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        <identifier>oai:figshare.com:article/33769963</identifier>
        <datestamp>2026-09-25T17:50:38Z</datestamp>
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          <dc:title>Data: &lt;b&gt;Human land modification shifts riverine alkalinity from silicate to carbonate sources across the contiguous United States&lt;/b&gt;</dc:title>
          <dc:creator>Xiying Sun (24910684)</dc:creator>
          <dc:subject>Inorganic geochemistry</dc:subject>
          <dc:subject>Surface water hydrology</dc:subject>
          <dc:subject>Rock weathering</dc:subject>
          <dc:subject>riverine alkalinity export</dc:subject>
          <dc:subject>carbon dioxide removal</dc:subject>
          <dc:description>&lt;p dir="ltr"&gt;Chemical weathering of continental rocks transfers atmospheric carbon dioxide into rivers, but its effects on the carbon cycle depend on whether weathering involves silicate or carbonate minerals. Silicate weathering provides a long-term carbon sink, whereas carbonate weathering is approximately carbon neutral over geologic timescales. Here, we combine an inverse river-chemistry model with interpretable machine learning to map alkalinity fluxes from silicate and carbonate weathering across 1,084 monitoring sites in the contiguous United States.&lt;/p&gt;</dc:description>
          <dc:date>2026-09-25T17:50:38Z</dc:date>
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          <dc:identifier>10.6084/m9.figshare.33769963.v1</dc:identifier>
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