Abstract

This study aims to determine soil physical properties and palm oil productivity in different of water levels (TMA) in peatland. This study conducted in palm oil plantation area in PT. Tabung Haji Indo Plantation Indragiri Hilir Regency, and Laboratory of Soil Science Faculty of Agriculture, University of Riau. This study was carried out started from July until October 2017 by using survey method. Sampling Location conducted by purposive sampling, and sampling point was determined by stratified random sampling. Analysed data used analyse of variance, followed by further test by Duncan’s new multiple range test level of 5%. Parameters observed in physical properties ware bulk density, porosity, water content of maximum occupied capacity, particles size distribution, and palm oil productivity. The result of this study showed that peatland with water levels (20-40) cm (TMA1) showed higher water content of maximum occupied capacity than water levels (>40-60) cm (TMA2), and >60 cm (TMA3). Peat soil with water level TMA2 owned bulk density, the particle size (≤63 µm) higher compared to TMA1 and TMA3. Peat soil with TMA3 showed higher porosity compared to TMA1 and TMA2. Peat soil TMA1 showed higher palm oil productivity compared to TMA2 and TMA3. Palm oil productivity TMA2 and TMA3 showed lower compared to TMA1 is caused by Ganoderma attack.

Highlights

  • Perkebunan kelapa sawit pada lahan gambut memerlukan sistem drainase sebagai pengatur kedalaman muka air tanah

  • This study aims to determine soil physical properties and oil palm productivity in different of water levels (TMA) in peatland

  • The result of this study showed that peatland with water levels (20-40) cm (TMA1) showed higher water content of maximum occupied capacity than water levels (>40-60) cm (TMA2), and >60 cm (TMA3)

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Summary

HASIL DAN PEMBAHASAN

Penelitian ini dilakukan di lahan gambut pada tanaman kelapa sawit PT. Tabung Haji Indo Plantation Tabel 1 menunjukkan bahwa tanah gambut pada kedalaman muka air tanah (20-40) cm dapat meningkatkan kadar air kapasitas lapang maksimum secara nyata. Tabel 2 menunjukkan pada lahan gambut dengan kedalaman muka air tanah (>40-60) cm memiliki nilai bulk density tertinggi dibandingkan dengan dua ketinggian air diatas. Tabel 3 menunjukkan bahwa tanah gambut pada kedalaman muka air tanah berbeda berpengaruh terhadap nilai porositas. Peningkatan porositas pada tinggi muka air tanah gambut >60 cm, dikarenakan bobot isi yang rendah dampak dari bahan organik yang banyak belum terdekomposisi sehingga menyebabkan porositas yang tinggi dengan proporsi poripori besar yang tinggi (Driessen, 1978). Belum terdekomposisinya bahan dapat dilihat bahwa pada ketinggian muka air >60 memiliki bulk density (Tabel 2) terendah dibandingkan dengan ketinggian muka air tanah gambut yang lain.

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