Monday, 7 November 2005
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The Soil Climate Regimes of Puerto Rico-Reassessment and Implications.

Jorge L. Lugo-Camacho, University of Puerto Rico-Mayagüez Campus, Urb. Mansiones de Monterrey, 627 Calle Asturias, Yauco, PR 00698-2576

THE SOIL CLIMATE REGIMES OF PUERTO RICO-REASSESSMENT AND IMPLICATIONS

Jorge L. Lugo-Camacho1, Miguel A. Muñoz2, Friedrich Beinroth3, Juan Pérez-Bolívar4 and Gregory Brannon5

1 Graduate Student, Agronomy and Soils Department , UPR-Mayagüez 2 Researcher, Agronomy and Soils Department, UPR-Mayagüez 3 Professor, Agronomy and Soils Department, UPR-Mayagüez 4 Associate Professor, Agronomy and Soils Department, UPR-Mayagüez 5 Soil Data Quality Specialist, USDA-NRCS.

Abstract

The soil climate regimes of Puerto Rico were evaluated and their implications discussed. The main objective of this project was to evaluate soil moisture and temperature regimes in Puerto Rico. Average monthly precipitation and temperature from 90 weather stations of the U.S. Weather Service were used to compute the soil moisture and temperature regimes using the Newhall Simulation Model program version 1.0. This model was validated with soil moisture and temperature data of five weather stations of the USDA-NRCS. The study confirms the existence of soils with an aridic moisture regime in the island. The NSM identified an area of 25,450 ha with an aridic moisture regime along the south coast and on Mona Island. This is first official recognition of an aridic moisture regime in Puerto Rico. An area with ustic soil moisture regime in the northwest corner of the island was also identified. This area is currently recognized as an udic moisture regime. The isomesic temperature regime, previously identified at the Caribbean National Forest was not identified by the Newhall Simulation Model. The isothermic temperature regime previously identified in areas above 600 m over sea level, were identified by the model in areas above 900 m under a udic moisture regime and above 750 m under perudic moisture regime. As a result these changes in the soil climate regimes, approximately 50 soil series need to be reclassified and new soil series will have to be proposed.


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