optically stimulated luminescence-dated beach ridge sequence in Northern Jutland, Denmark. / Nielsen, Asger Habekost; Elberling, Bo; Pejrup, Morten.

In: Canadian Journal of Soil Science, Vol. 90, No. 2, 2010, p. 295-307.

Research output: Contribution to journal › Journal article › Research › peer-review

Harvard

Nielsen, AH, Elberling, B & Pejrup, M 2010, 'Soil development rates from an optically stimulated luminescence-dated beach ridge sequence in Northern Jutland, Denmark', Canadian Journal of Soil Science, vol. 90, no. 2, pp. 295-307. https://doi.org/10.4141/CJSS09020

APA

Nielsen, A. H., Elberling, B., & Pejrup, M. (2010). Soil development rates from an optically stimulated luminescence-dated beach ridge sequence in Northern Jutland, Denmark. Canadian Journal of Soil Science, 90(2), 295-307. https://doi.org/10.4141/CJSS09020

Vancouver

Nielsen AH, Elberling B, Pejrup M. Soil development rates from an optically stimulated luminescence-dated beach ridge sequence in Northern Jutland, Denmark. Canadian Journal of Soil Science. 2010;90(2):295-307. https://doi.org/10.4141/CJSS09020

Author

Nielsen, Asger Habekost ; Elberling, Bo ; Pejrup, Morten. / Soil development rates from an optically stimulated luminescence-dated beach ridge sequence in Northern Jutland, Denmark. In: Canadian Journal of Soil Science. 2010 ; Vol. 90, No. 2. pp. 295-307.

Bibtex

@article{220bfd507eac11df928f000ea68e967b,
title = "Soil development rates from an optically stimulated luminescence-dated beach ridge sequence in Northern Jutland, Denmark",
abstract = "Rates of podzolic soil development in sandy, temperate soils were quantified based on 14 soil pedons with five substrata from a beach ridge chronosequence near Jerup, Northern Denmark (578N). Soil pH, organic carbon (C) as well as extractable iron (Fe) and aluminium (Al) were measured. The age of each pedon and soil stratum was measured by optically stimulated luminescence (OSL) dating and used to estimate soil development rates. Soils were divided into five groups from Typic Haplorthods and Entic Alorthods with a mean OSL age of 29659294 yr to Typic Quartzipsamments with a mean OSL age of 22911 yr. Acidification rates during the first 200 yr were1.9pH units per 100 yr in the A horizons and C-sequestration rates were25 g C m2 yr1 (excluding litter accumulation). After1500 yr, the mineral soil C stocks stabilised around 13.092.0 kg C m2. Translocation rates of Al into B horizons were0.3 kg Al m2 per 1000 yr, while translocation rates for Fe were scattered. Our study illustrates the potential of OSL dating in chronosequence studies to quantify soil development rates.",
keywords = "Faculty of Science, Soil development rates; chronosequence; OSL-dating; C-sequestration rates and translocation rates",
author = "Nielsen, {Asger Habekost} and Bo Elberling and Morten Pejrup",
year = "2010",
doi = "10.4141/CJSS09020",
language = "English",
volume = "90",
pages = "295--307",
journal = "Canadian Journal of Soil Science",
issn = "0008-4271",
publisher = "Agricultural Institute of Canada",
number = "2",

}

RIS

TY - JOUR

T1 - Soil development rates from an optically stimulated luminescence-dated beach ridge sequence in Northern Jutland, Denmark

AU - Nielsen, Asger Habekost

AU - Elberling, Bo

AU - Pejrup, Morten

PY - 2010

Y1 - 2010

N2 - Rates of podzolic soil development in sandy, temperate soils were quantified based on 14 soil pedons with five substrata from a beach ridge chronosequence near Jerup, Northern Denmark (578N). Soil pH, organic carbon (C) as well as extractable iron (Fe) and aluminium (Al) were measured. The age of each pedon and soil stratum was measured by optically stimulated luminescence (OSL) dating and used to estimate soil development rates. Soils were divided into five groups from Typic Haplorthods and Entic Alorthods with a mean OSL age of 29659294 yr to Typic Quartzipsamments with a mean OSL age of 22911 yr. Acidification rates during the first 200 yr were1.9pH units per 100 yr in the A horizons and C-sequestration rates were25 g C m2 yr1 (excluding litter accumulation). After1500 yr, the mineral soil C stocks stabilised around 13.092.0 kg C m2. Translocation rates of Al into B horizons were0.3 kg Al m2 per 1000 yr, while translocation rates for Fe were scattered. Our study illustrates the potential of OSL dating in chronosequence studies to quantify soil development rates.

AB - Rates of podzolic soil development in sandy, temperate soils were quantified based on 14 soil pedons with five substrata from a beach ridge chronosequence near Jerup, Northern Denmark (578N). Soil pH, organic carbon (C) as well as extractable iron (Fe) and aluminium (Al) were measured. The age of each pedon and soil stratum was measured by optically stimulated luminescence (OSL) dating and used to estimate soil development rates. Soils were divided into five groups from Typic Haplorthods and Entic Alorthods with a mean OSL age of 29659294 yr to Typic Quartzipsamments with a mean OSL age of 22911 yr. Acidification rates during the first 200 yr were1.9pH units per 100 yr in the A horizons and C-sequestration rates were25 g C m2 yr1 (excluding litter accumulation). After1500 yr, the mineral soil C stocks stabilised around 13.092.0 kg C m2. Translocation rates of Al into B horizons were0.3 kg Al m2 per 1000 yr, while translocation rates for Fe were scattered. Our study illustrates the potential of OSL dating in chronosequence studies to quantify soil development rates.

KW - Faculty of Science

KW - Soil development rates; chronosequence; OSL-dating; C-sequestration rates and translocation rates

U2 - 10.4141/CJSS09020

DO - 10.4141/CJSS09020

M3 - Journal article

VL - 90

SP - 295

EP - 307

JO - Canadian Journal of Soil Science

JF - Canadian Journal of Soil Science

SN - 0008-4271

IS - 2

ER -

ID: 20446715