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Fig. 3. Soil microbial respiration versus oxygen concentration for a meadow loamy soil (3- 7 cm clods) from a depth of 5-15 cm, at soil pore water pressure –11 kPa. 1 – first day after sampling, 2 – second day after sampling (from unpublished data of J. W. Bakker and W. Stępniewski). Fig. 4. Final emergence of oats versus oxygen diffusion rate (ODR). Modified from Gliński, Stępniewski, £abuda and Przywara, Roczn. Glebozn., 35, 3, 1984. 46
Fig. 5. Hatching percentages of Centropages hamatus eggs versus oxygen concentration in sea water (The incubation was performed in sea water oxygenated for 11 days). Modified from Lutz et al. 1992. REFERENCES 1. 2. 3. 4. 5. Gliński J., Stępniewski W. 1985 Soil Aeration and its Role for Plants. CRC Press, Boca Raton, Florida. Gliński J., Stępniewski W., Łabuda S., and Przywara G. 1984. Threshold values of ODR and Eh in soil for the emergence of cultivated plants. (in Polish with English summary). Roczn. Glebozn., 35, 3. Lutz R. A. et al. 1992 Marine Biology, 114, 241-247. Patrick W. H., Mikkelsen D. D. 1971. Plant Nutrient Behaviour in flooded soil. in Feritilizer Technology and Use. 2nd ed, Soil Science Society of America, Madison, Wisc. 187. Stępniewski W., Stępniewska Z. 1998. Oxygenology as a new discipline in the environmental sciences - a proposal for discussion. Intern. Agrophysics, 12, 53-55. 47
Page 2 and 3: Jan Gliński, Grzegorz Józefaciuk,
Page 4 and 5: CONTENTS PART A: GAS EXCHANGE Revie
Page 6 and 7: SOIL - PLANT - ATMOSPHERE AERATION
Page 8 and 9: In single observations, rates of N
Page 10 and 11: than in the night while CH 4 uptake
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 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 60 and 61: tics (Stępniewski et al., in press
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
Page 110 and 111:
mination, should be considered.The
Page 112 and 113:
Considering a possibility of detect
Page 114 and 115:
SURFACE PROPERTIES OF SOILS AND THE
Page 116 and 117:
clay content the latter processes p
Page 118 and 119:
der alkaline treatment the silica o
Page 120 and 121:
COMPACTION EFFECTS ON SOIL PHYSICAL
Page 122 and 123:
suming and expensive regression-bas
Page 124 and 125:
CROP RESPONSE Roots A characteristi
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CONCLUSIONS Alterations in the aggr
Page 128 and 129:
27. Keller, T., Arvidsson, J., Dawi
Page 130 and 131:
MONITORING OF POROUS MEDIA PROCESSE
Page 132 and 133:
- temperature: semiconductor, therm
Page 134 and 135:
This is the reason why the optimisa
Page 136 and 137:
CONCEPTS AND MORPHOLOGY OF HYDROMOR
Page 138 and 139:
conditions applied to the soil samp
Page 140 and 141:
ESTIMATION OF THE HYDROPHYSICAL CHA
Page 142 and 143:
Fig. 6. Scheme of EURO-ACCESS-II mo
Page 144 and 145:
The experimental field is located a
Page 146:
Nannipieri Paolo Ostrowska Aneta Os
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