The paper presents floral and soil diversity of selected soils of ecological grasslands in the Bystra Notec Valley. The state of
vegetation cover was described on the basis of floral composition and such soil properties as the: content of organic matter,
specific density, soil density, total porosity, maximal hygroscopic capacity, soil potential of water bonds, total and readily
available water and reaction were analysed. The analysed soils showed high diversity in the scope of the examined properties.
They resulted mostly from the content and state of transformation of organic matter. Meadow grasslands were diversified
in terms of flora and natural qualities. They were dominated by species characteristic to Phragmitetea class. The highest
floral diversity was observed on grasslands from Phalaridetum arundinaceae group H’=3,1of medium natural qualities.
It depended mostly on current habitat and agricultural use.
REFERENCES(31)
1.
Berglund Ö, Berglund K.: Influence of water table level and soil properties on emission of greenhouse gases from cultivated peat soil. Soil Biology and Biochemistry, 2011, 43, 923-931.
Bieniek A. Łachacz A.: Ewolucja gleb murszowych w krajobrazie sandrowym. „Wybrane problemy ochrony mokradeł”. Współczesne problemy Kształtowania i Ochrony Środowiska, 2012, 11-131.
Grzelak M., Gaweł E., Janyszek M., Diatta J.B., Gajewski P.: The effect of biotope and land use on floristic variation, nature and economic value of marsh sedge rushes. Journal of Food, Agriculture & Environment, 2014, Vol. 12 (2 ), 1201-1204.
Grzelak M., Kaczmarek., Gajewski P.: Zróżnicowanie glebowe i florystyczne ekologicznych zbiorowisk łąkowych na glebach organicznych. Journal of Research and Applications in Agricultural Engineering, 2012, Vol. 57 (3), 142-146.
Grzelak M., Kaczmarek., Gajewski P.: Kształtowanie się szuwaru trzcinowego Phragmitetum australis (Gams 1927) Schmale 1939 w warunkach gleby torfowo-murszowej. Journal of Research and Applications in Agricultural Engineering, 2013, Vol. 58 (3), 178-183.
Jaros H.: Zróżnicowanie właściwości fizycznych gleb hydrogenicznych Narwiańskiego Parku Narodowego w aspekcie ich ochrony. Acta Agrophys., 2003, 89, 1(4), 631-639.
Kaczmarek Z., Grzelak M., Gajewski P.: Warunki siedliskowe oraz różnorodność florystyczna ekologicznych siedlisk przyrodniczych w Dolinie Noteci. Journal of Research and Applications in Agricultural Engineering, 2010, Vol. 55 (3), 142-147.
Kalisz B., Łachacz A., Glazewski R.: Effect of peat drainage on labile organic carbon and water repellency in NE Poland. Turk. J. Agric For., 2015, 39, 20-27.
Klute A.: Water retention: Laboratory Methods In: Klute A. (Ed.). Methods of soil analysis, Part 1: Physical and mineralogical methods. 2nd ed. Agronomy Monographs 9 ASA and SSSA, Madison, Wi, USA, 1986, 635-662.
Lichner L., Holko L.Zhukova N., Schacht K., Rajkai K., Fodor N, Sandor R. Plants and biological soil crusts influence hydrophysical parameters and water flow in an aeolian sandy soil. J. Hydrol. Hydromech, 2012, 60, 309-318.
Okruszko H.: Okreslenie ciężaru właściwego gleb hydrogenicznych na podstawie zawartości w nich części mineralnych. Wiad. Inst. Melior. Użyt. Ziel., 1971, 10,1: 47-54.
Rząsa S., Owczarzak W., Mocek A.: Problemy odwodnieniowej degradacji gleb uprawnych w rejonach kopalnictwa odkrywkowego na Niżu Środkowopolskim. Wyd. Akademii Rolniczej w Poznaniu, 1999.
We process personal data collected when visiting the website. The function of obtaining information about users and their behavior is carried out by voluntarily entered information in forms and saving cookies in end devices. Data, including cookies, are used to provide services, improve the user experience and to analyze the traffic in accordance with the Privacy policy. Data are also collected and processed by Google Analytics tool (more).
You can change cookies settings in your browser. Restricted use of cookies in the browser configuration may affect some functionalities of the website.