Roczniki gleboznawcze  Tom LVII nr  3/4, Warszawa 2006: 1–176

 

 

 

Spis treści

 

Becher M., Kalembasa D.: Charakterystyka bituminów leśnych gleb

rdzawych  i bielicowych na Nizinie Południowopodlaskiej.characteristic

of bitumens of forest haplic arenosols and haplic podzols located on

south Podlasie lowland. ........ 5                             

 

Czarnowska K., Nowakowski W.: Zmiany zawartości Fe, Mn, Zn, Cu,  Pb w

trawach zieleńców  warszawy. Changes in the content of Fe, Mn, Zn, Cu,

Pb in grasses from lawns of warsaw. ...........13 

 

Frankowska-łukawska J.,  Chachulski Ł..: typy gleb i zespoły roślinne

powyżej wtórnej granicy lasu na połoninach w paśmie czarnohory. soil

types and plant associations above the secondary forest border on

poloninas in chernohora mountains.  ........... 18 

 

Jóźwiakowski K., Marzec  M., Obroślak R.: Zmiany stanu jakości wód

powierzchniowych w dolinie rzeki ciemięgi w latach 1999–2004. Changes of

surface water quality in the valley of Ciemięga river in 1999–2004 ....... 37

 

Kalembasa D., Becher M.: Węgiel i azot w wydzielonych frakcjach

materii organicznej  leśnych gleb rdzawych i bielicowych niziny

południowopodlaskiej. carbon and nitrogen in  separated fractions of

organic matter in forest haplic arenosols and haplic

podzols of south podlasie lowland. ........... 44

 

Kaźmierowski C.,  Spychalski M.,  Kaczmarek Z.:  Accuracy of the

indirect methods of hydraulic conductivity estimation in selected soils

of wielkopolska province. Dokładność pośrednich metod estymacji

współczynnika filtracji w wybranych glebach wielkopolski.   ......... 55

 

Kołodziej B.,  Słowińska-jurkiewicz  A.,  Jońca M.: Właściwości

powietrzne  gleby  rekultywowanej na terenie  po  kopalni  siarki. air

properties of reclaimed soil on the area of abandoned sulphur mine.

....... 66

 

Noworolnik K.,  Terelak H.: Wpływ agrochemicznych właściwości gleb

na plon ziarna i białka jęczmienia jarego i owsa oraz ich mieszanki. The

effect of soil properties on grain and protein yields of spring barley,

oats and their mixture.   ...........72

 

Oleszczuk P.,  Baran S.: Zastosowanie biotestów do oceny

zanieczyszczenia gleb przez wielopierścieniowe węglowodory

aromatyczne. .Application of biotests to evaluation of soil

contamination by polycyclic aromatic hydrocarbons. ........... 80   

 

Paszko T.: Wpływ konkurencyjnych oddziaływań Cr3+ i Cu2+ z Cd2+, Co2+,

Ni2+, Pb2+ lub Zn2+ na wielkość ich sorpcji oraz desorpcji w glebie.

Influence of competitive interactions of  Cr3+ and Cu2+ with  Cd2+,

 Co2+, Ni2+, Pb2+ or Zn2+ on the volume of their sorption and desorption

in a soil.   ......... 90

 

Pietrzykowski M.: właściwości gleb powstających na rekultywowanych i

pozostawionych sukcesji terenach wyrobiska po eksploatacji piasków

podsadzkowych. properties of soils formed on reclaimed areas and areas

left for succession  on abandoned sand  excavation.   ........... 97

 

Rusek A.: Aktywność dehydrogenaz w glebie zanieczyszczonej olejem

napędowym w polowym doświadczeniu lizymetrycznym. Dehydrogenase activity

in soils polluted by diesel oil in a field lysimeter experiment . ...... 106

 

Skorbiłowicz E.: wpływ rodzaju zlewni na stężenia ołowiu, cynku i

miedzi w osadach dennych wybranych dopływów górnej narwi. Influence of

type of drainage basin on concentrations of  lead, zinc and copper in

bottom sediments selected tributaries of  upper Narew.  ....... 117

 

Skorbiłowicz M.: ocena wpływu rodzaju oraz intensywności źródeł

zanieczyszczeń wód rzeki Supraśl. Evaluation of pollution sources

influence on river Supraśl water.   ........ 127

 

Wolna-Maruwka A.,  Sawicka  A.: Aktywność oddechowa gleby

nawożonej osadem ściekowym. respiration activity in the soil fertilised

with sewage sludge.  ........... 135

 

Zubala T., Węgorek T.,  Patro M.: Zmiany użytkowania gleb silnie

urzeźbionej zlewni w aspekcie ochrony Krajobrazu. the soil use changes

in high relief catchment in aspect of  the landscape conservation.  ........ 144

 

Artykół problemowy       

 

Konecka-Betley K., Czępińska-Kamińska D., Okołowicz M., Zagórski

Z.: Procesy glebotwórcze w lessowych glebach kopalnych odsłonięcia

polanów samborzecki –  okolice sandomierza. pedogenetic processes in

palaeosols of the polanów samborzecki loesses exposure – vicinity of

sandomierz. ........... 152

 

Chojnicki J.: Profesor Marian Kępka (1922–2005)  – Wspomnienie.  ......... 175

 

 

Becher M., Kalembasa D.: Charakterystyka bituminów leśnych

gleb rdzawych  i bielicowych na Nizinie Południowopodlaskiej.

characteristic of bitumens of forest haplic arenosols and haplic podzols

located on south Podlasie lowland.  

Abstract: In this paper  presented are the elemental composition and

IR spectra of soil bitumens extracted from organic and mineral horizons

of forest  Haplic Arenosols and Haplic Podzols, situated in South

Podlasie Lowland. The elemental composition of investigated bitumens did

not differ and the average content of  elements (in the atomic percents)

was as follows: C – 34.7; O – 7.60; H – 57.4; N – 0.24 and (in g · kg–1)

S – 2.35; P – 0.66. IR spectra showed intensive absorption of waves in

the ranges characteristic for the aliphatic chains, and less intensive

(disappearing as the depth of the profile increased) in respect to the

aromatic rings/./

Słowa kluczowe: bituminy, skład elementarny, IR, gleby rdzawe, gleby

bielicowe.

Key words: bitumens, elemental composition, IR, Haplic Arenosols,

Haplic Podzols.

 

Czarnowska K., Nowakowski W.: Zmiany zawartości Fe, Mn, Zn, Cu,

Pb w trawach zieleńców Warszawy  Changes in the content of Fe, Mn, Zn,

Cu, Pb in grasses from lawns of warsaw.  

Abstract: The present paper refers to the study on Fe, Mn, Zn, Cu and

Pb concentration in grasses situated in different places of Warsaw.

Considering twenty five years period covered by the present study the

concentration of lead has doubled in studied grasses, while the

concentration of Fe, Mn, Zn, Cu  in grasses has been stable.

Słowa kluczowe: trawy, żelazo, cynk, miedź, ołów, zanieczyszczenie,

zieleńce.

Key words: grasses, iron, zinc, copper, lead, pollution, lawns. 

 

 

 

Frankowska-Łukawska J., Chachulski Ł.: Typy gleb i zespoły roślinne

powyżej wtórnej granicy lasu na połoninach w paśmie czarnohory. soil

types and plant associations above the secondary forest border on

poloninas in chernohora mountains.

Abstract: In the years 2001–2003 the phytosociological and soil

investigations were conducted in the alpine and subalpine belt of

Chernohora Mountains. On the basis of percentage of soil granulometric

fractions and chemical properties of soil, three soil types were

identified. Phytosociological investigations carried out simultaneously,

indicated that particular plant associations occur on specific soil

types. Alpine phytocenoses Caricetum sempervirentis and

Rododendretum myrtifolii occur on Lithic Leptosols.

Pulmonario-Alnetum viridis and Calamagrostietum villosae in

typical form with smallest species richness but bigger amount of

characteristic plants occur on Lithic Leptosols while

Pulmonario-Alnetum viridis anthropogenic form of

Calamagrostietum villosae and Poo-Deschampsietum caespitosae

occur on Leptic Cambisols. On Leptic Regosols only Caricetum

sempervirentis was detected.

Słowa kluczowe:gleby górskie, subalpejskie zbiorowiska roślinne,

Karpaty Wschodnie, Czarnohora.

Key words: mountain soils, subalpine plant cover, Eastern

Carpathians, Chernohora Mountains Range. 

 

Jóźwiakowski K., Marzec  M., Obroślak R.: Zmiany stanu jakości wód

powierzchniowych w dolinie rzeki ciemięgi w latach 1999–2004. changes of

surface water quality in the valley of Ciemięga river in 1999–2004.

Abstract: This study presents the results of investigations

concerning changes of  the surface water quality in Valley of Ciemięga

River. The investigations were conducted in 1999–2004. The samples for

analyses were taken from four ponds and from the Ciemięga River in

Jastków and Snopków. The water quality in ponds and in the Ciemięga

River has been qualified to the fourth and fifth class of water quality.

The indicators which decrease water quality are: BOD5, COD, total

nitrogen, phosphates, total suspended solids and iron. no clear

improvement of water quality in analyzed reservoirs and Ciemięga river

was observed recently.

Słowa kluczowe: jakość wód powierzchniowych, zlewnia rolnicza.

Key words: surface water quality, agricultural catchment.

 

Kalembasa D., Becher M.: Węgiel i azot w wydzielonych frakcjach

materii organicznej leśnych gleb rdzawych i bielicowych niziny

południowopodlaskiej. carbon and nitrogen in  separated fractions of

organic matter in forest haplic arenosols and haplic podzols of south

podlasie lowland.     

Abstract: The content of total carbon and nitrogen in organic matter

and in different fractions in  forest soils of the South Podlasie

Lowland region is presented. The content of organic carbon in the

analyzed fractions was as follows (% C in Ct): bitumen 2.70–18.2, fulvic

acids 9.50–59.8, humic acid 3.28–37.6, in residue after extraction

15.8–71.0 and nitrogen respectively (% N in Nt): 0.57–55.1; 12.4–53.3;

10.1–60.0; 3.77–74.4. The content of nitrogen expressed as total amount

and in fractions was differentiated among analyzed profiles, and  was

significantly correlated with the content of organic carbon. The

differentiated values of ratio C:N confirmed big variability in the

quality of organic matter depending on the type of soil and genetic

horizons.

Słowa kluczowe: materia organiczna gleb, gleby rdzawe, gleby bielicowe.

Key words: soil organic matter, Haplic Arenosols,  Haplic

Podzols.       

 

Kaźmierowski C., Spychalski M., Kaczmarek Z.: Accuracy of the

indirect methods of hydraulic conductivity estimation in selected soils

of wielkopolska province. Dokładność pośrednich metod estymacji

współczynnika filtracji w wybranych glebach wielkopolski.

Abstract: The accuracies of estimation of saturated hydraulic

conductivity with the use of selected pedotransfer functions have been

analysed for a set of results from 73 soil horizons. The highest

accuracy has been obtained for estimations with the power function model

Ks = B(f/d//)n proposed by Ahuja et al. [1984]. The authors propose new

values of B and n parameters of this dependence derived for selected

soils of Wielkopolska for which a higher accuracy of Ks estimation has

been obtained than those achieved in the earlier published proposals.

Abstrakt: W pracy przeanalizowano dokładność estymacji

współczynnika filtracji – Ks przy użyciu wybranych funkcji PTF

(pedotransfer function). Analizy przeprowadzone na zbiorze oznaczeń

z 73 poziomów glebowych wykazały, iż największą dokładność estymacji Ks

zapewnia zależność Ks = B(fd)n [Ahuja i in. 1984]. Dla zależności tej

opracowano własne parametry uzyskując wzrost dokładności estymacji Ks w

badanych glebach w stosunku do publikowanych rozwiązań.

Key words: saturated hydraulic conductivity, drainage porosity,

pedotransfer function (PTF).

Słowa kluczowe: współczynnik filtracji (Ks), porowatość drenażowa,

funkcje PTF.

 

Kołodziej B., Słowińska-Jurkiewicz A., Jońca M.: Właściwości

powietrzne  gleby  rekultywowanej na terenie  po  kopalni  siarki. air

properties of reclaimed soil on the area of abandoned sulphur mine.

Abstract: The present project aims at research on the air properties

of soil on a devastated area of abandoned  sulphur mine in Jeziórko near

Tarnobrzeg. Serious problem of this area is not only chemical

degradation, but also degradation of physical properties of soil cover,

first of all, water-air properties of soil. The research was conducted

on fields of different reclamation direction (meadow and forest) and on

fields during reclamation. It was stated that the most advantageous air

properties occurred on the fields (especially meadow) six years after

reclamation, the worst on the field directly after technical reclamation

and introduction of sewage sludge.

Słowa kluczowe: właściwości powietrzne, gleby zdegradowane, rekultywacja.

Key words: air properties, deformed soils, reclamation.     

 

Noworolnik K., Terelak H.: Wpływ agrochemicznych właściwości

gleb na plon ziarna i białka jęczmienia jarego i owsa oraz ich

mieszanki. The effect of soil properties on grain and protein yields of

spring barley, oats and their mixture.

Abstract:  A series of field experiments with spring barley, oats and

their mixture were carried out across Poland in years 1987–2003. Grain

yield, protein content in grain and protein yield of cereals as effected

by soil pH and P, K and Mg content in soil were determined. The highest

grain and protein yields of cereals were obtained at soil pH above 5.5

and at P content above 48 mg, K content above 130 mg and Mg content

above 60 mg in kg of soil. Higher protein content in grain of barley and

oats was stated in the case of lower soil pH and lower P, K and Mg

content in soil.

Słowa kluczowe: pH gleby, zasobność gleby w P, K i Mg,  zboża jare,

plon ziarna i białka.

Key words: soil pH; P, K and Mg content in soil, spring cereals, grain

and protein yields

 

Oleszczuk P.,  Baran S.: Zastosowanie biotestów do oceny

zanieczyszczenia gleb przez wielopierścieniowe węglowodory aromatyczne.

Application of biotests to evaluation of soil contamination by

polycyclic aromatic hydrocarbons

Abstract: The aim of the present study was to determine

relationships between the content of polycyclic aromatic hydrocarbons

and results from biotests (Phytotoxkit F, Ostracodtoxkit F). The

experimental soils were collected from: Silesia, Lublin, Biała Podlaska

and Sokolniki. The PAH content ranged widely from 363 to 27883 mg ·

kg–1. Only in the case of  L. sativum significant statistical

relationships were noted between root lengths after 3 days of incubation

and PAH content, and between root length of S. alba and the content

of  5- and  6-ring PAHs after 6 days of incubation.

Słowa kluczowe: WWA, toksyczność, gleba, antropopresja, TZO, biotesty.

Key words: PAHs, toxicity, soil, anthropopressure, POPs, biotests. .

 

Paszko T.: Wpływ konkurencyjnych oddziaływań Cr3+ i Cu2+ z Cd2+,

Co2+, Ni2+, Pb2+ lub Zn2+ na wielkość ich sorpcji oraz desorpcji w

glebie. Influence of competitive interactions of  Cr3+ and Cu2+ with

Cd2+, Co2+, Ni2+, Pb2+ or Zn2+ on the volume of their sorption and

desorption in a soil.       

Abstract: The aim of the study was to determine the effect of

competition between selected heavy metal cations on range of their

non-specific and specific sorption. The mono-component CrCl3 or CuCl2,

two-component CrCl3 and CuCl2 and three component solutions CrCl3,

CuCl2 and CdCl2, CoCl2, NiCl2, Pb(NO3)2 or ZnCl2 were introduced into

the columns with samples from the Ap horizon of Albic Luvisols.

Desorption with 0.05 mol · dm–3 solution of CaCl2 was  the method chosen

to evaluate the range of non-specific sorption. In comparison with the

one-component systems, in two-component set a significant decrease of

both non-specific and specific sorption of Cr3+ and Cu2+ appeared. In

the three-component sets both kinds of sorption of  these ions were

limited most effectively by Pb2+ and in small degree by  Cd2+, Co2+,

Ni2+ and Zn2+ cations.

Słowa kluczowe: gleba, chrom, miedź, sorpcja konkurencyjna, desorpcja.

Key words: soil, chromium, copper, competitive sorption, desorption.

 

Pietrzykowski M.: właściwości gleb powstających na rekultywowanych i

pozostawionych sukcesji terenach wyrobiska po eksploatacji piasków

podsadzkowych. properties of soils formed on reclaimed areas and areas

left for succession  on abandoned sand  excavation.

Abstract: The paper presents properties of soils formed in reclaimed

areas and in areas left for succession on a sand excavation in

chronesequence of 5, 17, 20, 25 years. In both categories of areas there

was an increase of organic carbon content and thickness of the initial

organic-mineral horizon corresponding with soil age, although in

reclaimed areas the horizon was twice as thick. Investigated soils

showed low sorption capacity and nutrient content but changes of these

characteristics were not connected with soil age. Only loamy material

insertions resulted in an increase of these features.

Słowa kluczowe: wyrobisko popiaskowe, sukcesja, rekultywacja,

inicjalne gleby.

Key words: sand excavation, succession, reclamation, initial soils.

 

Rusek  A.: Aktywność dehydrogenaz w glebie zanieczyszczonej olejem

napędowym w polowym doświadczeniu lizymetrycznym. Dehydrogenase activity

in soils polluted by diesel oil in a field lysimeter experiment.         

Abstract: Oil product spills modify the activity of microorganisms. In

this paper dehydrogenase activity in soils polluted by fuel oil is

discussed. In field experiments the influence of mineral fertilization

and fatty acid ether methyl addition on dehydrogenase activity in soils

polluted by fuel oil was investigated. The results showed that pH is the

most important factor influencing dehydrogenase activity; growing of

acidity caused a decrease in activity. Dehydrogenase activity was lower

in fertilized soils, probably due to physiologically acidic nitrogen

fertilizer effect. Addition of 5% mass fraction of rape fatty acid

methyl ethers in the whole mass of pollution caused an increase in

dehydrogenase activity six months after the experiment was established.

Słowa kluczowe: aktywność dehydrogenaz, olej napędowy, nawożenie,

biopaliwo.

Key words: dehydrogenase activity, diesel oil, fertilization,

biodiesel.   

 

Skorbiłowicz E.: wpływ rodzaju zlewni na stężenia ołowiu, cynku

i miedzi w osadach dennych wybranych dopływów górnej narwi. Influence of

type of drainage basin on concentrations of  lead, zinc and copper in

bottom sediments selected tributaries of  upper Narew.

Abstract: Studies were carried out in years 2003 and 2004 in the

catchment basin of the upper Narew. 155 samples of sediments were taken

to determine total content of lead, zinc and copper. Concentrations of

analysed elements were found to be related to the type of land use. In

most of investigated  area sediments are mostly polluted by lead. Copper

mostly is present on geochemical background level.

Słowa kluczowe: metale ciężkie, osady denne, rzeki.

Key words: heavy metals, bottom sediments, rivers.  

 

Skorbiłowicz M.: ocena wpływu rodzaju oraz intensywności źródeł

zanieczyszczeń wód rzeki supraśl. Evaluation of pollution sources

influence on river Supraśl water.

Abstract: Multi-factorial analysis was applied to identify the

pollution sources of river Supraśl. The analysis made possible to

identify and evaluate the intensity of main pollution sources influence.

Determinations and analyses revealed that Gródek town, Białystok city,

and post-bog soils localized in region of Upper and Lower Supraśl were

main sources of water pollution. Area with Puszcza Knyszyńska, fragment

of river Supraśl flows through, is an ecotone zone for the river, and it

does not introduce additional chemicals.

Słowa kluczowe: rzeka, azotany V, analiza czynnikowa.

Key words: river, nitrates, factor analysis.        

 

Wolna-Maruwka A., Sawicka A.: Aktywność oddechowa gleby

nawożonej osadem ściekowym.respiration activity in the soil fertilised

with sewage sludge.

Abstract: The main aim of the research was to investigate the rate of

organic matter decomposition implicated by the amount of released CO2

from the soil. the rate of organic matter decomposition is an index of

metabolic activity of microbiological communities inhabiting the soil.

Furthermore, correlation between the respiration activity and the number

of microorganisms in the loam sand with addition of sewage sludge and

white mustard plants (Sinapis alba L.) cultivation was also

investigated in the experiment. The release of CO2 from the soil was

determined using the absorption method. 0.5 N NaOH was titrated using

0.1 N HCl in presence of phenolphtalein. The CO2 quantity and numbers of

microorganisms in the soil were determined in five, consecutive mustard

plants developmental phases. It was stated that CO2 quantity did not

correlate with the number of all studied groups microorganisms as

Salmonella sp., E. coli, Clostridium/ sp., Azotobacter sp., the

total bacteria number, fungi, actinomycetes. The highest respiration

activity in the soil was found in  the combination with loam sand+sewage

sludge+mustard plants in the term – directly after harvest.

Słowa kluczowe: osad ściekowy, gleba, mikroorganizmy, CO2, oddychanie.

Key words: sewage sludge, soil, microorganisms, CO2, respiration.       

 

Zubala T., Węgorek T., Patro M.: Zmiany użytkowania gleb

silnie urzeźbionej zlewni w aspekcie ochrony krajobrazu. the soil use

changes in high relief catchment in aspect of  the landscape

conservation. 

Abstract: Changes of land management in dried valley basin situated

in Kazimierski Landscape Park (1991–2005) were studied. Due to the

economics transformations in agriculture, the area of fallows increased

up to 24% of basin area in 2001. The growth of weeds and trees causes

degradation of ecological and visual virtues of the landscape. In 2005,

the share of fallows decreased to 16%. However, the most valuable

landscapes with rural elements (e.g. systems of terraces caused by

plough cultivation) disappear as a result of  tree succession. Land

reclamation tending to extensive green lands is recommended to protect

the Park’s specificity.

Słowa kluczowe: użytkowanie gleb, zlewnia lessowa, krajobraz rolniczy.

Key words: soil usage, loessic catchment, agricultural landscape.

 

Konecka-Betley K., Czępińska-Kamińska D., Okołowicz M., Zagórski

Z.: Procesy glebotwórcze w lessowych glebach kopalnych odsłonięcia

polanów samborzecki –  okolice sandomierza. pedogenetic processes in

palaeosols of the polanów samborzecki loesses exposure – vicinity of

sandomierz.

Abstract: The paper presents results of various pedological analyses

carried out in the exposure of loesses and alluvial deposits in Polanów

Samborzecki. The exposure is located in the embankment of River Vistula

in the vicinity of Sandomierz (SE Poland). During the study period its

length reached ca 150 m, and the top of the exposure was situated at 165

m above sea level, ca 20 m above the present-day Vistula valley.

Typologically and geochronologically different palaeosols, developed

from loesses or sandy loesses, underlain by older alluvia of River

Vistula, have been recognized and distinguished in three parts of the

exposure, based on their morphological, physical-chemical and

micromorphological features. The stratigraphy of the analysed loesses

has been based on the presence and typological development of soils

representing different ranges, i.e. on pedostratigraphy, where soils are

thus treated as formal lithostratigraphic units of the Quaternary.

Results of the analyses allowed to construct a scheme of palaeosol

occurrence in the study area (Fig. 1). The oldest soil is developed from

upper Wartanian loess during the Eemian Interglacial. This is incomplete

Albic Luvisol, overprinted with gley processes taking place at the end

of the interglacial. This soil lies on older alluvial deposits of the

Vistula. In its upper part occur the mollic horizon of interstadial

Glossic Chernozhem, developed from loess of the lowermost Vistulian,

deposited in completely different cool climatic conditions. Typically

both soils are distinguished as a palaeosol set, developed during the

Eemian Interglacial and Early Vistulian. However, in those cases where

the interstadial Albic Luvisol is better preserved, it is appropriate to

distinguish two separate soil units. From the lower younger loess

developed an interstadial, in some cases interphasal, Calcic Gleysol,

which disappears in part of the exposure. The youngest palaeosol, also

of interstadial origin, which developed from the middle younger loess,

is Gleyic Cambisol. Traces of gley processes can also be observed in

this case. In turn, from the upper younger loess, occurring on the

surface of the study area, Gleyic Cambisols or Albic Luvisols, and in

topographic lows – also Glossic Chernozhems developed. Interglacial

palaeopedologic processes of the Vistulian or Eemian Interglacial had a

similar course in comparison to the pedological processes of the

Holocene, which is treated here as an interglacial.

Słowa kluczowe: gleby kopalne, interglacjał eemski, procesy glebotwórcze.

Key words: palaeosols, Eemian Interglacial, pedogenetic processes.