Results 31 to 40 of about 4,076 (217)
Quaestiones GeographicaeSoil formation in polar regions is relatively weakly recognised due to their rarity and spatial dispersion. The main pedological, sedimentological and cryogenic features of the ice-free coasts of Admiralty Bay were described and quantified with an ...
Zieliński Artur +3 more
doaj +1 more source
Rates of soil-forming processes in three main models of pedogenesis 283 Rates of soil-forming processes in three main models of pedogenesis [PDF]
, 2020 Rates of soil-forming processes were evaluated for the three major models of pedogenesis: (1) normal "top-down" soil development (pedogenesis transforms the parent material under a geomorphically stable surface), (2) soil development ...
Alexander L Alexandrovskiy
core
Journal of Plant Nutrition and Soil Science, EarlyView.We provide a historic overview of microscopic soil structure characterization from its founding father, Walter Kubiëna, to several technical revolutions like automation, digitalization, and artificial intelligence. In addition to technical advancements, we explore how concepts and research questions have evolved in time.
Steffen Schlüter +3 more
wiley +1 more source
Reconstructing the Last 71 ka Paleoclimate in Northeast China by Integrating Typical Loess Sections
QuaternaryLong-term continuous deposits and well-preserved thick loess sections are natural archives for the reconstruction of global climate change. However, the loess sections are often discontinuous owing to soil erosions and accumulations.
Juan Li +7 more
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Land Degradation &Development, EarlyView.ABSTRACT Ensuring the long‐term erosional stability of post‐mining landforms remains a major challenge in open‐pit mining. Reconstructed landscapes must support the agreed post‐mining land use, such as cattle grazing in the Hunter region of southeastern Australia, requiring stable pasture and minimal soil loss.
I. P. Senanayake, G. R. Hancock
wiley +1 more source
Rapid loss of phosphorus during early pedogenesis along a glacier retreat choronosequence, Gongga Mountain (SW China) [PDF]
, 2015 The loss of phosphorus (P) during the early pedogenesis stage is important at the ecosystem level, and it also plays an important role in the global P cycle.
Jun Zhou +4 more
core +1 more source
Palaeowinds and depositional conditions from Holocene loess in Sweden and Finland
Boreas, EarlyView.The nature of deglacial and Holocene wind regimes in Fennoscandia is debated, as is the degree to which wind‐blown loess deposits exist in the region. Loess deposits in Fennoscandia are often relatively thin, discontinuous and less well‐sorted than typical loess, and questions remain over the degree of their post‐depositional reworking and the impact ...
Calum J. Edward +6 more
wiley +1 more source
, 2006 : The formation of soils from gyttja takes place under aeration, due to artificial drainage. In northern Europe gyttja deposits are found in northern Germany, Poland, Finland and Sweden. Their investigations date back to the middle of the last century.
Zeitz, Jutta, Chmieleski, Jana
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Boreas, EarlyView.Palynological records are central to the biostratigraphic subdivision of the Late Pleistocene in central Europe. Yet many interglacial and interstadial phases—such as the Eemian, Brörup and Odderade—remain only poorly constrained in time due to limited numerical dating.
Michael Hein +19 more
wiley +1 more source
AgricultureSoil chronosequences are crucial for understanding pedogenesis and ecosystem dynamics, yet a systematic bibliometric analysis of this field remains absent.
Jingtao Wu +5 more
doaj +1 more source