Results 71 to 80 of about 5,233 (246)
The composition of soil organic matter is considered to have a key influence on C sequestration and global climate change and can be associated with changes in vegetation cover in the terrestrial ecosystem.
Saven Thai +6 more
doaj +1 more source
ABSTRACT Deciphering the time milestones of clay formation is crucial for modeling the evolution of major geological systems near the Earth's surface. In the present study, kaolinite samples collected along four vertical profiles within a Gleysol‐Ferralsol‐Podzol soil toposequence near São Gabriel da Cachoeira, NW Amazon Basin (Brazil) are dated using ...
Célia Regina Montes +8 more
wiley +1 more source
Pedodiversity‐Based Covariates for Digital Soil Mapping Framework
ABSTRACT The integration of soil diversity as a covariate in digital soil mapping framework remains largely unexploited. However, we believe that it may carry important information that can be used to create more accurate digital maps of soil properties.
Radim Vašát +3 more
wiley +1 more source
Peatlands are vast carbon reservoirs, yet the processes that suppress plant‐matter decomposition and that can switch to carbon release under disturbance remain contested. One explanation is the Enzyme‐latch hypothesis, which proposes that enzymatic constraints ‘lock’ decomposition until peatlands are damaged.
Eleanor K. M. Birch, Nicholle G. A. Bell
wiley +1 more source
Vegetation strongly influences soil formation, yet its effect on Rare Earth Element (REE) distribution and fractionation across treeline ecotones remains insufficiently constrained.
Veneramaria Urso +5 more
doaj +1 more source
ABSTRACT Aim For improved predictions of the redistribution of species under climate change, there is a need to better understand how interactions among multiple abiotic drivers affect species distributions. We examined whether occupancy patterns of forest plant species change consistently along geographic and macroclimatic gradients. We further tested
Per‐Ola Hedwall +6 more
wiley +1 more source
Генезис и почвообразуване при Подзолите и Кафявите планинско- горски почви в Евразия
Brown Mountain Forest Soils are degraded Mountain Meadow Soils as a result of established bush and forest vegetation after glacial. Podzols were formed under influence of acid products forest litter (bedspread) over the mineral layer, supported or not ...
ГЕОРГИ АНТОНОВ
doaj
Free acid in Minnesota podzols
Copyright by the Ecological Society of AmericaGorham, E.. (1958). Free acid in Minnesota podzols.
Gorham, E.
core
Smectites from the E horizon of podzols dated at 1200–10,000 y in central and northern Finland were studied. Clay minerals in the fine (<0.1 μm) and coarse (0.1–2 μm) fractions were examined by X-ray diffraction.
D. Righi, F. Gillot, M. L. Räisänen
core +1 more source
Some podzols on Bateke sands and their origins, People's Republic of Congo
L'étude des podzols du pays Batéké (Congo) montre que leur genèse est liée à une histoire complexe en rapport avec les changements climatiques quaternaires.
Schwartz, Dominique
core +1 more source

