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Topography constrains the climatic response of treeline migration in Taiwan's subalpine forests
Ecography, EarlyView.Treelines are moving upslope, but the rates and drivers differ among different regions, globally. Many studies have examined the relationship between treeline movement and climate change, particularly rising temperature, while the role of topographical factors has received much less attention, despite the longstanding recognition of its importance.
Kuan‐Yu Chen +3 more
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Engineering properties and microscopic mechanism of phosphogypsum-rubber composite cemented soil. [PDF]
Sci RepMa Q, Li Y, Shu H, Song Z, Wu J.
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Solidification Performance and Mechanism of TSC Composite Soil Based on Microbially Induced Mineralization. [PDF]
Materials (Basel)Ding H, Zhan Q, Hu H, Xiong Y.
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Non-destructive assessment of lime and nano-alumina oxide stabilized clay for new material development. [PDF]
Sci RepFahimi R +4 more
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Effect of Soluble Glass Alkali Activation on the Geotechnical Performance of Sandy-Pebble Soil Stabilized with Biomass Bottom Ash. [PDF]
Materials (Basel)Vaičiukynienė D +2 more
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Shear strength characteristics of muddy interlayers with different water contents and particle size distributions. [PDF]
PLoS OneZha Z +7 more
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Soil compaction and soil management – a review
Soil Use and Management, 2009Abstract Soil compaction is an important component of the land degradation syndrome which is an issue for soil management throughout the world. It is a long standing phenomenon not only associated with agriculture but also with forest harvesting, amenity land use, pipeline installation, land restoration and wildlife trampling.
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Journal of the Institution of Civil Engineers, 1949
Synopsis. Soil compaction is the process whereby soil is mechanically compressed through a reduction in the air voids. It is measured in terms of the dry density or amount of solid matter in unit volume. Soils range in dry density from about 140 lb. per cubic foot for coarse-grained gravels and sands to about 90 lb.
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Synopsis. Soil compaction is the process whereby soil is mechanically compressed through a reduction in the air voids. It is measured in terms of the dry density or amount of solid matter in unit volume. Soils range in dry density from about 140 lb. per cubic foot for coarse-grained gravels and sands to about 90 lb.
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2022
When unsaturated soils are subjected to drained or undrained compression tests, they approach the saturated compression line with different slopes. This difference in slopes is produced by the amount of collapse of each path. During compression, four main phenomena occur in these materials: first, with the reduction in volume, the degree of ...
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When unsaturated soils are subjected to drained or undrained compression tests, they approach the saturated compression line with different slopes. This difference in slopes is produced by the amount of collapse of each path. During compression, four main phenomena occur in these materials: first, with the reduction in volume, the degree of ...
openaire +1 more source