Ghent University Academic Bibliography

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Your filters: cql: author="Yin, Qiuzhen" or (type any "bookEditor journalEditor issueEditor" and editor="Yin, Qiuzhen")

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Driving factors of interglacial paleosol formation on the Chinese loess plateau and the effect of precession and ice sheets

Keerthika Nirmani Ranathunga (UGent) , Peter Finke (UGent) , Qiuzhen Yin, Zhipeng Wu, Qingzhen Hao and Hao Lu

(2023) QUATERNARY SCIENCE REVIEWS. 300.
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Calibrating SoilGen2 for interglacial soil evolution in the Chinese Loess Plateau considering soil parameters and the effect of dust addition rhythm

Keerthika Nirmani Ranathunga (UGent) , Peter Finke (UGent) , Qiuzhen Yin and Yanyan Yu

(2022) QUATERNARY INTERNATIONAL. 607. p.100-112
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Unraveling loess records of climate change from the Chinese loess plateau using process-based models

Peter Finke (UGent) , Keerthika Nirmani Ranathunga Arachchige, Ann Verdoodt (UGent) , Yanyan Yu and Qiuzhen Yin

(2021) Hydrogeology, chemical weathering and soil formation. In Geophysical Monograph Series 257. p.163-175
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Soil modeling for soil loss tolerance estimations : exploring natural baselines and long-term variations

Keerthika Nirmani Ranathunga (UGent) , Peter Finke (UGent) , Qiuzhen Yin, Ann Verdoodt (UGent) and YanYan Yu

(2021) GLOBAL AND PLANETARY CHANGE. 204.
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Climate-soil model reveals causes of differences between Marine Isotope Stage 5e and 13 paleosols

Peter Finke (UGent) , Qiuzhen Yin, Nicholas John Bernardini and Yanyan Yu

(2018) GEOLOGY. 46(2). p.99-102

Academic Bibliography

Driving factors of interglacial paleosol formation on the Chinese loess plateau and the effect of precession and ice sheets

Calibrating SoilGen2 for interglacial soil evolution in the Chinese Loess Plateau considering soil parameters and the effect of dust addition rhythm

Unraveling loess records of climate change from the Chinese loess plateau using process-based models

Soil modeling for soil loss tolerance estimations : exploring natural baselines and long-term variations

Climate-soil model reveals causes of differences between Marine Isotope Stage 5e and 13 paleosols

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