Watershed class prediction equations for three main rock-type watersheds in humid tropical Thailand / by Samakkee Boonyawat.

Thesis (Ph.D. - - Forestry : Forest Resources Mgt.) Universit of the Philippines, College, Laguna.

Includes bibliographical references.

BOONYAWAT, SAMAKKEE. University of the Philippines at Los Banos, December 1986. Watershed Class Prediction Equations for Three Main Rock Type Watersheds in Humid Tropical Thailand. Major Professor: Dr. Severo R. Saplaco

A watershed class prediction equation in Thailand was proposed by Wooldridge (1984). The equation is a multiple linear regression which was developed using five variables, i.e., slope, elevation, landform, soil and geology without any transformation. Theory, however, suggests that the relationship between watershed class and the explanatory variables is not linear and the original equation requires too many variables. Therefore, linearized models were developed using one to five explanatory variables.

An analysis of the different equations tested showed that the equation using logarithmic transformation at the right side of the equation was the most appropriate form. Therefore, this form of the equation was used to develop the equations to predict watershed classes for the three rock type watersheds.

Watershed class prediction equations for all rock types taken together and each rock type considered individually, namely: granite, sandstone and limestone were developed from 300 randomly selected grids of each rock type of northern Thailand. Several variable combinations were used to develop the regression equation for water-shed classes. The equations having the highest R? were selected for field validation. Field validation was necessary to verify the usefulness and accuracy of these selected equations together with the Wooldridge equation. Eight selected watersheds were used: three watershed areas each for granite and sandstone rock type and only two watershed areas of limestone rock type due to the unavailability of additional data on this rock type watershed.

For the granite and limestone rock type watersheds, it was observed that slope alone is sufficiently adequate to predict water-shed class. This is due to the strong direct correlation between slope and soil erosion rate and land use in these watersheds.

For the sandstone rock type watershed, slope alone is not adequate to accurately predict watershed class. This is due to the presence of flat areas on top of these mountain watersheds. This condition is not distinctly present in the granite and limestone rock type watersheds. The inclusion of landform and elevation into the equation makes the model sufficiently accurate in predicting watershed class for the sandstone watershed.

For a single comprehensive watershed class prediction equation, a regression model with dummy variables for the three rock type was developed. The model has slope, elevation, landform, soil and rock type as explanatory variables with zero-one variables representing the rock types. If resources are not limited, this equation could

be used to determine watershed class for the three rock type watersheds instead of using three separate equations. On the other hand, if time is a constraint, the simpler model using one to three variables could be used to predict the watershed class for each rock type watershed.

The predicted watershed classes were used as the bases for mapping the watershed class for the eight selected watersheds. In addition, forest cover and socio-cultural factors were also used in mapping the watershed class.

The prediction equation using three variables (slope, elevation and landform) for sandstone rock type watershed was applied to the Limutan River Watershed in the Philippines which is predominantly a sandstone rock type watershed. The analysis indicated that the equation is highly applicable to this rock type watershed.

Submitted to the University Library 01/07/1994 T-1479