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Marinari, S.; Papp, R.; Sripada, U.; Thami-Alami, I.; Campiglia, E.; Pearce, B.D.; Bergkvist, G.; van der Heijden, M.; Baresel, J.P.; Finckh, Maria R.. |
Soil properties at the beginning of the MEE (Multi Environment Experiments) were statistically analyzed in order to verify the field homogeneity. The initial soil properties represent the starting point to interpret the effect of CC and LM on soil fertility during crop cycle.Soil properties of the fields were quite homogeneous at the beginning of crop cycles (first and second). The soil properties of the experimental fields in the selected areas showed a wide variety of pedons to be used for the comparison of CC and LM effect in different climate zones. Soils from the Northern European sites are more acid and richer of nutrients and organic matter with respect to the soils in Southern sites. |
Tipo: Conference paper, poster, etc. |
Palavras-chave: Soil quality; Soil biology; Nutrient turnover. |
Ano: 2014 |
URL: http://orgprints.org/29641/1/poster%20OSCAR%201.pdf |
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Marinari, S.; Papp, R.; Sripada, U.; Thami-Alami, I.; Campiglia, E.; Pearce, Bruce; Bergkvist, Göran; van der Heijden, Marcel; Baresel, Jörg Peter; Finckh, Maria R.. |
Soil chemical properties were correlated with microbial biomass and its activity. Different correlations were found at the beginning of the first and second cycles, respectively. Soil samples were grouped with respect to the different climate zones. The main variables that separated the countries were organic Carbon, total Nitrogen, pH and clay content. |
Tipo: Conference paper, poster, etc. |
Palavras-chave: Soil biology; Nutrient turnover; Soil. |
Ano: 2016 |
URL: http://orgprints.org/29643/1/poster%20OSCAR%202.pdf |
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Marinari, S.; Liburdi, K.; Fliessbach, A.; Kalbitz, K.. |
In this study we tested the hypothesis that water-extractable organic carbon (WEOC) content and its properties can be used to distinguish conventionally (CONV) from organically (ORG) managed arable soils as responsible for C mineralization. We sampled soils at three different European sites located in Mediterranean (Italy) and continental (Switzerland) regions under conventional and organic management. The Mediterranean sites are here called CVI and LSI and the continental one DOK. The main difference between the two management systems (ORG and CONV) at all sites was the amount of organic fertilizer yearly added into the soil: in the ORG systems 2.2–2.5 Mg C year−1 were added as organic fertilizer, while in the CONV systems only mineral fertilizers were... |
Tipo: Journal paper |
Palavras-chave: Soil biology. |
Ano: 2010 |
URL: http://orgprints.org/17862/1/Marianari%2Detal%2D2010%2Delsevier.pdf |
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