Past, present & future of information technology in pedometrics
DG Rossiter - Geoderma, 2018 - Elsevier
Although pedometric approaches were taken as early as 1925, the post-WWII development
of information technology radically transformed the possibilities for applying mathematical …
of information technology radically transformed the possibilities for applying mathematical …
On the role of hydrologic processes in soil and landscape evolution modeling: concepts, complications and partial solutions
The ability of water to transport and transform soil materials is one of the main drivers of soil
and landscape development. In turn, soil and landscape properties determine how water is …
and landscape development. In turn, soil and landscape properties determine how water is …
[HTML][HTML] Reviews and syntheses: Agropedogenesis–humankind as the sixth soil-forming factor and attractors of agricultural soil degradation
Y Kuzyakov, K Zamanian - Biogeosciences, 2019 - bg.copernicus.org
Abstract Agricultural land covers 5.1× 10 9 ha (ca. 50% of potentially suitable land area),
and agriculture has immense effects on soil formation and degradation. Although we have …
and agriculture has immense effects on soil formation and degradation. Although we have …
The trajectory of soil development and its relationship to soil carbon dynamics
It has been postulated that the amount of soil organic carbon (SOC) associated with soil
minerals exhibits a threshold relationship in response to effective soil moisture (estimated as …
minerals exhibits a threshold relationship in response to effective soil moisture (estimated as …
[HTML][HTML] The current and future role of biota in soil-landscape evolution models
X Meng, AM Kooijman, AJAM Temme… - Earth-Science …, 2022 - Elsevier
Biota are major drivers of geomorphological development. Vegetation and soil fauna act as
ecosystem engineers, changing the environment through physical structures and individual …
ecosystem engineers, changing the environment through physical structures and individual …
Calibrating SoilGen2 for interglacial soil evolution in the Chinese Loess Plateau considering soil parameters and the effect of dust addition rhythm
To better understand interglacial paleosol development by quantifying the paleosol
development processes on the Chinese Loess Plateau (CLP), we need a soil genesis model …
development processes on the Chinese Loess Plateau (CLP), we need a soil genesis model …
[HTML][HTML] Modeling soil and landscape evolution–the effect of rainfall and land-use change on soil and landscape patterns
Humans have substantially altered soil and landscape patterns and properties due to
agricultural use, with severe impacts on biodiversity, carbon sequestration and food security …
agricultural use, with severe impacts on biodiversity, carbon sequestration and food security …
Simulating soil organic carbon stock as affected by land use and climate change on volcanic soils in Indonesia
S Anindita, S Sleutel, P Finke - Geoderma Regional, 2023 - Elsevier
We assessed long-term trends in soil organic carbon (SOC) in volcanic soils with a process-
based soil genesis model, SoilGen2. 25. The relation between soil geochemistry and SOC …
based soil genesis model, SoilGen2. 25. The relation between soil geochemistry and SOC …
Including stable carbon isotopes to evaluate the dynamics of soil carbon in the land‐surface model ORCHIDEE
M Camino‐Serrano, M Tifafi, J Balesdent… - Journal of Advances …, 2019 - Wiley Online Library
Soil organic carbon (SOC) is a crucial component of the terrestrial carbon cycle and its
turnover time in models is a key source of uncertainty. Studies have highlighted the utility of …
turnover time in models is a key source of uncertainty. Studies have highlighted the utility of …
Can SOC modelling be improved by accounting for pedogenesis?
Recent findings suggest that soil organic carbon mineralization and stabilization depend to
a substantial degree on the soil geochemistry and the degree of weathering. We …
a substantial degree on the soil geochemistry and the degree of weathering. We …