<i>Modeling Palouse hills to quantify moisture redistribution from the selective non-uniform application of biochar</i>

2020 ◽  
Keyword(s):  
Moisture Redistribution

Moisture Redistribution and Phase Transitions During Bread Staling

2000 ◽  
Vol 77 (4) ◽  
pp. 484-488 ◽  
Author(s):  
Moo-Yeol Baik ◽  
Pavinee Chinachoti
Keyword(s):  
Phase Transitions ◽  
Bread Staling ◽  
Moisture Redistribution

Soil moisture redistribution and infiltration in frozen sandy soils

1999 ◽  
Vol 35 (1) ◽  
pp. 95-103 ◽  
Author(s):  
Manfred Stähli ◽  
Per-Erik Jansson ◽  
Lars-Christer Lundin
Keyword(s):  
Soil Moisture ◽  
Sandy Soils ◽  
Moisture Redistribution

scholarly journals Soil moisture redistribution and its effect on inter-annual active layer temperature and thickness variations in a dry loess terrace in Adventdalen, Svalbard

2016 ◽  
Author(s):  
C. Schuh ◽  
A. Frampton ◽  
H. H. Christiansen
Keyword(s):  
Soil Moisture ◽  
Layer Thickness ◽  
Active Layer ◽  
Field Data ◽  
Large Field ◽  
Thickness Variation ◽  
Unfrozen Water ◽  
Active Layer Thickness ◽  
Retention Characteristics ◽  
Moisture Redistribution

Abstract. High resolution field data for the period 2000–2014 consisting of active layer and permafrost temperature, active layer soil moisture, and thaw depth progression from the UNISCALM research site in Adventdalen, Svalbard, is combined with a physically-based coupled cryotic and hydrogeological model to investigate active layer dynamics. The site is a loess-covered river terrace characterized by dry conditions with little to no summer infiltration and an unsaturated active layer. A range of soil moisture characteristic curves consistent with loess sediments are considered and their effects on ice and moisture redistribution, heat flux, energy storage through latent heat transfer, and active layer thickness is investigated and quantified based on hydro-climatic site conditions. Results show that soil moisture retention characteristics exhibit notable control of ice distribution and circulation within the active layer by cryosuction subject to seasonal variability and site-specific surface temperature variations. The retention characteristics also impact unfrozen water and ice content in the permafrost. Although these effects lead to differences in thaw progression rates, the resulting inter-annual variability in active layer thickness is not large. Field data analysis reveals that variations in summer degree days do not notably affect the active layer thaw depths; instead, a cumulative winter degree day index is found to more significantly control inter-annual active layer thickness variation at this site. A tendency of increasing winter temperatures is found to cause a general warming of the subsurface down to 10 m depth (0.05 to 0.26 ˚C/yr, observed and modelled) including an increasing active layer thickness (0.8 cm/yr, observed and 0.3 to 0.8 cm/yr, modelled) during the 14-year study period.

Moisture Redistribution Mechanisms in Granular Mineral Fertilizers During Their Storage and Transportation

2020 ◽  
Author(s):  
Valeriy Sokolov ◽  
Natalia Nikolaeva ◽  
Irina Pochitalkina ◽  
Inna Kochetova
Keyword(s):  
Mineral Fertilizers ◽  
Moisture Redistribution

Soil moisture redistribution as a mechanism of facilitation in savanna tree–shrub clusters

Oecologia ◽  
2005 ◽  
Vol 145 (1) ◽  
pp. 32-40 ◽  
Author(s):  
C. B. Zou ◽  
P. W. Barnes ◽  
S. Archer ◽  
C. R. McMurtry
Keyword(s):  
Soil Moisture ◽  
Moisture Redistribution
Sign in / Sign up

Export Citation Format

Share Document