Effects of water quality in oil palm production landscapes on tropical waterbirds in Peninsular Malaysia

2015 ◽  
Vol 30 (5) ◽  
pp. 941-949 ◽  
Author(s):  
Petra Sulai ◽  
Siti Nurhidayu ◽  
Najjib Aziz ◽  
Mohamed Zakaria ◽  
Holly Barclay ◽  
...  
Mycobiology ◽  
2015 ◽  
Vol 43 (2) ◽  
pp. 107-117 ◽  
Author(s):  
Yit Kheng Goh ◽  
Teik Khiang Goh ◽  
Nurul Fadhilah Marzuki ◽  
Hun Jiat Tung ◽  
You Keng Goh ◽  
...  

2016 ◽  
Vol 9 (3) ◽  
pp. 277-284 ◽  
Author(s):  
Mohammad Zahirul Haque ◽  
Sahibin Abd Rahim ◽  
Md. Pauzi Abdullah ◽  
Ahmad Fuad Embi ◽  
Rahmah Elfithri ◽  
...  

2017 ◽  
Author(s):  
Arolu Ayanda Fatai ◽  
Jusop Shamshuddin ◽  
Che Ishaq Fauziah ◽  
Othman Radziah ◽  
Mohsen Bohluli

Abstract. Most of the soils in the upland areas of Peninsular Malaysia are classified as Ultisols. Oil palm production on these soils is usually limited by their inherent low soil productivity. However, the crop is cultivated successfully on most of the soils following right soil management practices. A study was conducted in Bera, Malaysia to determine the characteristics and fertility of an Ultisol cropped to oil palm for many years continuously. In this study, the soil in the plantation was sampled, analyzed and classified. The soil under study was formed under tropical environment with udic moisture regime on fine-grained sedimentary rocks mixed with tuffs of Permian age. Due to very long exposure to the condition of high temperature and high rainfall throughout its development, the soil in the area was reddish in color, clayey, deep and highly weathered. The study found that the clay fraction of the soil was dominated by kaolinite, hematite, goethite and gibbsite; hence, the CEC and basic cations were low. Besides, soil reaction was acidic in nature with soil pH slightly below 5, but the exchangeable Al was more than 1 cmolc/kg soil. However, it was believed that these inherent characteristics were not expected to significantly affect the production of oil palm grown on the soil. With proper agronomic practices, the area can be utilized for oil palm production sustainably.


2013 ◽  
Vol 34 (20) ◽  
pp. 7424-7446 ◽  
Author(s):  
Kian Pang Tan ◽  
Kasturi Devi Kanniah ◽  
Arthur Philip Cracknell

2012 ◽  
Vol 599 ◽  
pp. 237-240 ◽  
Author(s):  
Faridah Othman ◽  
Mohamed Elamin Alaa Eldin

The Klang river basin is located within the state of Selangor and Kuala Lumpur, Malaysia. The Klang River drains an area of 1,288 km2 from the steep mountain rain forests of the main Central Range along Peninsular Malaysia to the river mouth in Port Klang, covering a distance of 120 km. It originates from the northern part of Selangor, drains the Klang Valley, and finally discharges itself into the Straits of Malacca. The pollution discharges for various locations along the river basin was obtained from the Water Quality and GIS group. The pollutants can come from point sources (PS) such as industrial wastewater, municipal sewers, wet market, sand mining and landfill. Pollutants can also come from non-point sources (NPS) such as agricultural or urban runoff, and commercial activity such as forestry, and construction due to rainfall event. Mathematical–computational modeling of river water quality is possible but requires an extensive validation. Besides it requires previous knowledge of hydraulics and hydrodynamics. To overcome these difficulties, a water quality index (WQI) was developed. The water quality index (WQI) is a mathematical instrument used to transform large quantities of water quality data into a single number. The purpose of this research is to classify the upstream and downstream of the Klang main river based on WQI value.


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