A sapric is a subtype of a histosol[1] where virtually all of the organic material has undergone sufficient decomposition to prevent the identification of plant parts and even fecal matter.[2][3]Muck is a sapric soil that is naturally waterlogged or is artificially drained.
The World Reference Base for Soil Resources (WRB) defines "sapric" (sa) as a histosol having less than one-sixth (by volume) of the organic material consisting of recognizable plant tissue within 100 cm of the soil surface.[4]
Canada
Muck soils fall under the Organic Order in the Canadian system of soil classification.[5] Muck soils are organic soils, with at minimum of 30% organic matter and a depth of at least 40 cm.[5]
United States
In the USDA soil taxonomy, sapric may be a subtype of a haplohemist or glacistel type, and may also be a diagnostic organic soil material where the fiber content is less than one-sixth of the volume.[2] Muck soils are defined by the USDA NRCS as sapric organic soils that are saturated more than 30 cumulative days in normal years or are artificially drained.[6] An example would be a soil made up primarily of humus from drained swampland.[citation needed]
Muck farming is controversial because the drainage of wetlands destroys wildlife habitats and results in a variety of environmental problems. It is unlikely that any more will be created in the United States because of environmental regulations. It is prone to problems. The soil is very light, so windbreaks are necessary to protect these fields in dry weather. It also can catch fire and burn underground for months. Oxidation also removes a portion of the soil each year, making it progressively shallower. Oxidation also discharges carbon dioxide. Some muck land has been reclaimed and restored as wetlands for wildlife preserves.[citation needed]
The impacts of drainage and agricultural production cause the loss of organic matter in muck soils through erosion, oxidation, and other processes collectively called "subsidence." Agricultural practices such as cover cropping and reduced tillage can significantly reduce subsidence but can not reverse it. Muck soils are, in essence, a non-renewable agricultural resource.[8]
Etymology
The word muck has much usage in the English language, referring in some cases to agricultural soil, and in others to dirt in general, and animal dung (sometimes human feces) in particular. Origins are probably from Norse, Danish, and Proto-Germanic roots referring to cow dung.[9][10]
^ abCanada Soil Survey Committee, Subcommittee on soil classification (1978). "The Canadian system of soil classification". Can. Dep. Agric. Publ. 1646. Supply and Services Canada (Pb), Ottawa, Ontario. 83pp.