Evolution of soil erosion rates in alpine soils of the Central Rocky Mountains using fallout Pu and δ13C

Raquel Portes, Dennis Dahms, Dagmar Brandová, Gerald Raab, Marcus Christl, Peter Kühn, Michael Ketterer, Markus Egli

Research output: Contribution to journalArticle

3 Citations (Scopus)

Abstract

Data from soil chronosequences have been widely used to quantify soil formation and weathering rates, but are less used to determine erosion rates and the stabilisation of moraines over time. We hypothesise that soil erosion rates on moraine hillslopes decrease over time as soils evolve and slopes stabilise. We selected a sequence of moraines in the Wind River Range (Central Rocky Mountains) to study these processes over time. Moraine ages were based on 10Be surface exposure dating of moraine boulders. Quantitative soil erosion and accumulation rates along slopes with similar exposures, lengths and gradients were determined from profile patterns of 239+240Pu radionuclides. We used stable carbon isotopes (δ13C) in relation with the total soil organic carbon (SOC) content for qualitative information about soil erosion. The 10Be boulder exposure ages revealed that the moraines were deposited during the Younger Dryas and the pre Bølling–Allerød episodes of the late Pleistocene. The morphology of the soils suggests a complex history of development and shows that both erosion and aeolian deposition have affected the soils. The 239+240Pu measurements revealed that erosion rates strongly decrease with time as soils develop. A weakly developed soil (Cambisol) is found on the youngest moraine (11.8 ka) that exhibits an erosion rate, depending on the calculation procedure, in the range of 260 to 520 t km−2 a−1. With time the erosion rate rapidly decreases to almost zero, presumably as a full vegetation cover develops. Bioturbation and/or dust influx is increasingly obvious with increasing age of the soils, as evidenced by the comparison of δ13C and SOC. The mass balance of the oldest soil (15.8 ka) indicates that the slopes have reached a geomorphological stability with little or no net erosion. Aeolian influx appears to be the primary factor to account for mass changes in the oldest soil.

Original languageEnglish (US)
Pages (from-to)257-269
Number of pages13
JournalEarth and Planetary Science Letters
Volume496
DOIs
StatePublished - Aug 15 2018
Externally publishedYes

Fingerprint

soil erosion
Rocky Mountains (North America)
Fallout
fallout
erosion rate
Erosion
soils
Soils
mountain
erosion
soil
moraine
glacial drift
slopes
Wind River Range (WY)
Organic carbon
organic carbon
Cambisol
weathering rate
carbon isotopes

Keywords

  • carbon isotopes
  • Late Pleistocene
  • Pu isotopes
  • slope stability
  • soil chronosequence
  • Wind River Range

ASJC Scopus subject areas

  • Geophysics
  • Geochemistry and Petrology
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science

Cite this

Evolution of soil erosion rates in alpine soils of the Central Rocky Mountains using fallout Pu and δ13C. / Portes, Raquel; Dahms, Dennis; Brandová, Dagmar; Raab, Gerald; Christl, Marcus; Kühn, Peter; Ketterer, Michael; Egli, Markus.

In: Earth and Planetary Science Letters, Vol. 496, 15.08.2018, p. 257-269.

Research output: Contribution to journalArticle

Portes, Raquel ; Dahms, Dennis ; Brandová, Dagmar ; Raab, Gerald ; Christl, Marcus ; Kühn, Peter ; Ketterer, Michael ; Egli, Markus. / Evolution of soil erosion rates in alpine soils of the Central Rocky Mountains using fallout Pu and δ13C. In: Earth and Planetary Science Letters. 2018 ; Vol. 496. pp. 257-269.
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AU - Christl, Marcus

AU - Kühn, Peter

AU - Ketterer, Michael

AU - Egli, Markus

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AB - Data from soil chronosequences have been widely used to quantify soil formation and weathering rates, but are less used to determine erosion rates and the stabilisation of moraines over time. We hypothesise that soil erosion rates on moraine hillslopes decrease over time as soils evolve and slopes stabilise. We selected a sequence of moraines in the Wind River Range (Central Rocky Mountains) to study these processes over time. Moraine ages were based on 10Be surface exposure dating of moraine boulders. Quantitative soil erosion and accumulation rates along slopes with similar exposures, lengths and gradients were determined from profile patterns of 239+240Pu radionuclides. We used stable carbon isotopes (δ13C) in relation with the total soil organic carbon (SOC) content for qualitative information about soil erosion. The 10Be boulder exposure ages revealed that the moraines were deposited during the Younger Dryas and the pre Bølling–Allerød episodes of the late Pleistocene. The morphology of the soils suggests a complex history of development and shows that both erosion and aeolian deposition have affected the soils. The 239+240Pu measurements revealed that erosion rates strongly decrease with time as soils develop. A weakly developed soil (Cambisol) is found on the youngest moraine (11.8 ka) that exhibits an erosion rate, depending on the calculation procedure, in the range of 260 to 520 t km−2 a−1. With time the erosion rate rapidly decreases to almost zero, presumably as a full vegetation cover develops. Bioturbation and/or dust influx is increasingly obvious with increasing age of the soils, as evidenced by the comparison of δ13C and SOC. The mass balance of the oldest soil (15.8 ka) indicates that the slopes have reached a geomorphological stability with little or no net erosion. Aeolian influx appears to be the primary factor to account for mass changes in the oldest soil.

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