Weathering rates in the Hietajärvi Integrated Monitoring catchment

Rates of Ca and Mg release by weathering were calculated for four soil profiles (Haplic Podzols) in a small forested catchment in eastern Finland (63°10´N, 30°43´E). Three of the profiles were developed on glacifluvial fine sand and one on till, and all derived from granodiorites. Soil weathering rates (mmolc m–2 a–1) were calculated using three methods: Zr depletion, Ca + Mg\temperature sum regression, and the PROFILE model. The first two methods give long-term average rates while the latter gives the current rate. According to the Zr depletion method, the weathering rate of Ca was 7–32 (mean = 19) and that of Mg, 3–16 (mean = 9). According to the regression method, the weathering rate of Ca was 14–19 (mean = 15) and that of Mg, 5–9 (mean = 7). The mean values using the PROFILE model were 10 (Ca) and 3 (Mg). Values were corrected for stone content. Catchment input-output budgets gave values of 18 (Ca) and 8 (Mg).

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Publication Details

Journal
Boreal environment research
Published
2024-12-12
DOI
https://doi.org/10.60910/4u2p-c627
Citations
48
Primary Topic
Geology and Paleoclimatology Research
Type
article
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article

Weathering rates in the Hietajärvi Integrated Monitoring catchment

Timo Tarvainen, Michael Starr, Heikki Tanskanen, Antti‐Jussi Lindroos
48 citations
Boreal environment research
Geology and Paleoclimatology Research
article

Weathering rates in the Hietajärvi Integrated Monitoring catchment

Timo Tarvainen, Michael Starr, Heikki Tanskanen, Antti‐Jussi Lindroos
article en
48 citations

Abstract

Rates of Ca and Mg release by weathering were calculated for four soil profiles (Haplic Podzols) in a small forested catchment in eastern Finland (63°10´N, 30°43´E). Three of the profiles were developed on glacifluvial fine sand and one on till, and all derived from granodiorites. Soil weathering rates (mmolc m–2 a–1) were calculated using three methods: Zr depletion, Ca + Mg\temperature sum regression, and the PROFILE model. The first two methods give long-term average rates while the latter gives the current rate. According to the Zr depletion method, the weathering rate of Ca was 7–32 (mean = 19) and that of Mg, 3–16 (mean = 9). According to the regression method, the weathering rate of Ca was 14–19 (mean = 15) and that of Mg, 5–9 (mean = 7). The mean values using the PROFILE model were 10 (Ca) and 3 (Mg). Values were corrected for stone content. Catchment input-output budgets gave values of 18 (Ca) and 8 (Mg).

Boreal environment researchVol. 3(3)
Life in Land
Geology and Paleoclimatology Research
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