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Fengky Florante Adji
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STUDI KANDUNGAN C-ORGANIK, KADAR ABU, DAN BOBOT ISI GAMBUT PEDALAMAN DI KAWASAN HUTAN DENGAN TUJUAN KHUSUS (KHDTK) TUMBANG NUSA, KALIMANTAN TENGAH Nina Yulianti; Advenrikus A. Saleilei; Salampak Salampak; Fengky Florante Adji; Zafrullah Damanik; Giyanto Giyanto
Jurnal Ilmu Lingkungan Vol 16, No 1 (2022): Jurnal Ilmu Lingkungan
Publisher : Program Pascasarjana Universitas Riau

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31258/jil.16.1.p.58-65

Abstract

Peatlands is one of carbon stocks in ecosystem. Soil carbon is stored in the peat layer and and the above ground carbon is stored in vegetation. Central Kalimantan has large area of ombrogenic peatland in Indonesia. The aim of this research was; (1) Identify C-organic content, ash content, and bulk density in several peat land uses in KHDTK Tumbang Nusa, Central Kalimantan; (2) Identify the relationship between C-Organic with ash content and bulk density of peat soil. This research was conducted in July 2020 – December 2020. Sampling of peat soil took place in the Tumbang Nusa Special Purpose Forest Area (KHDTK). The analysis of the physical and chemical properties of the soil is located in the laboratory of the Department of Agronomy, Faculty of Agriculture, University of Palangka Raya, the Laboratory of the Research and Development Center for Environment and Forestry (BP2LHK) Banjar Baru, the University Integrated Laboratory. The research was conducted using a sampling method on each different land cover, namely natural forest, burnt areas, and revegetation. Each study site made 3 profiles, then soil samples were taken at a depth of 10 cm, 20 cm, 30 cm, and 40 cm. The results of the study show the conclusions of the results of this study, namely; (1) the largest of C content is 57.83% at secondary forest and the lowest of value of the C content is 54.24% the burnt land. The highest ash content is 9.01% at revegetation area and the lowest ash content is 0.31% at secondary forest land. The highest bulk density is 0.19 g cm-3  at revegetation area and the lowest bulk density is 0.12 g cm-3 at secondary forest. C organic has an inverse relationship with ash content. Further, the relationship between C-Organic and bulk density has a inverse relationship, too.
SIFAT FISIK GAMBUT PEDALAMAN PADA LABORATORIUM ALAM HUTAN GAMBUT SEBANGAU, KALIMANTAN TENGAH Yonodius Paskalis Bay; Nina Yulianti; Suparno Suparno; Fengky Florante Adji; Zafrullah Damanik; Sustiyah Sustiyah
Jurnal Ilmu Lingkungan Vol 15, No 2 (2021): Jurnal Ilmu Lingkungan
Publisher : Program Pascasarjana Universitas Riau

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31258/jil.15.2.p.216-233

Abstract

Indonesia has the largest peat area in the tropical zone, which estimated about 21 million ha, with a percentage of 70% of the peat area in Southeast Asia and 50% of the world's tropical peatlands. This study aims to evaluate the physical properties of soil in each layer of soil and land cover in inland peat swamp forests in LAHG in Central Kalimantan. The research used the profile method (minipit) measuring 120 cm x 120 cm. Each location is given 3 plots on 2 (two) land cover  namely forest and burnt area. The research location is in LAHG. This research was conducted in July-December 2020. Samples were analyzed at the Banjarbaru Research and Development Laboratory. The parameters observed were bulk density, moisture content, fiber content, soil color, infiltration, and hydraulic conductivity. The research data were analyzed statistically by means of regression and correlation analysis. The results showed that the study of the physical properties of inland peat soil in the forest had bulk density ranging from 0.10 to 0.15 g / cm-3, moisture content 541.18-910.00%, fiber content 8-40%, infiltration -0 , 58-29.27 ml / hour, hydraulic conductivity 2.4-66.6 cm / hour with reddish black soil color. Whereas on burnt land, bulk density ranged from 0.10 to 0.15 g / cm-3, moisture content was 500.00-916.67%, fiber content was 12-52%, infiltration was -3.19-60.99 ml. / hr, hydraulic conductivity 2.4-30.6 cm / hr with dark black soil color. The study relationship pattern shows positive and negative.