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disa farm, values are remarkably lower, probably in connection with removals determined by crops typologies and by the homogenization of surface horizons, determined by periodical tillage activities. The pinewood soils are usually poorly or weakly calcareous at surface and became moderately or very calcareous in subsurface horizons. Said trend reveals a remarkable surface decarbonation, favoured by the coarse texture and by the consequent high permeability of these soils. The decarbonation process is also indicated by the pH trend, which is basically neutral or subacid at surface and turns into subalkaline or moderately alkaline at depth. The soils of both the public park and the farm appear very calcareous from the surface and become strongly calcareous at depth. Therefore in these soils the decarbonation process seems to be not so evident as against surface horizons, both due to the reduced permeability (finer textures) and to the rearrangement operated by man. Moreover the values of CaCO3 show a discontinuous trend in relation to depth, which is suggestive of subsequent sediments contributions, unlike what observed in almost all the pinewood soils. As a direct consequence of the elevated rates in CaCO3, the pH value of public park or farm soils prove to be weakly to strongly alkaline, with trends generally decreasing with depth, except for profile PER2 that shows non-linear trends. As to soils electrical conductivity (EC), table 2 shows that no salinization problems arise either in the public park soils or in the farm ones. However things are different inside the pinewood where a more articulated situation can be observed. Some soils have a widespread salinity all along the profile (PW3, PW5, PW7 and PW9); others only at surface (PW1), and some others absence of salinity (PW2, PW4, PW6 and PWN8). The electrical conductivity recorded in soils results to be, in said litoraneous environments, strongly related with the one of groundwater. Studies recently carried out in the same area (Zannoni, 2008; Buscaroli and Zannoni, 2009) clearly indicate how, in soils belonging to more elevated areas from a topographical point of view (PW2, PW4, PW6 and PW8), the stratum is located at such a depth as to determine any possible consequence on deep horizons only (beyond 1 m of depth) while not affecting the surface. In inter-dune depressions, where the water table is at lower depths, it can significantly affect the soils characteristics. In particular, when the water table is strongly characterized by salinity as in the case of profiles PW2, PW4, PW6 and PW8, the EC of the whole profiles turns out to be elevated. Moreover, during the summer period, to coincide with strong surface evapotranspiration phenomena, a large increase in surface horizons EC has been observed, mainly due to saline accumulations, which can be observed also in investigated profiles. Soils classification. Data gathered have made it possible to locate soils from a taxonomical point of view, according to what provided for in the Keys to soil taxonomy, 10 th edition (SSS, 2006), up to the family hierarchical level (table 3). 124
The soils of the San Vitale Pinewood fall into the Psamments suborder. Studies carried out in the same area (Zannoni, 2008; Buscaroli and Zannoni, 2009) have highlighted how, under conditions similar to those of profiles PW3, PW7 and PW9, values of Sodium Adsorption Ratio (SAR) and of Exchangeable Sodium Percentage (ESP) observed are such so as to make soils fall within the Sodic subgroup (SSS, 2006). Besides a strict taxonomic arrangement, the presence of soluble bases and even more their mutual relation (SAR) can substantially affect the flora development. With this respect, some authors (Álvarez-Rogel et al., 1997, 2007; Alaoui-Sossè et al., 1998) stress how, within environmental contexts similar to those under study, the variations in soils salinity are among the main variables in the diffusion of plant species. Other authors (Gerdol et al., 1985; Piccoli et al., 1991; Blaylock, 1994; Reinman and Breckle, 1995; Álvarez-Rogel et al., 2001) associate the presence of plant species to the relation of some ionic forms and to the soil S.A.R.. Profile Soil Survey Staff, 2006 PW1 TYPIC PSAMMAQUENTS, mixed, calcareous, mesic PW2 TYPIC USTIPSAMMENTS Mixed, calcareous, mesic PW3 SODIC PSAMMAQUENTS Mixed, calcareous, mesic PW4 AQUIC USTIPSAMMENTS Mixed, calcareous, mesic PW5 TYPIC PSAMMAQUENTS Mixed, calcareous, mesic PW6 AQUIC USTIPSAMMENTS Mixed, calcareous, mesic PW7 SODIC PSAMMAQUENTS Mixed, calcareous, mesic PW8 TYPIC USTIPSAMMENTS Mixed, calcareous, mesic PW9 SODIC PSAMMAQUENTS Mixed, calcareous, mesic GP1 UDIFLUVENTIC HAPLUSTEPTS Fine-silty, mixed, mesic GP2 UDIFLUVENTIC HAPLUSTEPTS Coarse-loamy, mixed, mesic PER1 UDIFLUVENTIC HAPLUSTEPTS Fine-loamy, mixed, superactive PER2 UDIFLUVENTIC HAPLUSTEPTS Fine-silty, mixed, superactive Conclusions 125 Table 3 – Classification of soil profiles (SSS, 2006) Chemical-physical pedologic surveys carried out on 13 soils profiles have made it possible to confirm the taxonomic definitions indicated in the pedologic delineations of the Emilia-Romagna region soil map (RER, 2009). The survey carried out in the San Vitale Pinewood, along two transepts located at right angles with the dune system, has highlighted such a close relation between microtopography, surface stratum depth and relevant saline concentration as to enable a taxonomic selection at subgroup level, within the Ustipsamments/Psammaquents complex (Fig. 2). In the specific instance, profiles PW2, PW4, PW6 and PW8 located in the highest spots of the dune structure suffer either moderately (Aquic Ustipsamments, PW4 and PW6) or not at all (Typic Ustipsamments, PW2 and PW8) the presence of the water-table.
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ALMA MATER STUDIORUM UNIVERSITA DI
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Preface This third volume of the "Q
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Analytic index / Index analytique /
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. Marina Gatti, Anna Flora Campanal
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Sessione/Session I. Air quality Qua
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Mots-clés: Caractérisation physic
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120 100 80 60 40 20 0 . 120 100 80
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na del materiale particellare atmos
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zione degli IPA sui gas direttament
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Discussion The Lichen Biodiversity
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values, even if quite different fro
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CONTI M.E., CECCHETTI G. (2001) Bio
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26
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irrigation. Le déplacement de la z
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ecorded by the use of a GPS and the
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There were observed seasonal variat
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The concentrations of copper in the
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VAN BENNEKOM A.J., SALOMONS W. (198
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d'échanges cationiques à l'interf
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Results The oxygen and hydrogen iso
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References 42 Figure 3 Distributi
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ésultant de la contamination par l
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At selected sites, sampling was car
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Moreover, this process is clearly r
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Fondazione Banco di Sardegna. Autho
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ive ouzbèke, est encore critique.
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cooperative enterprises; Sovkhoz we
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Kazakh and Uzbek cotton fields suff
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evaluation: if finished, it could p
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period such as a reduction of cotto
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PIASTRA S. (1992) «(...) no one ha
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distribuzione fuori commercio del l
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Risultati Alla fine, fu deciso di r
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Riferimenti bibliografici ARCHAIMBA
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Mots-clés : Rana perezi; asymétri
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FA values were higher in rice field
Page 74 and 75: POPE SE, FAHRIG L, MERRIAM NG. (200
Page 76 and 77: significatives, le but étant de co
Page 78 and 79: 78 Figura 3 Esempio di scala di de
Page 80 and 81: . 80 Figura-6 Tabelle statistiche
Page 82 and 83: 3. F. Reno a Casalecchio Tiro a Vol
Page 84 and 85: Conclusioni In linea generale, per
Page 86 and 87: Introduzione Il territorio imolese,
Page 88 and 89: La media-bassa vallata del Santerno
Page 90 and 91: 90 Figura 4 Vista dall’alto del
Page 92 and 93: coltivi, abitazioni e strade. Ridot
Page 94 and 95: mediterranee e semiaride hanno evol
Page 96 and 97: 96
Page 99 and 100: BEHAVIOR OF ORGANIC POLLUTANTS IN T
Page 101 and 102: végétale du sol et des propriét
Page 103 and 104: Figure 1 - Role of the soil in the
Page 105 and 106: for soils, it sums up at a total su
Page 107 and 108: Lupicka et al., 1997; Krzysko-Lupic
Page 109 and 110: glyphosate and metabolites in water
Page 111 and 112: KRUEGER J, PETERSON M, LUNDGREN E (
Page 113 and 114: WARNEMUENDE EA, PATTERSON JP, SMITH
Page 115 and 116: SOIL SURVEY AND CLASSIFICATION IN A
Page 117 and 118: aspects, linked with the destinatio
Page 119 and 120: The Luigi Perdisa farm, covering an
Page 121 and 122: Table 1 - (follows) Pro ile GP1 GP2
Page 123: C horizons that make up the parent
Page 127 and 128: ALLOWAY B.J., (1995) The origins of
Page 129 and 130: POTENTIALLY TOXIC ELEMENTS ALONG SO
Page 131 and 132: petrolchimico, ma anche soggetta ad
Page 133 and 134: quents). The extra urban farm ITAS
Page 135 and 136: soil and the background material wa
Page 137 and 138: .Comparison between total and pseud
Page 139 and 140: . . Figure 2a - Comparison of total
Page 141 and 142: total concentrations for (Ba, Cr, C
Page 143 and 144: Sr ISOTOPIC EVIDENCE FOR STUDYING T
Page 145 and 146: tively. A level of turf occurs at d
Page 147 and 148: Acknowledgment. Research co-finance
Page 149 and 150: PRELIMINARY RESULTS ON THE DISTRIBU
Page 151 and 152: mente un inquinamento di origine an
Page 153 and 154: profiles vary with respect to textu
Page 155 and 156: of PIN-3, being located to the nort
Page 157 and 158: plants. Besides metal chemical spec
Page 159 and 160: References ADRIANO D.C. (2001) Trac
Page 161 and 162: SOIL QUALITY ASPECTS IN THE REMEDIA
Page 163 and 164: elevata funzionalità anche i suoli
Page 165 and 166: Questa applicazione delle tecnologi
Page 167 and 168: TREND OF METAL AND METALLOID CONCEN
Page 169 and 170: (Pleistocene), caratterizzata da se
Page 171 and 172: L4 L3 PUNTI ETTARI DENSITA oss./ha
Page 173 and 174: elevati riscontrati nello stesso pu
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.SOIL AND LAND QUALITIES INFLUENCE
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Problematiche di conservazione dei
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colte sono state determinate utiliz
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e i vari fattori in gioco nel cambi
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CONTROL AND ANALYSIS ACTIVITIES ON
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totali) e dei limiti superiori per
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Bibliografia DECRETO LEGISLATIVO 3
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SOIL MICROARTHROPOD CONTRIBUTION TO
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zione fornita dall'ambiente ipogeo
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miorecettori. Queste strutture, che
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di comunità, la struttura di comun
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- non devono migrare su lunghe dist
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TRACE ELEMENTS IN FRUIT AND VEGETAB
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with trace metal may be due to irri
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chronic hazards. In addition the da
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SOIL DEPLETION DUE TO URBANISATION
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207
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Table 1 - Soil types present in the
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Soil delineations Surface in hectar
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Approximately 3.5% of the soil surf
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MINERAL HORIZONS, ELECTROMAGNETIC F
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slope movements, the flows of the m
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Materials and methods The research
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are under higher pressure, the valu
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