The use of subsidence to estimate carbon loss from deforested and drained tropical peatlands in Indonesia
Drainage is a major means of the conversion of tropical peat forests into agriculture.
Accordingly, drained peat becomes a large source of carbon. However, the amount of …
Accordingly, drained peat becomes a large source of carbon. However, the amount of …
The role of compaction on pyhsicochemical properties and carbon emissions of tropical peat soils: a review
The peat compaction method is currently adopted by Malaysia oil palm companies to
mitigate the uprising environmental issues. This method is claimed to be effective in …
mitigate the uprising environmental issues. This method is claimed to be effective in …
[HTML][HTML] Drying kinetics of Indonesian peat
Indonesia has the largest peatland area in the tropical region, situated mainly in Sumatra,
Kalimantan and Papua. Peat is an organic substance which is highly combustible in dry …
Kalimantan and Papua. Peat is an organic substance which is highly combustible in dry …
Physical and hydrological properties of peat as proxies for degradation of South African peatlands: Implications for conservation and restoration
M Gabriel, C Toader, F Faul, N Rosskopf, PL Grundling… - 2018 - publishup.uni-potsdam.de
The physical and hydrological properties of peat from seven peatlands in northern
Maputaland (South Africa) were investigated and related to the degradation processes of …
Maputaland (South Africa) were investigated and related to the degradation processes of …
[PDF][PDF] Relationship between Groundwater Level and Water Content in Oil Palm Plantation on Drained Peatland in Siak, Riau Province, Indonesia.
YA Adhi, S Anwar, SD Tarigan… - Pertanika Journal of …, 2020 - pertanika.upm.edu.my
The decrease in groundwater level (GWL) on peatlands, especially in the dry season, can
lead to extensive peat drying and making it more vulnerable to the occurrence of wildfire …
lead to extensive peat drying and making it more vulnerable to the occurrence of wildfire …
Increases in greenhouse gases following the use of peatlands for agricultural areas
Peatlands with very high C contents are generally considered a source of greenhouse gas
(GHG) emissions. This research aimed to quantify the changes in peatland characteristics …
(GHG) emissions. This research aimed to quantify the changes in peatland characteristics …
[PDF][PDF] Determination of cation exchange capacity and analysis of cation availability in hemic and sapric peat with different preparation and extraction methods
MA Siregar, A Ma'as, M Nurudin - Ilmu Pertanian (Agricultural …, 2021 - academia.edu
The use of mineral soil analysis procedures in peat soils is considered unsuitable. Peat soil
is vulnerable to disturbance, which leads to the damage of peat inert structure, such as the …
is vulnerable to disturbance, which leads to the damage of peat inert structure, such as the …
Pengaruh fluktuasi muka air tanah terhadap pelepah bawah mengering (low frond desiccation) kelapa sawit di lahan gambut Labuhan Batu, Sumatera Utara
R FARRASATI, A Susanto - Jurnal Penelitian …, 2020 - jurnalkelapasawit.iopri.org
Low frond desiccation (LFD) on oil palm plantation has been a major issue, which often
occurs on peatland. LFD is generally associated with a fluctuation of peatland water table …
occurs on peatland. LFD is generally associated with a fluctuation of peatland water table …
Subsiden, Emisi Karbon Dan Fisik Tanah Gambut Terbakar Dan Tidak Terbakar Di Areal Konservasi Gambut
M Nuriman - Jurnal Solum, 2024 - jurnalsolum.faperta.unand.ac.id
Today, peatland fires cause peat soil changes and release carbon emissions. The area
protected as a peat conservation area in 2019 was not spared from fire incidents, where the …
protected as a peat conservation area in 2019 was not spared from fire incidents, where the …
A critical contribution on understanding the mechanism and implication of peat irreversible drying
IK Wardani, B Sumawinata - IOP Conference Series: Earth and …, 2019 - iopscience.iop.org
The term irreversible drying is known as a condition when peat soil material is dry and
cannot be re-wet after an intensive drying. This condition is a result of peat soil …
cannot be re-wet after an intensive drying. This condition is a result of peat soil …