A watershed is simply defined as all land area that drains into a stream system, upstream from its mount, and is surrounded by a divide. A watershed, if properly managed, will supply water for agricultural and industrial use, including water for domestic consumption [2]. Further, Paragas [2] mentioned that three (3) watershed forest reserves covering 3179 hectares were proclaimed. This new proclamation increased the number of watershed forest reserves to 117, covering an area of 1368 million hectares. The Philippine watershed areas, on the other hand, are already in critical condition [2]. Deforestation contributes a lot to the degradation of almost 2.6 million hectares of identified critical watershed areas of the country.

Watershed management is the process of organizing and directing the use of land, water, and other natural resources in a watershed in order to provide appropriate goods and services while minimizing the impact on the soil and watershed resources [7]. It entails socioeconomic, human-institutional, and biophysical interactions between soil and water, as well as the connection between upland and downstream areas [8]. Section 3 of Presidential Decree (PD) No. 705, known as the Revised Forestry Code of the Philippines, mandated that critical areas of a river system supporting existing and proposed hydroelectric power and irrigation works need immediate rehabilitation as they are too fast denudation causing accelerated erosion and destructive floods. These areas must be closed for logging until fully rehabilitated [9]. DENR Memorandum Circular No. 17 series of 1989 states that “effective immediately, all DENR offices involved in planning and implementation of watershed and reforestation programs and projects are instructed to incorporate Assisted Natural Regeneration (ANR) methods in all such projects, whenever applicable, regardless of whatever these are carried out by the administration, by contract or by combination thereof.

Forested watersheds improve water quality and enhance water storage naturally regulate stream flows, reduce flood damages and storm water runoff, replenish groundwater and provide a myriad of other benefits [10]. Moreover, water draining from undisturbed forested watersheds is generally of the highest quality, particularly with regard to beneficial uses including drinking water, aquatic habitat for native species, and contact recreation [11].

Forest inventory is a process for obtaining information on the quality and quantity of forest resources and forms the foundation of forest planning and forest policy. While the early concept of sustainable forest management and forest inventory focused on timber production [12]. Modern forest inventory is well-established means of obtaining information on forest areas, usually with an emphasis on timber resources [13]. In addition, forest inventory essentially started with mapping of forest stands as homogeneous units with regard to species composition, density, and size, and strongly developed during the 20^th century with the establishment of a wide array of sampling techniques, focusing on timber volume and forest stand structure [14] [15].

In the conduct of the study, different materials were used such as a record book, ballpen, meter stick, steel tape, and tree caliper for the collection of data. Quadrant samples were located using a GPS device in obtaining the coordinates and elevation.

This study followed the principles of research ethics to guarantee that all plant subjects were not harmed during identification. Municipal Mayor, Barangay officials, and other involved persons had their own free will to participate and they have fully informed regarding the procedures of the study and any potential risks.

The secondary data such as the area, elevation, slope, climatic factors, forest soil component, major land uses, and other related information were gathered from maps and reports from the Department of Environment and Natural Resource (DENR), Water District of the Local Government Unit (LGU) of Pandan and barangays of San Rosario, Guia, and Candari.

Assessment of floral components was conducted particularly for the tree, palm, and bamboo species through Quadrant Sampling using stratified random sampling. With the use of a topographic map, there were seven (7) elevation ranges identified and these were the following (Table 1).

A maximum of three (3) by 50 m × 20 m (1000 m²) plots were laid out at every elevation range. And a total of 21 sampling plots were laid out. However, the actual location of the plots was dependent on the accessibility of the site.

Species of trees, palms, and bamboo inside the plot were identified with the help of local experts, available books, journals, and references such as the book of [16] and [17] and counted accordingly. Other trees, palm, and bamboo species outside the plots were also documented.

The data gathered were analyzed using descriptive statistics. The flora species were identified and the average height of trees, volume, and canopy cover were determined.

Bugang River watershed was estimated at 1881.43 hectares or approximately 18.23 percent of the total upland areas of the municipality of Pandan. The highest elevation of the watershed was 400 meters above sea level (masl) and the mean elevation of the watershed is about 54 masl. The percent slope of the area gradually increases as the elevation increases. The lower elevations were gently sloping to undulating, middle elevation ranges were rolling to moderately steep, and the height elevation ranges were steep to very steep. The slope of the area was recorded from 50 to 100 masl lies between 3 to 8 percent, from 100 to 150 meters the slope was within the range of 9 to 18 percent, and from 150 to 200 meters the slope was from 19 to 30 percent. The slope ranges from 31 to 50 percent when the elevation above sea level reached 250 to 300 meters and 50 percent and above when the elevation measures up to 300 to 400 masl. Elevation and latitude are well-known broad-scale factors affecting species richness [19]. In addition, the climatic factors (temperature, potential evaporation, length of the growing season, humidity, air pressure, ultraviolet radiation, moisture index, and rainfall) vary with elevation [20].

The municipality of Pandan belongs to climate Type III where seasons were not very pronounced, it is relatively dry from November to April and wet for the rest of the year. The average annual temperature in the area is 27.5˚C and about 4448 mm of precipitation falls annually. The driest month is April, with about 87 mm of rain, and the month of July has the most rainfall amount, with an average of 679 mm. The warmest month is May with an average of 28.8˚C and January is the coldest with an average temperature of 26.3˚C. Land-use change was observed in the area over a five-year period (2010-2015). Changes in land use have an impact on the watershed, particularly on run-off volume, sedimentary yield, and stream flows. According to a field survey and interviews with local residents, a portion of the watershed was a Kaingin area. The conservation efforts of the government and other involved organizations, in collaboration with the local people, were strengthened in the recent year, resulting in partial reforestation and rehabilitation of the area.

The soil component of the watershed area was identified as Alimodian Sandy clay with medium granular and slightly friable structure and sandy clay with gravel soil texture. The clay loam soil was reddish-brown to yellow-red in color and ranged in elevation from 50 to 150 masl with nearly level to moderately steep lands. Species from the Araliaceae and Meliaceae families were the most numerous at this elevation. On the elevated plains, moderately steep, rolling hills, and mountain landscapes with elevations ranging from 150 to 300 masl, a clayey, deep, and well-drained soil was observed, which was dominated by species from the Bignoniaceae and Fabaceae families. Elevation ranging from 300 to 400 masl, brown to reddish clay soi was observed on elevated plains, hilly to moderately steep to steep mountainous areas. The species belonged to the Anacardiaceae family, and the genus Buchanania dominated in this elevation range. In general, the soil structure was determined visually, and it was discovered that the soil structure in the area was granular, with nearly spherical grains that allowed water to circulate freely. Soil is an important component of the forest ecosystem as it helps regulate important ecosystem processes, such as nutrient uptake, decomposition, and water availability [21].

The height of the piled-up forest residues was used to determine the thickness of the forest floor. The thickness of the forest floor was measured in various sampling areas. The elevation range of 50 to 100 masl had 0.04 to 0.69 cm piled forest residue, 100 to 200 masl had 2.02 cm to 2.67 cm piled forest residue, 200 to 300 masl had 2.68 cm to 3.33 cm piled forest residue, and 300 to 400 masl had the highest piled residue of about 4.00 to 4.65 cm. It was discovered that as elevation increased, the thickness of the forest floor increased. The difference in forest floor thickness was influenced by the density of trees by elevation level, as more trees were found at higher elevations, affecting the rate of accumulation of litterfall. Furthermore, the higher the elevation, the higher the humidity in a forested area aids in the rate of decomposition of organic materials [22].

The Bugang River watershed is home to a diverse range of tree and palm species. The total number of species discovered in the sampling plots was 1583, which included trees, palms, and bamboo. Gogo (Entada phaseoloides) had the most, accounting for 222 of the total species (14 percent). This study included 60 trees, palms, and bamboo species from 31 families and 52 genera, and 47 of the 60 species were identified, leaving 13 unidentified due to a lack of available references (Table 2).

Outside of the sampling plots tree, palm, and bamboo species were identified (Table 3). These species were abundant in number and can be found on river easements, residential areas, and in some parts of the forest.

There were five (5) palm species and 1 higher form of grass among the 60 species (Table 4). The majority of the palm and bamboo were observed at an elevation ranging from 50 to 150 masl, near local community plantations and cultivated areas. Furthermore, some areas had previously been subjected to slash and burn (Kaingin), and these areas were now covered with grasses, coconut, and bamboo.

All trees with a diameter of 10 cm or greater were measured. Figure 1 demonstrated that the average diameter of species decreased as elevation increased, with the highest average diameter of species identified at 50 - 100 masl elevation and the lowest at 300 - 350 masl elevation. Species at higher elevation levels were denser than those at lower elevation levels. The density of species per area influences the development of stem diameter [23], but other factors such as edaphic and climatic factors may also influence the secondary growth of tree species.

The average height of species was determined for each elevation range. The highest average height of species was recorded at an elevation of 300 - 350 masl, while the lowest was recorded at elevations of 200 - 250 masl. In the 300 - 350 masl range, species from the Lecythidaceae and Sterculiaceae families predominated. The study hypothesized that increasing elevation has a direct effect on the height of tree species. Figure 2 showed, however, that the average height of species did not increase significantly as elevation increased.

The volume varies by species, in this study, and the total volume of the trees and palms in the study area was 102.31 cubic meters (m³), with a mean volume of 0.1393 m³ per tree. The average volume of trees and palms at various elevation levels was 73.64 m³. Figure 3 shows that the tree species in the 50 - 100 masl elevation range have the highest average volume of 30.56 m³ and the lowest average volume of 0.76 m³ in the 300 - 400 masl elevation range. There was also a decrease in average volume at 200 - 250 masl, which was caused by a change in land use.

Strata were determined for each tree and classified as Suppressed (S), Intermediated (I), Codominant (CD), and Dominant (D). Dominant species accounted for 3 percent of all species. These species were found at elevations ranging from 50 to 100 masl. There were 282 codominant species, accounting for 18 percent of the total number of species, 717 intermediate species, accounting for 45 percent of the total number of species, and 542 suppressed species, accounting for 34 percent of the total number of species. In higher elevations, suppressed species were abundant, and these species were saplings and seedlings (Figure 4).

The total crown diameter of the dominant tree species determined the area canopy cover. The elevation range of 250 - 300 masl had the lowest canopy cover of 266.91 m² and the highest canopy cover of 780.42 m². The study area's total canopy area was 3154.67 m² (Figure 5).