Zobrazeno 1 - 10
of 107
pro vyhledávání: '"clay-illuvial soils"'
Autor:
Świtoniak, Marcin1 swit@umk.pl
Publikováno v:
Soil Science Annual. 2023, Vol. 74 Issue 4, p1-14. 14p.
Autor:
Kabała, Cezary1 cezary.kabala@upwr.edu.pl
Publikováno v:
Soil Science Annual. 2023, Vol. 74 Issue 4, p1-16. 16p.
Autor:
Świtoniak, Marcin1 swit@umk.pl
Publikováno v:
Soil Science Annual. 2021, Vol. 72 Issue 4, p1-8. 8p.
Autor:
Kabała Cezary, Musztyfaga Elżbieta
Publikováno v:
Soil Science Annual, Vol 66, Iss 4, Pp 204-213 (2015)
Soil with a clay-illuvial subsurface horizon are the most widespread soil type in Poland and significantly differ in morphology and properties developed under variable environmental conditions. Despite the long history of investigations, the rules of
Externí odkaz:
https://doaj.org/article/11cf46ce5db14257a76c8ce65531c3ac
Autor:
Marcin Świtoniak
Publikováno v:
Soil Science Annual. 72:1-8
Autor:
Cezary Kabała, Elżbieta Musztyfaga
Publikováno v:
Soil Science Annual, Vol 66, Iss 4, Pp 204-213 (2015)
Soil with a clay-illuvial subsurface horizon are the most widespread soil type in Poland and significantly differ in morphology and properties developed under variable environmental conditions. Despite the long history of investigations, the rules of
Autor:
Radziuk, Hanna1 anka.radziuk@gmail.com, Świtoniak, Marcin1
Publikováno v:
Soil Science Annual. 2021, Vol. 72 Issue 1, p1-8. 8p.
Autor:
Pindral Sylwia, Świtoniak Marcin
Publikováno v:
Soil Science Annual, Vol 68, Iss 1, Pp 2-10 (2017)
Soil erosion led to the severe transformations of the soil cover of young morainic areas of northern Poland. Main alterations are connected with soil truncation on summits and in upper part of slopes, whereas at foot slopes and within depressions col
Externí odkaz:
https://doaj.org/article/34eb7a9407a449f6a67dbbd2a3597a3a
Autor:
Bryk, Maja1 maja.bryk@up.lublin.pl
Publikováno v:
Soil Science Annual. 2023, Vol. 74 Issue 4, p1-17. 17p.
Autor:
Sylwia Pindral, Marcin Świtoniak
Publikováno v:
Soil Science Annual, Vol 68, Iss 1, Pp 2-10 (2017)
Soil erosion led to the severe transformations of the soil cover of young morainic areas of northern Poland. Main alterations are connected with soil truncation on summits and in upper part of slopes, whereas at foot slopes and within depressions col