chernozemic


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cher·no·zem

 (chĕr′nə-zĕm′, chîr′nə-zyôm′)
n.
A very black topsoil, rich in humus, typical of cool to temperate semiarid regions such as the grasslands of Ukraine and southern Russia.

[Russian chernozëm : chërnyĭ, black + Old Russian zemĭ, earth; see dhghem- in Indo-European roots.]

cher′no·zem′ic adj.

chernozemic

(ˌtʃɜːnəʊˈzɛmɪk)
adj
of or relating to a chernozem
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References in periodicals archive ?
Shukla MK, Slater BK, Lal R, Cepuder P (2004) Spatial variability of soil properties and potential management classification of a chernozemic field in Lower Austria.
2) Chernozemic, typically occurring in the cool, subarid to subhumid climates of central Canada;
Schmidt MWI, Skjemstad JO, Gehrt E, Kogel-Knabner I (1999) Charred organic carbon in German chernozemic soils.
The assumption that Alberta matched Saskatchewan's suitability to wheat was reinforced by the rich chernozemic soils between Calgary and Edmonton which were the first to be opened to agricultural settlement.
Role of continuous wheat and amendments in ameliorating an artificially eroded dark brown chernozemic soil under dryland conditions.