The Anatomy of Uncertain Terrains: Soil Topography Characterization and Discharge Analysis of the Baroro River Basin, Northern Philippines
Jericho A. Trio | Patricia Mae M. Clariño | Chris C. Guevarra
Discipline: others in geographical studies
Abstract:
The Baroro River Basin in Northern Luzon is a critical hydrological
feature providing irrigation and biodiversity services. However, the watershed
faces severe vulnerabilities due to the interplay between high-discharge
hydrological behaviors and anthropogenic pressures, specifically rapid Land
Use and Land Cover (LULC) changes that fragment forest blocks and
compromise soil stability. While socio-ecological baselines and local
perceptions of degradation are well documented, there remains a lack of
integrated quantitative modeling of the pedological and lotic processes on
which human settlements depend. Existing studies do not adequately account
for the physical feedback loops among soil properties, river discharge, and
landscape fragmentation. This study used the Soil and Water Assessment Tool+
(SWAT+) in QGIS to simulate hydro-pedological trajectories from 1963 to 2063.
The methodology integrated remote sensing with descriptive statistics to
correlate variables such as Topographic Wetness Index (TWI), Soil Bulk Density
(BD), and Soil Water Potential (SWP) against historical rainfall data. The
analysis revealed the San Juan Anomaly, a 2–3 km zone of amplified TWI and
sediment accumulation acting as a vital hydrological capacitor for riverine
agriculture. Statistical modeling showed a decoupling between precipitation
and discharge, with high upstream porosity (BD ≈ 0.69 g/cm³) buffering storm
runoff. However, a sharp divergence exists between the simulated restorative
potential forest recovery and the observed reality of downstream urban
compaction and soil densification. The basin demands a management paradigm
that treats it as a single functional unit. Immediate policy interventions must
zone the San Juan alluvial scar for sustainable agriculture to prevent
infrastructure encroachment. Long-term strategies should prioritize deep
pedological rehabilitation through upstream reforestation to reduce bulk
density, thereby restoring carbon storage and flood-mitigation capacity.
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