Matches in DBpedia 2014 for { <http://dbpedia.org/resource/Soil_compaction> ?p ?o. }
Showing items 1 to 27 of
27
with 100 items per page.
- Soil_compaction abstract "In geotechnical engineering, soil compaction is the process in which a stress applied to a soil causes densification as air is displaced from the pores between the soil grains. When stress is applied that causes densification due to water (or other liquid) being displaced from between the soil grains then consolidation, not compaction, has occurred. Normally, compaction is the result of heavy machinery compressing the soil, but it can also occur due to the passage of (e.g.) animal feet. In soil science and agronomy soil compaction is usually a combination of both engineering compaction and consolidation, so may occur due to a lack of water in the soil, the applied stress being internal suction due to water evaporation as well as due to passage of animal feet. Affected soils become less able to absorb rainfall, thus increasing runoff and erosion. Plants have difficulty in compacted soil because the mineral grains are pressed together, leaving little space for air and water, which are essential for root growth. Burrowing animals also find it a hostile environment, because the denser soil is more difficult to penetrate. The ability of a soil to recover from this type of compaction depends on climate, mineralogy and fauna. Soils with high shrink-swell capacity, such as vertisols, recover quickly from compaction where moisture conditions are variable (dry spells shrink the soil, causing it to crack). But clays which do not crack as they dry cannot recover from compaction on their own unless they host ground-dwelling animals such as earthworms — the Cecil soil series is an example.".
- Soil_compaction thumbnail CaseCrawlerWithTamper3658.JPG?width=300.
- Soil_compaction wikiPageExternalLink www.denichsoiltest.com.
- Soil_compaction wikiPageExternalLink Green_Infrastructure.html.
- Soil_compaction wikiPageExternalLink soil-compaction-%e2%80%93-not-conducive-to-root-growth.
- Soil_compaction wikiPageExternalLink online.php.
- Soil_compaction wikiPageID "4156794".
- Soil_compaction wikiPageRevisionID "606509942".
- Soil_compaction hasPhotoCollection Soil_compaction.
- Soil_compaction subject Category:Geotechnical_engineering.
- Soil_compaction subject Category:Soil_science.
- Soil_compaction comment "In geotechnical engineering, soil compaction is the process in which a stress applied to a soil causes densification as air is displaced from the pores between the soil grains. When stress is applied that causes densification due to water (or other liquid) being displaced from between the soil grains then consolidation, not compaction, has occurred. Normally, compaction is the result of heavy machinery compressing the soil, but it can also occur due to the passage of (e.g.) animal feet.".
- Soil_compaction label "Bodenverdichtung".
- Soil_compaction label "Compactage de sol".
- Soil_compaction label "Soil compaction".
- Soil_compaction label "Уплотнение грунтов".
- Soil_compaction label "رص التربة".
- Soil_compaction label "土壤压实".
- Soil_compaction sameAs Zhutňování_půd.
- Soil_compaction sameAs Bodenverdichtung.
- Soil_compaction sameAs Compactage_de_sol.
- Soil_compaction sameAs m.0bm5rc.
- Soil_compaction sameAs Q618290.
- Soil_compaction sameAs Q618290.
- Soil_compaction wasDerivedFrom Soil_compaction?oldid=606509942.
- Soil_compaction depiction CaseCrawlerWithTamper3658.JPG.
- Soil_compaction isPrimaryTopicOf Soil_compaction.
