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William Larsen
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Lab dissolution experiments and reactive transport models reveal the interplay between alkalinity generation and secondary mineral formation in the Upper Deschutes Basin, Oregon
Field‑Scale Quantification of Enhanced Rock Weathering and net CDR
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Lab dissolution experiments and reactive transport models reveal the interplay between alkalinity generation and secondary mineral formation in the Upper Deschutes Basin, Oregon
 
Field‑Scale Quantification of Enhanced Rock Weathering and net CDR