Often, soils from cold regions, such as Arctic soils, show polygonal forms in their surface. These polygons are formed because of the freeze-thaw cycle, characteristic of permafrost. What is permafrost? Permafrost is a subsurface soil layer which stays permanently frozen (below 0 oC) during long periods of time, usually more than two consecutive years. Most extensive permafrost areas can be found ...[Read More]
Cracked soils
Vertisols are dark clayey soils that show cracks at least during some part of the year. Normally, Vertisols are found in depressions or plain areas under subhumid or semiarid climate, with a wet and a dry season. Although climax vegetation is savanna, grassland or woodland, Vertisols are very fertile, so that agricultural use is very common. However, the process of swelling/shrinking makes Vertiso ...[Read More]
Forest residue mulching reduces post-fire soil erosion
Sergio A. Prats University of Aveiro, Portugal Still under the effect of the last wave of wildfires of summer 2013, Porto Canal interviewed the last Ph.D. student of the CESAM Research Centre at the University of Aveiro, who deals with soil erosion mitigation after wildfires. Porto Canal wanted to disseminate the last advances in recognizing the main effects of wildfires, the selection of soil ero ...[Read More]
Ladies and gentlemen: the Rolling Stones
Racetrack Playa is a plain without vegetation of a dry located above the northwestern side of Death Valley, in Death Valley National Park, Inyo County, CA, USA (click here to see in Google Maps). Although “playa” is the Spanish word for beach, it is also used in English to refer to a dry lake. Racetrack Playa occupies an area of 4.5 km (north-south) by 2 km (east-west) which is 1,130 m ...[Read More]