Search results
Results from the WOW.Com Content Network
Peat swamp forests occur where waterlogged soils prevent dead leaves and wood from fully decomposing, which over time creates thick layer of acidic peat.The peat swamp forests on Borneo occur in the Indonesian state of Kalimantan, the Malaysian state of Sarawak and in the Belait District of Brunei on coastal lowlands, built up behind the brackish mangrove forests and bounded by the Borneo ...
In Australia, net acidity is used in combination with the texture or clay content of the sample and the weight of acid sulfate soil to be disturbed (e.g., excavated for construction) to determine whether or not an Acid Sulfate Soil Management Plan (ASSMP) is required as part of statutory environmental management protocols.
As the peat thickens and the dome becomes elevated, the top of the peat is no longer affected by the river or groundwater input, instead they are becoming ombrotrophic, exclusively obtaining water from the precipitation [8] [10] Input only from the rain causes a low nutrient and mineral content, especially calcium. The peat thus becomes highly ...
Peat formation typically initiates as a paludification of a mineral soil forests, terrestrialisation of lakes, or primary peat formation on bare soils on previously glaciated areas. [3] A peatland that is actively forming peat is called a mire .
[11] [12] Soil degradation is a gradual process involving the natural and anthropogenic processes that result in the physical loss (erosion) and reduction in soil quality. [7] The recognition of anthropogenic effects on soil degradation has influenced discourse of urban soil management, and formulation of policies by regional organizations. [13]
Python library for the manipulation and storage of a wide range of geoscientific data (points, curve, surface, 2D and 3D grids) in geoh5 file format, natively supported by Geoscience ANALYST free 3D viewer Mira Geoscience Ltd. LPGL 3.0 Cross-platform: Python: Documentation and tutorials fully available in ReadTheDocs: geoapps repository [24]
The amount of carbon a soil can sequester depends on the climate and current and historical land-use and management. [6] Cropland has the potential to sequester 0.5–1.2 Pg C/year and grazing and pasture land could sequester 0.3–0.7 Pg C/year. [7] Agricultural practices that sequester carbon can help mitigate climate change. [8]
Tropical peat is a type of histosol that is found in tropical latitudes, including South East Asia, Africa, and Central and South America. [2] Tropical peat mostly consists of dead organic matter from trees instead of spaghnum which are commonly found in temperate peat. [ 3 ]