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Influence of secondary transformation index of peat-muck soils on the content of selected metals

100%

Boguta P., Sokołowska Z., Bowanko G.

Acta Agrophysica

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2011

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tom 18

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nr 2[193]

The main aim of the study was the determination of the content of selected metal ions in soils originating from Polesie Lubelskie and Biebrza River Region, as well as an attempt at relating the results obtained to the degree of secondary transformation of studied soils. All the soils belonged to peat-muck soils and differed from each other in their secondary transformation index. The study included analyses of the content of potassium, calcium, magnesium and manganese with the use of absorption atomic spectroscopy for the determination of the concentration of those metals. At the next stage of the study, relationships between the secondary transformation index of peat-muck soils and selected metal contents were examined. Weak linear relationships were found for the secondary transformation index and the content of calcium, manganese and potassium. A more complex situation was observed for the relation of magnesium ions. The lack of a straight-line trend could be explained in this case by the effect of chemical processes occurring in particular classes of mucks transformation on magnesium ion binding.

2

Verification of the hydraulic model for the surface water system of the Central Biebrza River Basin

86%

Kubrak J., Okruszko T., Byczkowski A., Chormanski J., Kardel I.

Annals of Warsaw Agricultural University. Land Reclamation

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2000

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tom 30

29-36

3

Terrestrial Laser Scanning (TLS) as a detection method of the natural river valley microtopography – case study of the Upper Biebrza

86%

Brach M., Chormanski J.

Annals of Warsaw University of Life Sciences - SGGW. Land Reclamation

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2014

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tom 46

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nr 4

This paper concerns the use of Terrestrial Laser Scanning (TLS) methods and the Geographic Information Systems (GIS) analysis to determine microtopography of a natural river valley, case study of the upper Biebrza valley. The scientific problem analyzed in this paper is a morphology of the selected segments of the valley covered by sedge ecosystems which in natural stage form a characteristic tussocks from their root systems. In order to capture the microtopography it was necessary to remove vegetation from the selected areas, and then, for a five typical location, registration of its structure using the laser scanner. As a result the point cloud was generated for each of the selected area and after GIS analysis the microtopography was obtained in form of digital terrain model (DTM). The DTM of each area represents valleys microstructure possible to obtain by use of TLS (TLS DTM), is usually not registered by the Airborne Laser Scanning (ALS), and is the main reason of inaccuracy of the DTM obtained based on ALS. The resulting TLS DTM has been processed by various filtering methods to lower the noise and fi ll the voids from blocking the laser beam by a tussocks. Finally, this allowed to determine the spatial structure of each measurement field.

4

Effect of peat decomposition on the capillary rise in peat-moorsh soils from the Biebrza River Valley

86%

Gnatowski T., Szatylowicz J., Brandyk T.

International Agrophysics

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2002

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tom 16

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nr 2

5

The flood extent in the lower Biebrza basin calculated by the 1D flow model for different land use scenarios

72%

Szporak S., Miroslaw-Swiatek D., Chormanski J.

Annals of Warsaw University of Life Sciences - SGGW. Land Reclamation

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2008

|

tom 40

6

Determination of influence of vegetation on the friction factors of the Biebrza River

72%

Swiatek D., Verhoeven R., Chormanski J., Okruszko T., Ignar S., Banasiak R.

Electronic Journal of Polish Agricultural Universities. Series Environmental Development

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2008

|

tom 11

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nr 1

7

Roslinnosc lesna Doliny Biebrzanskiej

72%

Czerwinski A.

Acta Agrophysica

|

2002

|

tom 67

45-58

8

Basis of water management in the valley of Lower Biebrza River

72%

Mioduszewski W., Querner E. P., Slesicka A., Zdanowicz A.

Journal of Water and Land Development

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2004

|

nr 08

9

Risks associated with river maintenance outside protected areas - the case of Unio crassus in a tributary of the Biebrza River, n.e. Poland

72%

Ozgo M., Urbanska M., Biereznoj-Bazillle U.

Folia Malacologica

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2016

|

tom 24

|

nr 1

10

Spatial and temporal variability of the interception in the natural wetland valley, the lower Biebrza basin case study

72%

Ignar S., Weglewska A., Szporak-Wasilewska S., Chormanski J.

Annals of Warsaw University of Life Sciences - SGGW. Land Reclamation

|

2013

|

tom 45

|

nr 1

The paper presents the research carried out in the lower basin of Biebrza River valley in order to identify interception for natural wetland plant communities. Maximum interception, i.e. the largest amount of water, expressed in millimeters, which can be captured and retained by plant canopy from rainfall is one of the key parameters of the water cycle modeling. Maximum interception was determined based on the difference of the masses of wet and dry fresh plant samples. Collection of plant material samples took place during the five measurement sessions, which began immediately after the flood recedes, and then lasted until the end of the growing season. Interception spatial variability was analyzed on the basis of the results of maximum interception measured for selected plant aggregations in the different sampling points. The obtained values were extrapolated to the area of the lower basin of Biebrza River using vegetation map of the Biebrza National Park. By conducting a test sessions in the five coming months, the maps of the spatial variability also show changes over time. Methodology used in the described tests allowed for obtaining of satisfactory results. They present, in a correct way, variation occurring between the plant aggregations due to their morphology. In most cases the results are consistent with data from the literature. As results of the analysis of spatial variability of the maximum interception, the highest values were found for the plant communities located in the immediate vicinity of the river channel. With the increase of the distance from river towards the valley edges the maximum interception values decrease. These changes can be seen in the form of strips parallel to the river channel, which corresponds to the plant zones. Obtained map of spatial variability of the maximum interception, which is the results of extrapolation of the values assigned to plant communities, has a high correlation with the map resulting from the analysis of satellite images.

11

Occurrence of nitrogen cycle bacteria in the Biebrza River

72%

Frak M., Kardel I., Jankiewicz U.

Annals of Warsaw University of Life Sciences - SGGW. Land Reclamation

|

2012

|

tom 44

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nr 1

This paper of the selected groups of nitrogen cycle bacteria in the Biebrza River was analysed. In the water samples the quantity of ammonifying bacteria, nitrifying bacteria, proteolitic bacteria was estimated and also selected water quality indicators were analysed. Large quantities of proteolitic bacteria and ammonifying bacteria were found while the quantity of nitrifying bacteria was very small. Water quality analyses proved high TOC concentrations and low nitrate as well as nitrite concentrations. It was found, that the mineral forms of nitrogen being the intensive product of organic matter degradation is not released (low concentrations of ammonia), but it is accumulated in microorganisms cells. Low concentrations of ammonia are limiting for the number of nitrifying bacteria. The seasonal character of the occurrence of all analysed bacteria groups was as well found. The analytical procedure used was adjusted for bacteriological research on rivers of low anthropopressure.

12

The Shuttle Radar Topography Mission Digital Elevation Model as an alternative data source for deriving hydrological characteristics in lowland catchment - Rogozynek catchment case study

72%

Wasilewski M., Chormanski J.

Annals of Warsaw University of Life Sciences - SGGW. Land Reclamation

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2009

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tom 41

|

nr 1

13

Temporal variability of the selected flood parameters in the Biebrza River valley

72%

Ignar S., Maksymiliuk-Dziuban A., Miroslaw-Swiatek D., Chormanski J., Okruszko T., Wysocki P.

Annals of Warsaw University of Life Sciences - SGGW. Land Reclamation

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2011

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tom 43

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nr 2

14

Further studies on aquatic fungi in the River Biebrza within Biebrza National Park

72%

Czeczuga B., Kiziewicz B., Mazalska B.

Polish Journal of Environmental Studies

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2003

|

tom 12

|

nr 5

Zoosporic and conidial fungi species and environmental factors in 12 various sites of the River Biebrza in Biebrza National Park were studied. Samples of water were collected in autumn 1999 and spring 2000 for hydrochemical analysis in order to determine the number of fungal species. Buckwheat-seeds, hemp- seeds, cellophane and snake exuviae were used as bait during exposure in a laboratory. 199 lower aquatic fungus species were found in various sites of the River Biebrza. 16 species were recorded for the first time from Poland.

15

Influence of different management measures on water conditions within the Lower Biebrza Valley

72%

Bielecka J., Wielechowska-Nauta A., Querner E.

Journal of Water and Land Development

|

2005

|

nr 09

16

Application of the WetSpa distributed hydrological model for catchment with significant contribution of organic soil. Upper Biebrza case study

58%

Chormanski J., Batelaan O.

Annals of Warsaw University of Life Sciences - SGGW. Land Reclamation

|

2011

|

tom 43

|

nr 1

The paper treats on hydrological distributed model adaptation for a catchment with significant contribution of wetland. The WetSpa model was applied to analyzing the effects of topography, soil type, and land use cover on the runoff characteristics for upper Biebrza catchment. The derivation of parameter maps and analysis of the daily runoff as reaction of the catchment on rainfall was performed. The semi-automated calibration of the model was executed using PEST module. Then, the assessment of that crucial processes was done by calculating errors of mathematical models performance as well as hydrograph comparison. Error values, have shown that the model efficiency was estimated to be good for high flows, but unsatisfactory for low flows. This initial modeling approach gives possibility to ask question about limitation and needs of wetland catchment for rainfall-runoff modeling.

17

Protection of natural wetlands - the examples of conflicts

58%

Mioduszewski W., Okruszko T.

Journal of Water and Land Development

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2012

|

nr 16

18

Nutrients availability and hydrological conditions of selected wetland ecosystems in the Biebrza river valley

58%

Stelmaszczyk M., Okruszko T., Meire P.

Annals of Warsaw University of Life Sciences - SGGW. Land Reclamation

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2015

|

tom 47

|

nr 1

Nutrients availability and hydrological conditions of selected wetland ecosystems in the Biebrza river valley. Paper presents results of investigation of hydrological conditions and nutrients limitation and availability for wetland vegetation in selected sites within Biebrza river valley. Analysed sites were overgrown by tall sedge Magnocaricion vegetation (Caricetum gracilis and Caricetum elatae), wet meadow Molinio-Arrhenatheretea vegetation (Molinietum caeruleae), and sedge-moss Scheuchzerio-Caricetea nigrae vegetation (Caricetum lasiocarpae). There were noted a close relationship between vegetation types, hydrological regimes and kind of nutrient limitation. Low productive Molinio-Arrhenatheretea and Scheuchzerio-Caricetea nigrae vegetations fed mainly by groundwater were limited by phosphorus, while highly productive Magnocaricion vegetation, fed by river water, was subjected to nitrogen limitation. We have found big diversifi cation of groundwater and surface water levels within habitats of different vegetation types along the Biebrza river valley. Magnocaricion vegetation present on fl ooded areas is characterized by signifi cant water level fl uctuations and long-lasting inundations. On areas covered by Molinio- -Arrhenatheretea vegetation we noted majority of water levels not exceeding the level of the ground surface. Whereas Scheuchzerio-Caricetea nigrae vegetation, fed by groundwater, is characterized by low variation of groundwater levels.

19

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

58%

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

Polish Ecological Studies

|

1997

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tom 23

|

nr 3-4

20

Spring assemblies of waders in flood plains of the lower Biebrza and the middle Narew River valleys

58%

Gorski A., Nowakowski J. J.

The Ring

|

1998

|

tom 20

|

nr 1-2

Ograniczanie wyników

Influence of secondary transformation index of peat-muck soils on the content of selected metals

Verification of the hydraulic model for the surface water system of the Central Biebrza River Basin

Terrestrial Laser Scanning (TLS) as a detection method of the natural river valley microtopography – case study of the Upper Biebrza

Effect of peat decomposition on the capillary rise in peat-moorsh soils from the Biebrza River Valley

The flood extent in the lower Biebrza basin calculated by the 1D flow model for different land use scenarios

Determination of influence of vegetation on the friction factors of the Biebrza River

Roslinnosc lesna Doliny Biebrzanskiej

Basis of water management in the valley of Lower Biebrza River

Risks associated with river maintenance outside protected areas - the case of Unio crassus in a tributary of the Biebrza River, n.e. Poland

Spatial and temporal variability of the interception in the natural wetland valley, the lower Biebrza basin case study

Occurrence of nitrogen cycle bacteria in the Biebrza River

The Shuttle Radar Topography Mission Digital Elevation Model as an alternative data source for deriving hydrological characteristics in lowland catchment - Rogozynek catchment case study

Temporal variability of the selected flood parameters in the Biebrza River valley

Further studies on aquatic fungi in the River Biebrza within Biebrza National Park

Influence of different management measures on water conditions within the Lower Biebrza Valley

Application of the WetSpa distributed hydrological model for catchment with significant contribution of organic soil. Upper Biebrza case study

Protection of natural wetlands - the examples of conflicts

Nutrients availability and hydrological conditions of selected wetland ecosystems in the Biebrza river valley

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

Spring assemblies of waders in flood plains of the lower Biebrza and the middle Narew River valleys