Articles | Volume 11, issue 3
https://doi.org/10.5194/esurf-11-475-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esurf-11-475-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Mobile evaporite enhances the cycle of physical–chemical erosion in badlands
Department of Geography, National Taiwan University, No. 1, Sec. 4,
Roosevelt Rd., Taipei 10617, Taiwan
German Research Centre for Geosciences (GFZ), Telegrafenberg 14473,
Potsdam, Germany
Pei-Hao Chen
Department of Geography, National Taiwan University, No. 1, Sec. 4,
Roosevelt Rd., Taipei 10617, Taiwan
Erica D. Erlanger
German Research Centre for Geosciences (GFZ), Telegrafenberg 14473,
Potsdam, Germany
Jens M. Turowski
German Research Centre for Geosciences (GFZ), Telegrafenberg 14473,
Potsdam, Germany
German Research Centre for Geosciences (GFZ), Telegrafenberg 14473,
Potsdam, Germany
Tse-Yang Teng
Department of Geography, National Taiwan Normal University, No. 162, Sec. 1, Heping E. Rd., Taipei 106, Taiwan
Jiun-Chuan Lin
Department of Geography, National Taiwan University, No. 1, Sec. 4,
Roosevelt Rd., Taipei 10617, Taiwan
Jr-Chuang Huang
Department of Geography, National Taiwan University, No. 1, Sec. 4,
Roosevelt Rd., Taipei 10617, Taiwan
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Short summary
Observations of the interaction between extreme physical erosion and chemical weathering dynamics are limited. We presented major elements of stream water in the badland catchment at 3 h intervals during a 3 d typhoon. The excess sodium in the evaporite deposits causes material dispersion through deflocculation, which enhances the suspended sediment flux. Moreover, we observed a shift from predominantly evaporite weathering at peak precipitation to silicate weathering at peak discharge.
Observations of the interaction between extreme physical erosion and chemical weathering...