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<dc:title xml:lang="en"><![CDATA[Forest reclamation of the postmining dumps. I. Changes in the properties of miocene sediments material = Rekultywacja leśna hałd pokopalnianych. I. Zmiana właściwości gruntu zwałowego pochodzenia mioceńskiego]]></dc:title>
<dc:title xml:lang="pl"><![CDATA[Forest reclamation of the postmining dumps. I. Changes in the properties of miocene sediments material = Rekultywacja leśna hałd pokopalnianych. I. Zmiana właściwości gruntu zwałowego pochodzenia mioceńskiego]]></dc:title>
<dc:creator><![CDATA[Drab, Michał]]></dc:creator>
<dc:creator><![CDATA[Greinert, Henryk]]></dc:creator>
<dc:subject xml:lang="en"><![CDATA[4 Międzynarodowa konferencja "Ochrona i rekultywacja terenów dorzecza Odry: rekultywacja terenów zdegradowanych" (28-29.06.2007)]]></dc:subject>
<dc:subject xml:lang="en"><![CDATA[miocene sediments]]></dc:subject>
<dc:subject xml:lang="en"><![CDATA[dumps reclamation]]></dc:subject>
<dc:subject xml:lang="en"><![CDATA[forest reclamation]]></dc:subject>
<dc:subject xml:lang="en"><![CDATA[anthropogenic soils]]></dc:subject>
<dc:subject xml:lang="pl"><![CDATA[4 Międzynarodowa konferencja "Ochrona i rekultywacja terenów dorzecza Odry: rekultywacja terenów zdegradowanych" (28-29.06.2007)]]></dc:subject>
<dc:subject xml:lang="pl"><![CDATA[miocene sediments]]></dc:subject>
<dc:subject xml:lang="pl"><![CDATA[dumps reclamation]]></dc:subject>
<dc:subject xml:lang="pl"><![CDATA[forest reclamation]]></dc:subject>
<dc:subject xml:lang="pl"><![CDATA[anthropogenic soils]]></dc:subject>
<dc:description xml:lang="en"><![CDATA[Miocene sediments, collected during brown coal excavation, have generally mechanical composition of loamy sand. The most negative feature of them is a very low pH-value, in a consequence of pyrite-oxidation. 20 years after technical reclamation and dump areas afforestation, a few conclusions about effects of the reclamation have been drawn:]]></dc:description>
<dc:description xml:lang="en"><![CDATA[1). The soil material in layer from 1 to 2 m deep is not homogenous. The layer from 0 to 20 cm is more homogenous as the result of mechanical cultivation before the sowing]]></dc:description>
<dc:description xml:lang="en"><![CDATA[2). After the slopes leveling intensive erosion processes have been occurred. About 25% of the total area has been damaged by water erosion. This effect should be connected with the absence of plant-cover]]></dc:description>
<dc:description xml:lang="en"><![CDATA[3). Soil-formation is related to anthropogenic activity, especially intensive liming, mineral fertilizing and afforestation. The influence of afforestation on soil is yet not very high. Clearly visible is a thin duff-layer (A0) ? about 1 cm]]></dc:description>
<dc:description xml:lang="en"><![CDATA[4). Nevertheless the heavy machines using during leveling, physical and water properties of the soils are quite good]]></dc:description>
<dc:description xml:lang="en"><![CDATA[5). The high lime doses causing rising the pH of top-soil-material (20-30 cm deep) to the value about 5-8. The soluble forms of Ca and Mg have been elevated considerably]]></dc:description>
<dc:description xml:lang="en"><![CDATA[6). The mineral fertilizing has caused an increase in the available forms of K and P]]></dc:description>
<dc:description xml:lang="en"><![CDATA[7). In the effect of waste lime use (from the smelting work) a distinct increase of the heavy metal content in the soil (especially Cu, Pb, Zn, Cd, Mn and Co) has been noted]]></dc:description>
<dc:description xml:lang="en"><![CDATA[zeszyt 15 ukazał się jako nr 135 serii głównej]]></dc:description>
<dc:description xml:lang="en"><![CDATA[seria główna: Zeszyty Naukowe]]></dc:description>
<dc:description xml:lang="en"><![CDATA[nr 1-4 tytuł: Wyższa Szkoła Inżynierska im. Jurija Gagarina w Zielonej Górze - Zeszyty Naukowe]]></dc:description>
<dc:description xml:lang="en"><![CDATA[nr 5-11 tytuł: Politechnika Zielonogórska - Zeszyty Naukowe]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[Miocene sediments, collected during brown coal excavation, have generally mechanical composition of loamy sand. The most negative feature of them is a very low pH-value, in a consequence of pyrite-oxidation. 20 years after technical reclamation and dump areas afforestation, a few conclusions about effects of the reclamation have been drawn:]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[1). The soil material in layer from 1 to 2 m deep is not homogenous. The layer from 0 to 20 cm is more homogenous as the result of mechanical cultivation before the sowing]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[2). After the slopes leveling intensive erosion processes have been occurred. About 25% of the total area has been damaged by water erosion. This effect should be connected with the absence of plant-cover]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[3). Soil-formation is related to anthropogenic activity, especially intensive liming, mineral fertilizing and afforestation. The influence of afforestation on soil is yet not very high. Clearly visible is a thin duff-layer (A0) ? about 1 cm]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[4). Nevertheless the heavy machines using during leveling, physical and water properties of the soils are quite good]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[5). The high lime doses causing rising the pH of top-soil-material (20-30 cm deep) to the value about 5-8. The soluble forms of Ca and Mg have been elevated considerably]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[6). The mineral fertilizing has caused an increase in the available forms of K and P]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[7). In the effect of waste lime use (from the smelting work) a distinct increase of the heavy metal content in the soil (especially Cu, Pb, Zn, Cd, Mn and Co) has been noted]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[zeszyt 15 ukazał się jako nr 135 serii głównej]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[seria główna: Zeszyty Naukowe]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[nr 1-4 tytuł: Wyższa Szkoła Inżynierska im. Jurija Gagarina w Zielonej Górze - Zeszyty Naukowe]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[nr 5-11 tytuł: Politechnika Zielonogórska - Zeszyty Naukowe]]></dc:description>
<dc:publisher><![CDATA[Zielona Góra: Oficyna Wydawnicza Uniwersytetu Zielonogórskiego]]></dc:publisher>
<dc:contributor><![CDATA[Kołodziejczyk, Urszula - red.]]></dc:contributor>
<dc:contributor><![CDATA[Greinert, Andrzej - red.]]></dc:contributor>
<dc:date><![CDATA[2007]]></dc:date>
<dc:type xml:lang="en"><![CDATA[artykuł]]></dc:type>
<dc:type xml:lang="pl"><![CDATA[artykuł]]></dc:type>
<dc:format xml:lang="en"><![CDATA[application/pdf]]></dc:format>
<dc:format xml:lang="pl"><![CDATA[application/pdf]]></dc:format>
<dc:identifier><![CDATA[http://www.zbc.uz.zgora.pl/repozytorium/Content/45386/PDF/8_drab_forest.pdf]]></dc:identifier>
<dc:identifier><![CDATA[https://zbc.uz.zgora.pl/repozytorium/dlibra/publication/51618/edition/45386/content]]></dc:identifier>
<dc:identifier><![CDATA[oai:zbc.uz.zgora.pl:45386]]></dc:identifier>
<dc:source xml:lang="en"><![CDATA[Zeszyty Naukowe Uniwersytetu Zielonogórskiego, Tom 15]]></dc:source>
<dc:source xml:lang="pl"><![CDATA[Zeszyty Naukowe Uniwersytetu Zielonogórskiego, Tom 15]]></dc:source>
<dc:language><![CDATA[pol]]></dc:language>
<dc:language><![CDATA[eng]]></dc:language>
<dc:relation><![CDATA[oai:zbc.uz.zgora.pl:publication:51618]]></dc:relation>
<dc:rights xml:lang="en"><![CDATA[Biblioteka Uniwersytetu Zielonogórskiego]]></dc:rights>
<dc:rights xml:lang="pl"><![CDATA[Biblioteka Uniwersytetu Zielonogórskiego]]></dc:rights>
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