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AGRONOMIJAS VĒSTIS (Latvian Journal of Agronomy), No.10, LLU, 2008values of BOD t and active carbon C hws , and of the values determining the aerobic and anaerobicstability of soil organic matter, i.e. means of the rate constant of biochemical oxidation K andanaerobic degradability D CHOD . The critical value α crit is still too high to prove a statisticallysignificant correlation. Therefore the results are not presented (Eckschlager et al., 1980).Table 3 shows the results of degradability of organic matter of samples in anaerobicconditions. It documents theoretical substrate production of methane TV CH4S derived from CHODand substrate production of methane V CH4S calculated from the measured production of CH 4 in thetest apparatus Oxi Top Control AN 12 Merck in accordance with ISO CD 11734 after subtractionof endogenous production of CH 4 by the inoculum added to test flasks. The anaerobic degradabilityof organic matter of samples of organic and organomineral horizons is expressed in % as D CHOD . Sowe transferred our investigation to comfortable work with CHOD, but as mentioned above in thetheoretical part, even if the Oxi Top Control AN 12 Merck apparatus is not available, it is possibleto determine organic matter degradability in anaerobic conditions, though less exactly, from theratio of carbon in the produced volume of biogas in an alternative apparatus to the organic carboncontent of the sample at the beginning of the test. Because in these alternative apparatuses it is notusually possible to determine the numbers of CO 2 moles in the gaseous and liquid phase andnumbers of CH 4 moles, and of these values the total number of moles of transformed carbon, wework only with the substrate production of biogas V BPS . The results are only approximate, and it isnecessary to decide whether the orientation values are acceptable with regard to the considerableacceleration of the work.Table 3. Theoretical substrate production of methane TV CH4S , substrate production of methaneC CH4S , anaerobic degradability of organic matter D CHOD in samples of organic and organomineralsurface horizons. Calculated values (D CHOD ) mol and difference D CHOD – (D CHOD ) molParametrs A t O f F a T sTV CH4S , l.g -1 (101.3 kPa, 35°C) 0.30 0.40 0.43 0.31V CH4S , l.g -1 0.0043 0.0087 0.0206 0.0019D C , % 1.45 2.17 4.81 0.60(D CHOD ) mol 1.43 2.14 4.80 0.59D CHOD – (D CHOD ) mol 0.02 0.03 0.01 0.01The last value (D CHOD ) mol in Tab. 3 is the value that was not derived from the methane volume at101.3 kPa and 35º C but from the calculated numbers of produced CH 4 moles converted to CHOD.The difference between this value and D CHOD shows the existence of some differences but the erroris negligible.The values in Tab. 2 and 3 document an important fact that there is no relationship betweenthe aerobic and anaerobic degradability of SOM of organic and organomineral soil horizons, whichwe did not assume at the beginning of our study.ConclusionsIn the analyzed samples no relationship between the aerobic and anaerobic stability of theirorganic matter was found; nor the expected relationship between total biochemical oxygen demandand “active carbon” C hws was proved.This study was supported by project No. MSM 6007665806 of the Ministry of Education, Youthand Sport of the Czech Republic.References1. Capriel, P., Beck, T., Borchert, H., Gronholz, J., Zachmann, G. (1995) Hydrophobicity of the organicmatter in arable soils. Soil Biology and Biochemistry, 27, 1453-1458.2. Eckschlager, K., Horsák, I., Kodejš, Z. (1980) Evaluation of analytical results and method. SNTL Pragueand ALFA Bratislava, CZ.-223.3. Horáková, M., Lischke, P., Grünwald, A. (1989) Chemical and physical method of water analysis. SNTLPrague, CZ.-389.4. ISO CD 11734. Water quality – Evaluation of the “ultimate” anaerobic biodegradability of organiccompounds in digested sludge – Method by measurement of the biogas production. CZ.-2050
AGRONOMIJAS VĒSTIS (Latvian Journal of Agronomy), No.10, LLU, 20085. Kolář, L., Kužel, S. (1999) Organic matter in soil. In: Balík J. (eds) Reasonable using of fertilizer.International conference CAU Prague CZ, 15-19.6. Kolář, L., Klimeš, F., Ledvina, R., Kužel, S. (2003) A method to determine mineralization kinetics of adecomposable part of soil organic matter in the soil. Plant Soil Environment, 49, (1), pp. 8-11.7. Kolář, L., Kužel, S., Hanušová, A., Gergel, J., Ledvina, R., Šindelářová, M., Silovská, Š., Štindl, P. (2005a) The use of Spectroquant Merck BOD photometric test to evaluate the stability of organic matters in soil.Plant, Soil and Environment, 51, (1), 46-50.8. Kolář L., Klimeš F., Gergel J., Kužel S., Kobes M., Ledvina R., Šindelářová M. (2005 b) Methods toevaluate substrate degradability in anaerobic digestion and biogas production. Plan, Soil and Environment,51, (4), 173-178.9. Kolář, L., Ledvina, R., Kužel, S., Klimeš, F., Štindl, P. (2006) Soil organic mater and its stability inaerobic and anaerobic conditions. Soil and Water Research, 1, (2), 57-64.10. Körschens, M., Schulz, E., Böhm, R. (1990) Heisswasserlöslicher C und N im Boden als Kriterium fürdas N-Nachlieferungsvermögen. Zentralblatt für Mikrobiologie, Jena, 145, (4), 305-311.11. Kužel, S., Kolář, L., Ledvina, R., Spalevič, V. (2001) Transformation Soil organic matter in mountainand submountain regions of Šumava in Comparison with České Budějovice basin. In: Zaujec A., Bielek P.,Gonet S.S., (eds) Humic substances in ecosystems. The 4 th International conference SAU Nitra, SSCRIBratislava, UTA Bydgoszcz, SK, 79-83.12. Němeček, J. (2001): Taxonomical classificatory system of soil Czech Republic. CAU Prague, RIMSPPrague, CZ.-78 s.13. Schulz, E. (1990) Die heisswass erextrahierbare C-Fraktion als Kenngröse zur Einschätzung desVersorgungszustands mit organischer Substanz.. Tag.-Ber., Akad. Landwirtsch. Wis., Berlin, 295, 269-27514. Süssmuth, R., Doser, Ch., Lueders, T. (1999) Determination of the biological biodegradability of organicsubstances under anaerobic conditions using the Oxi Top Control measuring system. Appl. rep. 0600412 e,Universität Hohenheim, Inst. für Mikrobiologie, Wissenschaftlich-Technische Werkstäten GmbH & Co., KGWeilheim, D.-2015. Štindl, P., Hrušková-Silovská, Š., Kolář, L., Kužel, S. (2005) Stanovení rozložitelnosti organické hmoty.Sborník z mezinárodního semináře „Nepotravinářské využití fytomasy“, SBU České Budějovice, 86-92,16. Weigel, A., Kubát, J., Körschens, M., Powlson, D., Mercik, S. (1998) Determination of thedecomposable part of soil organic matter in arable soils. Archiv fuer Acker- und Pflanzenbau undBodenkunde, 43, 123-143THE CHOICE OF THE DIFFERENTIATION CRITERIA OF SOIL TILLAGEUSING THE GEOGRAPHIC INFORMATION SYSTEM (GIS)Lapins D., Vilde A., Berzins A., Plume A. and Dinaburga G.Latvia University of Agriculture, 2 Liela Street, Jelgava, Latvia, LV-3001phone: +371 63005632, e-mail: Dainis.Lapins@llu.lvKopsavilkumsLatvijas zemnieku saimniecībās pēdējos gados parādās precīzās lauksaimniecības elementiun vispirms labību kombainu aprīkojums ražu karšu veidošanai. Nākošā etapa: ražu kartesizmantošana saistīta vispirms ar augšĦu īpašību izpēti. (Vilde, LapiĦš et al. 2005). Tas nozīmē, kasaimniecībās jāveido sava lokālā ăeogrāfiskās informācijas sistēma. AugšĦu īpašību izpētesmateriāli ir kā bāze diferencētas, uz ĂIS bāzētas resursus taupošās augsnes apstrādes ieviešanai.Latvijā jau iepriekšējos gados ir veikti pētījumi par augsnes apstrādes pasākumu optimizēšanasiespējām, lietojot GPS (Lapins, Vilde, Berzins, et. al., 2006). Pētījumu rezultātu analīzes mērėis irsistematizēt iegūto datu materiālu un ieteikt augsnes apstrādes diferences kritērijus, lietojot lokālāssaimniecības ăeogrāfiskās informācijas sistēmas.LLU MPS "Vecauce" „Kurpnieku” masīvā 47 stacionāros novērojuma punktos ražošanassējumos 2004. - 2006.g. veikti pētījumi par faktoru ietekmi uz ziemas kviešu ražu. Meteoroloăiskieapstākli abos gados bija atšėirīgi: 2005.g. raksturojās ar pazeminātām vidējām gaisa temperatūrām,bet 2006.g. – ar izteikti zemu nokrišĦu daudzumu un līdz ar to arī mitruma deficītu augsnē.Skaidrotas augsnes apstrādes diferences iespējas saistībā ar augšĦu īpašību raksturojumu.Koordinātu noteikšanā izmantota GPS. Ražu noteica ar Claas Lexion 420 GPS izveidotām ražukartēm, lietojot AGROCOM programmatūru. Kā ražu ietekmējošie faktori pētīti augsnes A51
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