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        <identifier>oai:figshare.com:article/33954604</identifier>
        <datestamp>2026-09-23T13:28:48Z</datestamp>
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          <dc:title>&lt;b&gt;Fertilization drives divergent responses of soil aggregation, operational Fe–Al–Mn pools and potential carbon turnover in an acidic tea soil&lt;/b&gt;</dc:title>
          <dc:creator>Huan Li (11826209)</dc:creator>
          <dc:subject>Agricultural management of nutrients</dc:subject>
          <dc:subject>Fertilisers (incl. application)</dc:subject>
          <dc:subject>soil organic carbon</dc:subject>
          <dc:subject>soil aggregation</dc:subject>
          <dc:subject>operationally extractable Fe and Al</dc:subject>
          <dc:subject>carbon mineralization</dc:subject>
          <dc:subject>organo-mineral interactions</dc:subject>
          <dc:subject>aggregate-size dependence</dc:subject>
          <dc:description>&lt;p dir="ltr"&gt;Fertilization can alter soil aggregation and operationally extractable metal pools without producing equivalent changes in carbon turnover. We tested how six fertilizer regimes affected wet-sieved aggregate structure, operational Fe, Al and Mn pools, bulk X-ray diffraction profiles and 30-day, aggregate-resolved potential carbon mineralization in an acidic tea soil. The inferential archive comprised three spatially distinct, independent field replicate plots per regime; synchrotron-radiation FTIR maps provided descriptive microscale context. Operational Fe–Al–Mn pools showed the strongest multivariate treatment response (R²=0.832, q=0.00025), whereas bulk XRD profiles did not differ after correction (q=0.236). No corrected evidence supported a shared treatment-response configuration across aggregation, operational-mineral, mineralization and XRD domains. After treatment centring, operational-mineral pools covaried with fraction-specific potential mineralization (RV=0.638, q=0.0081), provisionally localizing to 0.25–2 mm aggregates (RV=0.498, q=0.0453). Within this fraction, bulk-soil Feₒ was negatively associated with mineralization (ρ=−0.715; hypothesis-guided 40-edge q=0.0223), and the association remained similar under treatment-blind imputation (ρ=−0.723). These findings are consistent with, but do not confirm, aggregate-size-dependent mineral–turnover coupling. Aggregate stability, Feₒ and bulk mineralogy should not be treated as interchangeable proxies for persistent soil-carbon stabilization.&lt;/p&gt;</dc:description>
          <dc:date>2026-09-23T13:28:48Z</dc:date>
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          <dc:identifier>10.6084/m9.figshare.33954604.v2</dc:identifier>
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          <dc:rights>CC BY 4.0</dc:rights>
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