Results 141 to 150 of about 70,104 (239)

Chapter 13 - The Peat fires of Italy.

open access: yes, 2012
A gather of technical images concerning the peat combustion phenomena in a selected italian area is offered as introduction to a new contribution on coal and peat fires in the whole Italy that will appear on the 4th volume of the the same collection ...
CREMONINI, STEFANO   +2 more
core   +1 more source

Tree stem methane emissions are regulated by site‐level biogeochemistry over species identity in Amazon floodplain forests

open access: yesNew Phytologist, Volume 251, Issue 1, Page 179-190, July 2026.
Summary Tree stems in Amazonian floodplains emit substantial methane (CH4), yet controls on emission variability remain unclear. Emissions span orders of magnitude between várzea (nutrient‐rich) and igapó (nutrient‐poor) forests and among trees, suggesting controls beyond flooding.
Holly R. Blincow   +9 more
wiley   +1 more source

Soil Organic Matter Reduces Persistent Nighttime Surface Warm Bias in Convection‐Permitting U.S. Simulations

open access: yesGeophysical Research Letters, Volume 53, Issue 11, 16 June 2026.
Abstract Convection‐permitting modeling has become a cornerstone for improving representation of land‐atmosphere processes, predicting weather extremes, and creating long‐term hydrometeorological data sets. The convection‐permitting Weather Research and Forecasting (WRF) modeling with the NoahMP land‐surface scheme is widely used for kilometer‐scale ...
Tzu‐Shun Lin   +7 more
wiley   +1 more source

Soil edaphic condition in peat affecting the growth peformance of sago palm [PDF]

open access: yes, 2014
Sago palms (Metroxylon spp.) planted on shallow and deep peat, adhering to" good agricultura. practice showed good growth performance at early stage of its development i.e. less than 4 years after planting (Fariza, 2008).
Yong, Roland Chiew Ming
core  

Detecting local surface motion of pas­tures on peat soils using laser scanning technology

open access: yes, 2021
Subsidence can be observed at various locations in the Netherlands. While it can be due to both shallow and deep subsurface processes, the shallow subsidence is mainly a result from compaction, oxidation and/or groundwater drainage.
Li, Ze (author)
core  

Catchment-based approach for water table management with irrigation for cultivated peatlands

open access: yesAgricultural Water Management
Controlled drainage and subsurface irrigation have been proposed to enable shallow-drained agriculture in organic soils and mitigate greenhouse gas (GHG) emissions from intensively cultivated peatlands.
Miika Läpikivi   +3 more
doaj   +1 more source

The effects of salinization on aerobic and anaerobic decomposition and mineralization in peat meadows: the roles of peat type and land use

open access: yes, 2014
Peat soils comprise a large part of the western and northern Netherlands. Drainage for agriculture has caused increased soil aeration which has stimulated decomposition and, hence, soil subsidence, currently amounting to 1-2 cm/yr.
Ecology and Biodiversity   +4 more
core   +1 more source

Subsidence of peat soils the tidal swamplands of Barambai, South Kalimantan

open access: yes, 2003
Large-scale reclamation of tropical peats in tidal swamplands areas for agriculture through the installation of irrigation-drainage system has been carried by the Department of Public Works since 1970.
M. Dradjad, Soeprapto Soekodarmodjo, M. Shodiq Hidayat, Mulyono Nitisapto
core   +2 more sources

Peran Gambut Terhadap Nitrogen Total Tanah Di Lahan Rawa [the Role of Peat on Total Nitrogen in the Wetland Soils] [PDF]

open access: yes, 2013
Peatland has important role in wetland ecosystem stability. Depletion and disappearance of peat layer lead to loss of potential source of nutrient and disruption of wetland ecosystem stability.
Fahmi, A. (Arifin)   +1 more
core  

Fractions of nitrogen in drained peat-muck soils located in the upper Liwiec River valley

open access: yes, 2009
Celem pracy było zbadanie właściwości trzech płytkich gleb torfowo-murszowych, zlokalizowanych w dolinie górnego biegu rzeki Liwiec, a także określenie zmian zawartości i udziału azotu glebowego w sekwencyjnie wydzielonych frakcjach tego pierwiastka.
Becher, M., Kalembasa, D.
core  

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