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        <full_title>International Journal of Applied Mathematics Computational Science and Systems Engineering</full_title>
        <issn media_type="electronic">2766-9823</issn>
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        <titles>
          <title>Computational Evaluation of Open Irrigation Channel Flow with Variable Depth Based on the 1D–2D Saint–Venant Equations</title>
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        <contributors>
          <person_name sequence="first" contributor_role="author">
            <given_name>Irla</given_name>
            <surname>Mantilla</surname>
            <affiliations>
              <institution>
                <institution_name>Universidad Nacional de Ingeniería, Av. Túpac Amaru 210, Rímac, 27 PERÚ</institution_name>
              </institution>
            </affiliations>
          </person_name>
          <person_name sequence="additional" contributor_role="author">
            <given_name>Mihael</given_name>
            <surname>Arce</surname>
            <affiliations>
              <institution>
                <institution_name>Universidad Nacional de Ingeniería, Av. Túpac Amaru 210, Rímac, 27 PERÚ</institution_name>
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        <jats:abstract>
          <jats:p>This work presents a computational evaluation of water flow in an open agricultural irrigation channel with variable depth using the one- and two-dimensional Saint–Venant equations. The mathematical formulation is derived from mass and momentum conservation principles for shallow water flow. A linearized one-dimensional model is first analyzed to obtain an equivalent wave-type equation through perturbation and separation of variables. A nonlinear formulation with variable bottom topography and discontinuities is then considered, incorporating analytical integration with Dirac delta representation of step changes in the channel bed. The two-dimensional Saint–Venant system is subsequently introduced to model spatially distributed depth and velocity fields. Numerical implementation is carried out using a finite difference FTCS scheme, including stability constraints of CFL type. Simulations illustrate the temporal evolution of water depth under step-type bottom discontinuities in both 1D and 2D configurations. The results show the capacity of the model to capture wave propagation, depth transitions, and spatial flow redistribution. The framework provides a computational basis for hydraulic analysis and future high-resolution modeling of irrigation channels.</jats:p>
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        <publication_date media_type="print">
          <month>07</month>
          <day>16</day>
          <year>2026</year>
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        <publication_date media_type="online">
          <month>07</month>
          <day>16</day>
          <year>2026</year>
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        <pages>
          <first_page>116</first_page>
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          <item_number item_number_type="article_number">11</item_number>
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          <doi>10.37394/232026.2026.8.11</doi>
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