tics (Stępniewski et al., in press). On the basis of analysis of t 300 values determined in 4 temperatures (4, 10, 15 and 20°C) for 3 subsequent <strong>soil</strong> horizons, 4 homogenic <strong>soil</strong> groups were distinguished and mapped for the whole country: <strong>soil</strong>s with inconsiderable (
inventories and options for control proceedings. Ed. Van Amstel AR. Natl. Inst. Public Health and Environ. Prot ., Bilthoven, The Netherlands, 343-346. 12. Ostrowski J., Sławiński C., Walczak R.: Ocena i kartograficzna prezentacja wrażliwości gleb ornych na hydrooksygeniczną degradację. Evaluation and cartographic presentation of arable <strong>soil</strong>s sensibility to hydrooxygenic degradation. in press. 13. Ostrowski J., Stępniewska Z., Stępniewski W., Gliński J. 1998: Computer maps of the redox properties of arable <strong>soil</strong>s in Poland. J. Water and Land Development, 2, 19-29. 14. Patrick I., Jugusjinda A. 1992: Sequential reduction and oxidation of inorganic nitrogen, manganese and iron in flooded <strong>soil</strong>. Soil Sci. Soc. Am. J. 56, 1071-1073. 15. Pedrazzini F.R., Moore P.A. 1983: N 2 O Emission and changings of redox potential and pH in submerged <strong>soil</strong> samples. Zeitschrift für Pflanzenennernahrung und Bodenkunde, 146, 660-66. 16. Spier T.W., Kettles H.A., More R.D. 1995: Aerobic emission of N 2 O and N 2 from <strong>soil</strong> cores. Measurement procedures using 13 Nlabelled NO 3 and NH 4 . Soil Biol. Bioch. 27, 1289-1298. 17. Stawiński J., Gliński J., Ostrowski J., Stępniewska Z., Sokołowska Z., Bowanko G., Józefaciuk G., Księżopolska A., Matyka-Sarzyńska D. 2000: Spatial characterization of specific surface area of arable <strong>soil</strong>s in Poland in Polish. Acta Agrophysica 33, pp. 52. 18. Stępniewska Z. 1988: Właściwości oksydoredukcyjne mineralnych gleb Polski. Problemy Agrofizyki, Nr 56. 19. Stępniewska Z., Ostrowski J., Stępniewski W., Gliński J.: Klasyfikacja ocen odporności oksydoredukcyjnych gleb ornych Polski i ich przestrzenna charakterystyka. Classification of redox resistance evaluation of Polish arable <strong>soil</strong>s and their spatial characteristics. in press. 20. Stępniewska Z., Stępniewski W., Gliński J., Ostrowski J. 1997: Atlas of the redox properties of arable <strong>soil</strong>s in Poland. Institute of Agrophysics, <strong>Lublin</strong> and IMUZ, Falenty, Poland. 21. Van Cleemput O., Patrick W.H., Mc Ilhenny R.C. 1976: Nitrite decomposition in flooded <strong>soil</strong> under different pH and redox potential conditions. Soil Sci. Soc. Am. J. 40, 55-60. 22. Walczak R., Ostrowski J., Witkowska-Walczak B., Sławiński C. 2002: Hydrophysical characteristics of mineral arable <strong>soil</strong>s in Poland in Polish. Acta Agrophysica 79, pp. 95. 23. Yu Tian-Ren 1985: Physical Chemistry of Paddy Soils. Science Press. Beijing Springer-Verlag. Berlin. 64
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Jan Gliński, Grzegorz Józefaciuk,
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CONTENTS PART A: GAS EXCHANGE Revie
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SOIL - PLANT - ATMOSPHERE AERATION
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In single observations, rates of N
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- Page 12 and 13: Pumpanen et al. (2003b) measured wi
- Page 14 and 15: 5. Liikanen A 2002. Greenhouse gas
- Page 16 and 17: EFFECT OF SOIL TILLAGE AND COMPACTI
- Page 18 and 19: Cumulative CO 2 (kg C ha -1 ) 600 F
- Page 20 and 21: Soil depth (mm) 0 20 40 60 80 Diffu
- Page 22 and 23: METHANE Main suppliers to the atmos
- Page 24 and 25: 3. Emission of N 2 O is higher from
- Page 26 and 27: 30. Kusa, K., Sawamoto, T., Hatano,
- Page 28 and 29: GAS EMISSION FROM WETLANDS Stępnie
- Page 30 and 31: ater retention capacity in the chan
- Page 32 and 33: zone, while in Nadrybie lake the le
- Page 34 and 35: Eh 350 300 250 mV 200 150 100 50 0
- Page 36 and 37: Table 1. Sources and sinks of atmos
- Page 38 and 39: Fig. 1. Quasi - equilibrium methane
- Page 40 and 41: Fig. 5. Concentration of nitrous ox
- Page 42 and 43: drooxygenology, such subbranches as
- Page 44 and 45: Fig. 3. Soil microbial respiration
- Page 46 and 47: NITROUS OXIDE EMISSION FROM SOILS W
- Page 48 and 49: N2O-N [mg kg -1 ] 100 80 60 40 20 0
- Page 50 and 51: 7. McKenney, D.J., C.F. Drury, and
- Page 52 and 53: AERATION STATUS OF SOIL AND ENZYME
- Page 54 and 55: Catalase is heme-containing enzyme
- Page 56 and 57: 8. Deng S., Dick R. Sulfur oxidatio
- Page 58 and 59: The number of profiles representing
- Page 62 and 63: MICROBIAL ECOLOGY OF SOIL POROUS ME
- Page 64 and 65: The bulk of non-rhizosphere soil is
- Page 66 and 67: RELATIONS The relations between soi
- Page 68 and 69: 23. Mamilov A.Sh., Byzov, B.A. Zvya
- Page 70 and 71: silts. The content of C org in the
- Page 72 and 73: Table 2. Continued Location Day of
- Page 74 and 75: 5 o C Eh (mV 400 300 200 100 1A 1B
- Page 76 and 77: STRUCTURE FORMATION AND ITS CONSEQU
- Page 78 and 79: when water content differences are
- Page 80 and 81: authors stated that O 2 gradients i
- Page 82 and 83: strength of the already existing st
- Page 84 and 85: source of transforming DNA for Acin
- Page 86 and 87: THE BIOCHEMISTRY OF THE RHIZOSPHERE
- Page 88 and 89: der field conditions r-strategists
- Page 90 and 91: 22. Tarafdar JC and Jungk A 1987. P
- Page 92 and 93: ics behavior have been published (K
- Page 94 and 95: Activity of dehydrogenase (DHA) was
- Page 96 and 97: The rather small concentration of A
- Page 98 and 99: The effect of the pesticide dosage
- Page 100 and 101: METHANOTROPHIC ACTIVITY OF COAL MIN
- Page 102 and 103: GC TESTS Air-tight bottles (60 ml)
- Page 104 and 105: dumping. For older rock samples, af
- Page 106 and 107: SOIL - PLANT - ATMOSPHERE AERATION
- Page 108 and 109: - properties of plant surface and c
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mination, should be considered.The
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Considering a possibility of detect
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SURFACE PROPERTIES OF SOILS AND THE
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clay content the latter processes p
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der alkaline treatment the silica o
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COMPACTION EFFECTS ON SOIL PHYSICAL
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suming and expensive regression-bas
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CROP RESPONSE Roots A characteristi
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CONCLUSIONS Alterations in the aggr
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27. Keller, T., Arvidsson, J., Dawi
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MONITORING OF POROUS MEDIA PROCESSE
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- temperature: semiconductor, therm
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This is the reason why the optimisa
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CONCEPTS AND MORPHOLOGY OF HYDROMOR
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conditions applied to the soil samp
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ESTIMATION OF THE HYDROPHYSICAL CHA
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Fig. 6. Scheme of EURO-ACCESS-II mo
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The experimental field is located a
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Nannipieri Paolo Ostrowska Aneta Os