Wyniki wyszukiwania

1

Floods in the river valleys of the Eastern Mid-European Lowland

100%

Kolodziejczyk U.

Zeszyty Naukowe Uniwersytetu Zielonogórskiego. Inżynieria Środowiska

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2004

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nr 12[131]

2

Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik

Phylogenetic analyses of Bartonella sp. (Bacteria) of rodents from four separated valleys in Sinai Mountains (Egypt)

100%

Alsarraf M., Mohallal E. M., Kwiatowski J., Mierzejewska E. J., Welc-Faleciak R., Behnke J. M., Bajer A.

Annals of Parasitology

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2016

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tom 62

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nr Suppl.

3

Perception of Vistula Valley landscape in Warsaw cultural elements. Balance and repletion process

100%

Skalski J.

Annals of Warsaw Agricultural University. Horticulture

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1999

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tom 20

4

Symbolism and utilitarian significance of Cistercian fountains

84%

Milecka M., Rozanska A.

Annals of Warsaw University of Life Sciences - SGGW. Horticulture and Landscape Architecture

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2008

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tom 29

5

Floristic diversity of chosen grass communities in the Nadwieprzanski Landscape Park

84%

Warda M., Stamirowska-Krzaczek E.

Annales Universitatis Mariae Curie-Skłodowska. Sectio E. Agricultura

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2010

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tom 65

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nr 1

6

The development of Lithuanian river valleys in late and post-glacial times

84%

Dvareckas V.

Quaestiones Geographicae. Zeszyt Specjalny

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1992

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tom 03

7

Recognition of valley evolution during the Pleistocene-Holocene transition in non-glaciated regions of the Polish lowland

84%

Turkowska K.

Biuletyn Peryglacjalny

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1995

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tom 34

8

Holocene overbank deposits and mollusc fauna, Olawa River valley [Sudety Foothills, Western Poland]

84%

Alexandrowicz S. W., Teisseyre A. K.

Bulletin of the Polish Academy of Sciences. Earth Sciences

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1997

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tom 45

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nr 1

9

Arbuscular mycorrhizal fungi of the Brda River valley in the Tuchola Forests

84%

Tadych M., Blaszkowski J.

Acta Mycologica

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2000

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tom 35

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nr 1

10

Evolution of the lower Vistula River valley in the upper Pleni Vistulian

84%

Wisniewski E.

Quaestiones Geographicae. Zeszyt Specjalny

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1992

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tom 03

11

The role of neotectonics in the Quaternary evolution of the landscape of the Sowie Mts, Sudetes, Southwestern Poland

84%

Krzyszkowski D., Olejnik W.

Geologia Sudetica

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1998

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tom 31

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nr 2

12

Dynamics of Prunus domestica L.ssp.domestica on the area of Odra Valley slopes near Krosno Odrzanskie after reduction of human impact

84%

Boratynski A., Ratynska H., Waldon B.

Publications of the Department of Plant Taxonomy of the Adam Mickiewicz University in Poznan

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2000

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tom 10

13

High-mountain environment of the Tatras in the period of Pleistocene and Holocene transition

84%

Baumgart-Kotarba M., Kotarba A.

Biuletyn Peryglacjalny

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1995

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tom 34

14

Geographic record of human impact conformance to different water relationships along a coastal river (the Lupawa catchment)

67%

Drwal J., Cieslinski R., Fac-Beneda J.

Quaestiones Geographicae

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2011

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tom 30

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nr 1

15

Links between vegetation and morphodynamics of high-mountain slopes in the Tatra Mountains

67%

Kozlowska A., Raczkowska Z., Zagajewski B.

Geographia Polonica

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2006

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tom 79

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nr 1

16

Metodyka obliczania niedoborów wodnych użytków zielonych, z uwzględnieniem zróżnicowanych warunków wodnych w siedliskach dolinowych

67%

Roguski W.

Zeszyty Problemowe Postępów Nauk Rolniczych

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1990

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tom 387

Травяные угодья в Польше расположены главным образом в речных долинах и в понижениях площади. Находящиеся там почвы располагают запасами легко усвояемой воды колеблющиеся от 30 до 120 мм. Кроме того грунтовые воды могут интенсивно снабжать некоторые биотопы лугов за счет капиллярного подпитывания. Таким образом биотопы травяных угодий имеют различные водные режимы. Автор предлагает проводить оценку дефицитов воды в декадах по формуле: N = ETP - P - EPUn + EPUk + H, где: N - дефицит воды, ETP - актуальная эвапотранспирация, Р - атмосферные осадки, EPUp, EPUk - легко усвояемая растениями вода в начале и конце периода, Н - сток воды. Установлено, что травяние угодья на хороших торфяно-муршевых почвах интенсивно подпитываемые от уровня грунтовых вод, не нуждаются в орошении, тогда на худших почвах без подитывания необходимы в сухие годы орошения на уровне 120-230 мм.

17

Concentration of 137Cs, 40K, 238Pu and 239plus240Pu radionuclides and some heavy metals in soil samples from two main valleys from Tatra National Park

67%

Kubica B., Mietelski J. W., Golas J., Skiba S., Tomankiewicz E., Gaca P., Jasinska M., Tuteja-Krysa M.

Polish Journal of Environmental Studies

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2002

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tom 11

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nr 5

This paper presents the results of determinations of radiocesium and plutonium activity concentrations and some heavy metals in soil samples from two main Tatra Valleys: Kościeliska and Rybi Potok Valley. The results were obtained during 2001. It has been found that the content of 137Cs and 239+240Pu is much higher at altitudes over 1300 m asl.

18

Sward density on Wizna Fen grasslands differing in their peat origin [ice-marginal valley of River Biebrza, Poland]

67%

Pasternak-Kusmierska D., Cieslewicz M., Kotowska J., Wilpiszewska I.

Polish Ecological Studies

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1997

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tom 23

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nr 3-4

19

An effect of a damming on the Odra River in Brzeg Dolny ob water conditions in the valley

67%

Plywaczyk L.

Journal of Water and Land Development

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2000

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nr 04

This paper presents changes in the water conditions of the Odra River valley as a result of the construction and 40 years of operation of the Brzeg Dolny dam. The following characteristics of the Odra River valley are shown: a dynamics of changes of the river bed and water levels above and below the dam, changes of groundwater structure and variations of the water table in the valley. Relations between the groundwater table and water levels in the Odra River are presented and the influence of the groundwater table on soil water management is demonstrated. An analysis of surface water resources in the area adjacent to the valley was carried out above and below the Brzeg Dolny dam.

20

The role of drainage basin orography in the river channel pattern tranformation during Late Vistulian, Subcarpathian Oswiecim Basin, Poland

67%

Klimek K.

Quaestiones Geographicae. Zeszyt Specjalny

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1995

|

tom 04

Ograniczanie wyników

Floods in the river valleys of the Eastern Mid-European Lowland

Phylogenetic analyses of Bartonella sp. (Bacteria) of rodents from four separated valleys in Sinai Mountains (Egypt)

Perception of Vistula Valley landscape in Warsaw cultural elements. Balance and repletion process

Symbolism and utilitarian significance of Cistercian fountains

Floristic diversity of chosen grass communities in the Nadwieprzanski Landscape Park

The development of Lithuanian river valleys in late and post-glacial times

Recognition of valley evolution during the Pleistocene-Holocene transition in non-glaciated regions of the Polish lowland

Holocene overbank deposits and mollusc fauna, Olawa River valley [Sudety Foothills, Western Poland]

Arbuscular mycorrhizal fungi of the Brda River valley in the Tuchola Forests

Evolution of the lower Vistula River valley in the upper Pleni Vistulian

The role of neotectonics in the Quaternary evolution of the landscape of the Sowie Mts, Sudetes, Southwestern Poland

Dynamics of Prunus domestica L.ssp.domestica on the area of Odra Valley slopes near Krosno Odrzanskie after reduction of human impact

High-mountain environment of the Tatras in the period of Pleistocene and Holocene transition

Geographic record of human impact conformance to different water relationships along a coastal river (the Lupawa catchment)

Links between vegetation and morphodynamics of high-mountain slopes in the Tatra Mountains

Metodyka obliczania niedoborów wodnych użytków zielonych, z uwzględnieniem zróżnicowanych warunków wodnych w siedliskach dolinowych

Concentration of 137Cs, 40K, 238Pu and 239plus240Pu radionuclides and some heavy metals in soil samples from two main valleys from Tatra National Park

Sward density on Wizna Fen grasslands differing in their peat origin [ice-marginal valley of River Biebrza, Poland]

An effect of a damming on the Odra River in Brzeg Dolny ob water conditions in the valley

The role of drainage basin orography in the river channel pattern tranformation during Late Vistulian, Subcarpathian Oswiecim Basin, Poland