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        <datestamp>2026-09-29T15:34:12Z</datestamp>
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          <dc:title>An Atomistic
Investigation of Vicinal Calcite Surfaces:
The Effect of Terrace Width on Surface Structure and Adsorption Behavior</dc:title>
          <dc:creator>Evren Ataman (1280742)</dc:creator>
          <dc:creator>Martin P. Andersson (3772123)</dc:creator>
          <dc:creator>S. L. S. Stipp (8045276)</dc:creator>
          <dc:subject>Biotechnology</dc:subject>
          <dc:subject>Environmental Sciences not elsewhere classified</dc:subject>
          <dc:subject>Chemical Sciences not elsewhere classified</dc:subject>
          <dc:subject>Ecology</dc:subject>
          <dc:subject>Biological Sciences not elsewhere classified</dc:subject>
          <dc:subject>therefore significantly wider</dc:subject>
          <dc:subject>likely affected similarly</dc:subject>
          <dc:subject>early molecular dynamics</dc:subject>
          <dc:subject>dominates crystal form</dc:subject>
          <dc:subject>accurate theoretical treatment</dc:subject>
          <dc:subject>∼ 26 å</dc:subject>
          <dc:subject>modeling atomic steps</dc:subject>
          <dc:subject>high step frequencies</dc:subject>
          <dc:subject>relatively narrow terraces</dc:subject>
          <dc:subject>fracture terraces separated</dc:subject>
          <dc:subject>adsorption energies resemble</dc:subject>
          <dc:subject>16 vicinal surfaces</dc:subject>
          <dc:subject>vicinal calcite surfaces</dc:subject>
          <dc:subject>terrace width required</dc:subject>
          <dc:subject>∼ 10 å</dc:subject>
          <dc:subject>vicinal surfaces</dc:subject>
          <dc:subject>adsorption energies</dc:subject>
          <dc:subject>2 å</dc:subject>
          <dc:subject>calcite surface</dc:subject>
          <dc:subject>adsorption energy</dc:subject>
          <dc:subject>adsorption behavior</dc:subject>
          <dc:subject>terrace width</dc:subject>
          <dc:subject>wide must</dc:subject>
          <dc:subject>studied experimentally</dc:subject>
          <dc:subject>steps must</dc:subject>
          <dc:subject>step sites</dc:subject>
          <dc:subject>standard approach</dc:subject>
          <dc:subject>obvious question</dc:subject>
          <dc:subject>obtuse steps</dc:subject>
          <dc:subject>nanometers wide</dc:subject>
          <dc:subject>manually created</dc:subject>
          <dc:subject>made dispersion</dc:subject>
          <dc:subject>explicitly studied</dc:subject>
          <dc:subject>etch pits</dc:subject>
          <dc:subject>computational costs</dc:subject>
          <dc:subject>commonly chosen</dc:subject>
          <dc:subject>atomistic investigation</dc:subject>
          <dc:subject>2 ev</dc:subject>
          <dc:description>The {10.4} calcite surface is commonly chosen for computational
studies because unless some growth modifier is present, it dominates
crystal form in nature and industry. Its rhombohedral symmetry produces
growth and fracture terraces separated by acute and obtuse steps that
have been studied experimentally in vacuum, air, and solution, during
growth and dissolution. The two favored model systems for computational
studies are vicinal surfaces with {10.4} terraces and etch pits or
islands, manually created on {10.4} surfaces. Although experimental
studies demonstrate that even for high step frequencies, terraces
are hundreds to thousands of nanometers wide between steps, computational
costs have driven density functional theory, DFT, and early molecular
dynamics, MD, studies to work with relatively narrow terraces. An
obvious question is how wide must a terrace be to correctly predict
stepped surface structure and properties? We made dispersion-corrected
DFT (DFT-D2) calculations for 16 vicinal surfaces and analyzed the
effect of terrace width on surface structure and adsorption energy.
For accurate theoretical treatment, the distance between the steps
must be around ∼22 Å for acute and ∼26 Å for
obtuse steps. On terraces, structure and adsorption energies resemble
those of {10.4} surfaces at ∼13 Å away, above and below
acute steps; on obtuse steps, the distances are ∼16 Å
away, above and ∼10 Å below. The terrace width required
for convergence is therefore significantly wider than assumed in most
previous studies. This means that the standard approach for modeling
atomic steps on calcite introduces systematic errors, namely up to
0.2 Å for Ca–Ca distances at the step and up to 0.2 eV
for the difference between terrace and step sites, for the adsorption
energy of water. In this study, water served as a probe for adsorption
energy, and though not explicitly studied, adsorption energies for
other molecules are likely affected similarly.</dc:description>
          <dc:date>2026-09-29T00:00:00Z</dc:date>
          <dc:type>Text</dc:type>
          <dc:type>Journal contribution</dc:type>
          <dc:identifier>10.1021/acs.langmuir.6c04191.s001</dc:identifier>
          <dc:relation>https://figshare.com/articles/journal_contribution/An_Atomistic_Investigation_of_Vicinal_Calcite_Surfaces_The_Effect_of_Terrace_Width_on_Surface_Structure_and_Adsorption_Behavior/34024789</dc:relation>
          <dc:rights>CC BY-NC 4.0</dc:rights>
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