
Existing environment
Topography
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The project site is situated within mixed terrain areas consists of hilly terrain and flatter areas.
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Our project site is low to mid elevated, and the elevation varies from 400 m to 500m.
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The highest point approximately 500 m above sea level is spotted within the project site.
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The topography and contour regimes of the project site are shown in the picture below.

Geology
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Based on the Geological Map of Malaysia published by Mineral and Geoscience department, it is observed that the project site falls under igneous rock located within intrusive rocks, mainly granite with minor granodiorite.
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Besides, certain portion of the areas are composed of schist, phyllite, slate and limestone as well as minor intercalations of sandstone and volcanics.
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The geological contact, fault and fracture zone were found at the study area may indicate the geological process that undergoes at a place locally or regionally.
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In general, our project site consists of several lithologies such as alluvium, tephra dust, and granitic rock.
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Moreover, it is noted that the geological formation of the project site ranges from Permian until Jurassic which is from 145 million years to 298 million years ago. The overall view of general geological profile of the project site area is illustrated in the picture.

Project Site

Project Site
Soil
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The soil in Peninsular Malaysia can be divided into four (4) major groups as steepland soil, sedentary soils, alluvial soils and organic soils.
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Department of Agriculture (DOA) Malaysia have carried out their soil mapping throughout Malaysia to provide information on soil characteristic and suitability and also as planning tool for agriculture purpose.
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With reference to Reconnaissance Soil Map of Peninsular Malaysia (Revised 2002) for Piah Forest Reserve Perak, the type of soils within project site falls under steep land soils which surrounded by soil series of Bekenu and alluvial soils which surrounded by soil series of Telemong.
Steep land soils
Bekenu series
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The Bekenu Series is a representative of the Bekenu Family, which is fine loamy, siliceous, isohyperthermic, red-yellow to yellow Tipik Tualemkuts.
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It characterizes the family and is grown over mixed sedimentary rocks.
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Soils of the Bekenu Series are reformulated here as being identified by their buried, well drained profiles with brownish yellow to yellow subsoil colours controlling the subsoil.
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These soils have an argillic horizon with fine sandy clay loam textures and a ECECclay of less than 24 cmol (+) kg–1 clay in all sub horizons between 25 to 100 cm depth.
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Structures are weak medium to coarse subangular blocky, and stability is friable. Patchy clay skins happen on ped faces.
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They are reconceived here as soils having only an argillic horizon with red-yellow to yellow colour class and a CECclay of smaller than 24 cmol in all sub horizons between 25 cm to 100 cm depth.
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Little is known about the scope in component of the Bekenu Series.
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They commonly happen on rolling, hilly to steep terrain. On the steeper terrain the profiles become somewhat deep and are no longer the Bekenu Series.
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Textures in this soil are consistently fine sandy clay loam and colours are brownish yellow, yellow to olive yellow.
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Structure is commonly weak medium to coarse subangular blocky and consistence friable.
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CECclay values are higher than 16 but less than 24 cmol (+) kg–1 clay. In some profiles a few sub horizons may have a CECclay of less than 16 cmol in the 25 to 100 cm depth

Alluvial soils
Telemong series
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Telemong soils are very crumbly, coarse to moderately coarse textured, very light brown to moderately coarse textured, very light brown to brownish yellow, deep soils evolved on recent riverine alluvium.
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They are originated on the levees and floodplains of the vital and middle-sized rivers where they are issue to additions of material by periodic flooding.
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These are immature soils differing in texture from the fine sand to fine sandy clay foam.
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The surface soil is a very friable, yellowish brown to light yellowish brown, fine loamy sand to fine sandy clay loam, which possesses feebly developed fine subangular blocky to crumb structures. The subsoil is a very friable, light brown to brownish yellow fine sand to fine sandy clay loam, with weakly developed fine and medium subangular blocky to single grain structures
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The soil is regularly porous, well to somewhat overly drained, with many roots, and may on occasion be somewhat grainy.
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The sand commonly contains mica.
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Alternating layers of fine to coarse sand usually occur at depths beneath 100 cm.
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Some of these layers may even show weak soil development in which case they represent buried horizons.
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Very pale reddish yellow mottles are sometimes recognizable at depth, but these are never a conspicuous feature of the profile.

River and Drainage Pattern
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The Perak river basin has a catchment area of about 14,908 km2, which covers about 70% of Perak state.
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It originates from the mountainous Perak-Kelantan-Thailand border of the Belum Forest Reserve in the north.
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The river flows southward from Perak River Hydro Scheme to Telok Intan and subsequently turns west to discharge into the Straits of Melaka at Bagan Datuk
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There are several rivulets and streamlets which are scattered within the project site. The rivulets and streamlets flowed from south Sungai Soh and finally west into Sungai Pelong & east into Sungai Da.
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Sungai Soh has an elevation of 296 meters and is situated north of Kampung Bukit Sapi. Lenggong is situated 9 km southwest of Sungai Soh.
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Rivers that are also connected within the project site are Sungai Salu, Sungai Da, Sungai Palung, Sungai Salu, Sungai Labu and Sungai Dam.
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The nearest water treatment plants are Lenggong Water Treatment Plant, Sauk Water Treatment Plant and Kota Lama Kiri Water Treatment Plant which are located 41.2 km, 10.9 km and 23.9 km from the proposed project site.

1)River pattern of Perak rivers
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2) Map of rivers in Lenggong
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3) River pattern around the project site
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Meteorology
Temperature
The minimum and maximum of the mean annual temperatures data from year 2015 to 2020 at Lenggong, Perak Meteorological station ranges from 27°C to 30°C. It is observed that the temperature recorded at the station showed slightly high temperature from March to November.
Monthly Annual Temperature ( °C) From Year 2015 to 2020

Rainfall
The highest rainfall was recorded in year 2020 (757.4mm) while the lowest year rainfall was recorded in year 2017 (28.17mm). It is noted that high rainfall amount was recorded from April to November.
Monthly Annual Rainfall (mm) From Year 2015 to 2020

Relative humidity
There were no obvious seasonal variations in relative humidity detected throughout the six years
Monthly Annual Relative Humdity Form Year 2015 to 2020

Windspeed
Monthly Annual Windspeed (kmph) From Year 2015 to 2020

Seasonal Monsoon
Generally, the wind condition of the Malaysia shows periodic changes with four seasons namely Northeast (NE) Monsoon (November –March), Southwest (SW) Monsoon (May-September), and two inter-monsoon periods occur during April-May and September-October. The weather station in Lenggong, Perak facing the Strait of Malacca. Therefore, the influences of the sea breeze (Southwest monsoon) can be seen throughout the year. Prevailing southeasterly winds flow across the Strait of Malacca bringing in abundant moisture.
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River water quality
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The sampling of river water was conducted at ten (10) sampling points, namely W1C2A, W1C2B, W2C1A, W2C1B, W2C2A, W2C2B, W3C2A,W3C2B, W4C2A and W4C2B.
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The river water sampling was conducted to assess the existing water quality within the project site.
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The sampling stations were chosen based on the water flow direction of the rivulets within the project site.
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Any impact from the projects during the implementation of project will flow from these rivulets into main watercourse.
River water Sampling Stations & List of Parameters Tested
