Onttojen puiden lahopuukovakuoriaiset — kolmen pyydystyypin vertailu

Vanhat ja ontot puut ovat tärkeä elinympäristö monelle lahopuusta riippuvaiselle eliölajille. Onttoihin puihin on erikoistunut suuri määrä myös vaarantuneita ja harvinaisia hyönteislajeja, jotka elävät puun onkalon seinämillä tai onkalon pohjalle kerääntyvässä orgaanisessa aineksessa, ns. mulmissa. Tutkimuksen tavoitteena oli selvittää, mikä kolmesta pyydystyypistä (ikkuna-, vuoka- ja kuoppapyydys) soveltuu parhaiten onttojen puiden lahopuukovakuoriaisten pyyntiin. Lisäksi tavoitteena oli kartoittaa hyönteisnäytteiden ensimmäiseen laboratoriokäsittelyyn vaadittua aikaa. Tutkimuksessa oli mukana vanhoja rungostaan onttoutuneita lehmuksia, tammia ja vaahteroita pääkaupunkiseudun puisto- ja kartanoalueilta. Puiden onkaloiden sisään aseteltiin ikkuna-, vuoka- ja kuoppapyydyksiä, kaksi kutakin tyyppiä ja ne tyhjennettiin kolmen viikon välein touko-heinäkuussa 2006. Pyydyksiä oli siis yhteensä 90 per pyyntijakso. Kun näytteistä eroteltiin halutut hyönteislahkot (mukaanlukien kovakuoriaiset) niiden käsittelyyn käytetty aika kirjattiin ylös. Aineistosta tunnistettiin yhteensä 3825 kovakuoriaisyksilöä ja 212 lajia, joista lahopuusta riippuvaisia oli yhteensä 3398 yksilöä ja 121 lajia. Ikkunapyydyksissä esiintyi yhteensä 1639 yksilöä ja 140 lajia, vuokapyydyksissä 1506 yksilöä ja 134 lajia, kuoppapyydyksissä 680 yksilöä ja 111 lajia. Näytteiden käsittelyaikojen keskiarvot olivat 48,3 minuuttia ikkunapyydykselle, 65,5 minuuttia vuokapyydykselle ja 34,1 kuoppapyydykselle. Lajistokoostumuksen huomioiva ?-diversiteetti erosi huomattavasti pyydysten välillä, se oli 36,5 % ikkuna- ja vuokapyydysten välillä, 13,1 % ikkuna- ja kuoppapyydysten välillä ja 14,2 % vuoka- ja kuoppapyydysten välillä. Ikkuna- ja vuokapyydysten välillä ei havaittu tilastollisesti merkitsevää eroa saproksyylilajien (p<0,05), -yksilöiden (p<0,05) tai käsittelyaikojen (p<0,05) keskiarvoissa. Ikkuna- ja vuokapyydyksillä saatiin keskimäärin selvästi enemmän saproksyylilajeja ja –yksilöitä kuoppapyydykseen verrattuna. Kuoppapyydyksellä saatiin kokonaisyksilömäärään verrattuna suhteellisesti vähemmän saproksyylejä (59 %) kuin ikkuna- (69 %) ja vuokapyydyksillä (71 %). Ikkunapyydykset olivat tehokkain pyydystyyppi vertailtaessa pyydysten keräämää saproksyyliyksilömäärää suhteessa aineiston käsittelyn vaatimaan aikaan. Tehokkuus (yksilöä minuutissa) ikkunapyydykselle oli 0,74, vuokapyydykselle 0,43 ja kuoppapyydykselle 0,21. Ikkunapyydyksiä ei ole aikaisemmin käytetty puun onkalon sisällä hyönteisiä pyydettäessä vaan ne ovat aikaisemmissa tutkimuksissa roikkuneet onkalon ulkopuolella. Ikkunapyydykset kuitenkin toimivat erinomaisesti myös onkaloiden sisällä. Ikkuna- sekä vuokapyydys toimivatkin selkeästi paremmin lahopuukovakuoriaisten pyynnissä verrattuna kuoppapyydykseen, jonka poisjättäminen olisi kuitenkin tuottanut huomattavasti lajiköyhemmän aineiston. Mahdollisimman monimuotoisen onttojen puiden lahopuukovakuoriaislajiston keräämiseksi tulisi käyttää ikkuna- tai vuokapyydyksiä yhdessä kuoppapyydysten kanssa.

Análisis de la capacidad de acumulación de agua de diferentes especies de hojarasca en relación con la intercepción arbórea.

En el presente estudio se aborda la problemática de la capacidad de acumulación de agua de hojarasca de 4 especies arbóreas (Quercus robur, Fagus sylvatica, Pinus radiata y Pinus sylvestris). Se realizaron experimentos en el laboratorio de mojado y secado de la hojarasca para determinar su capacidad máxima de retención de agua. Así como experimentos de campo en los que se colocaron las muestras bajo copas de diferentes árboles (P.radiata y Q.robur) y en claros para determinar el efecto de la intercepción arbórea en la capacidad acumulativa de la hojarasca. Tanto los resultados del laboratorio como los de campo mostraron que la hojarasca que mayor capacidad de acumulación tiene es la de haya (F. sylvatica). Sin embargo aparecen diferencias entre los valores del pino entre ambos experimentos lo cual indica que, por encima de la masa de la hojarasca, es la profundidad de la capa lo que determina la capacidad de acumulación. Asimismo se observan diferencias significativas en la acumulación de agua dependiendo bajo que tipo de dosel se encuentre la hojarasca, siendo bajo pino donde se produce una mayor acumulación; lo que sugiere que el dosel cambia las características de la precipitación afectando a la capacidad de acumulación de la hojarasca.

Intercepción de la lluvia del dosel arbóreo y la hojarasca

[es]La intercepción de la lluvia, tanto por el dosel como por la hojarasca, es un proceso importante que influye en las condiciones de humedad del suelo, ya que una parte vuelve mediante evaporación a la atmosfera. Por lo tanto el objetivo de este estudio es profundizar más en el conocimiento de la capacidad de almacenaje e intercepción de los robles (Quercus robur) y en especial analizar si el tamaño de los árboles influye la intercepción. El estudio se llevo a cabo en dos robledales diferenciados por su tamaño durante tres estaciones del año: otoño, invierno y primavera (2014-2015) en las que se obtuvieron medidas de intercepción del dosel de la precipitación. También se obtuvieron muestras de hoja verde y hojarasca con objeto de calcular su capacidad máxima de retención de agua. Los resultados mostraron que el tamaño de los árboles es una característica que influye en el Índice de área foliar (LAI), y por tanto en la intercepción, pero que su efecto parece ser menos importante que el efecto causado por la variabilidad del volumen de lluvia. Del mismo modo, la intercepción relativa (en relación al volumen de lluvia) dependió de la interacción entre la estacionalidad y el tamaño de los árboles. Finalmente, la cantidad máxima de almacenamiento de agua fue mayor en la hojarasca que en la hoja verde, siendo mayor en el robledal de mayor tamaño al presentar significativamente mayor cantidad de hojarasca acumulada.

Biological parameters and glomalin levels as quality indicators in a soil implanted with exotic forest species in Argentine Patagonia

p.83-88

Bursaphelenchus pinophilus Brzeski & Baujard, 1997 (Nematoda: Parasitaphelenchinae) associated with nematangia on Pityogenes bidentatus (Herbst, 1783) (Coleoptera: Scolytinae), from the Czech Republic

The occurrence of Bursaphelenchus species in the Czech Republic is poorly known, the first report of the genus being made by Kubátová et al. (2000) who reported the association of B. eremus with the hyphomycetous microfungus, Esteya vermicola, and the bark beetle, Scolytus intricatus, collected from Quercus robur, in central Bohemia. To date, four other species have been reported from the country, namely B. fungivorus (Braasch et al., 2002), B. hofmanni (see Braasch, 2001), B. mucronatus (see Braasch, 2001) and B. vallesianus (Gaar et al., 2006). More recently, a survey for Bursaphelenchus species associated with bark- and wood-boring insects in the Czech Republic identified B. pinophilus Brzeski & Baujard, 1997 from the Moravia region. Although this represents a new country record, it was also associated with nematangia on the hind wings of a new insect vector. A total of 404 bark- and wood-boring insects were collected from declining or symptomatic trees and screened for the presence of Bursaphelenchus. Bark and longhorn beetles were captured manually after debarking parts of the trunk displaying symptoms of insect attacks. Longhorn beetle larvae were also collected together with logs cut from the trunk. Logs were kept at room temperature in the laboratory until insect emergence. Each adult insect was individually dissected in water and examined for nematodes. All nematodes resembling dauer juveniles of Bursaphelenchus were collected and identified by molecular characterisation using a region of ribosomal DNA (rDNA) containing the internal transcribed spacer regions ITS1 and ITS2. ITS-RFLP analyses using five restriction enzymes (AluI, HaeIII, HinfI, MspI, RsaI) were performed to generate the species-specific profile according to Burgermeister et al. (2009). Species identification was also confirmed by morphological data after culture of the dauers on Botrytis cinerea Pers. ex Ft., growing in 5% malt extract agar. During this survey, only species belonging to the Curculionidae, subfamily Scolytinae, revealed the presence of nematodes belonging to Bursaphelenchus. Dauers of this genus were found aggregated under the elytra in nematangia formed at the root of the hind wings (Fig. 1). The dauers were identified from 12 individuals of Pityogenes bidentatus (Herbst, 1783) (Coleoptera: Scolytinae) collected under the bark of Pinus sylvestris trunks. Each insect carried ca 10-100 dauers. The ITS-RFLP patterns of the dauers so obtained confirmed the identification of B. pinophilus associated with this insect species. Bursaphelenchus pinophilus has been found mainly in Europe and has been reported from various countries such as Poland (Brzeski & Baujard, 1997), Germany (Braasch, 2001), and Portugal (Penas et al., 2007). The recent detection of this species associated with dead P. koraiensis in Korea (Han et al., 2009) expands its geographical distribution and potential importance. It has been found associated only with Pinus species, but very little is known about the insect vector. The bark beetle, Hylurgus ligniperda, was initially suggested as the insect vector by Pe-nas et al. (2006), although the nematode associated with this insect was later reclassified as B. sexdentati by morphological and molecular analysis (Penas et al., 2007). According to the literature, P. bidentatus has been cited as a vector of Ektaphelenchus sp. (Kakuliya, 1966) in Georgia, and an unidentified nematode species in Spain (Roberston et al., 2008). Interestingly, B. pinophilus was found in the nematangia formed at the root of the hind wings of P. bidentatus. Although this phenomenon is not so common in other Bursaphelenchus species, B. rufipennis has been found recently in such a structure on the hind wings of the insect Dendroctonus rufipennis (Kanzaki et al., 2008). Although other nematode species (e.g., Ektaphelenchus spp.) are frequently found associated within the same nematangia (see Kanzaki et al., 2008), in this particular case, only dauers of B. pinophilus were identified. The association between B. pinophilus and P. bidentatus represents the first report of this biological association and the association with the Scolytinae strengthens the tight and specific links between this group of Bursaphelenchus species and members of the Scolytinae (Ryss et al., 2005).

Spechte als ökologische Indikatoren in Natur- und Wirtschaftswäldern im Bialowiera-Wald (Ostpolen)

Die vorliegende Untersuchung analysiert die Eignung der "Spechtgemeinschaft" als ökologische Indikatorengruppe und formuliert vor dem Hintergrund der Ergebnisse Forderungen und Empfehlungen für einen "spechtgerechten" Umgang mit Wäldern. Die Habitatnutzung von sieben Spechtarten beim Nahrungserwerb wurde über einen Zeitraum von zwei Jahren in urwaldartigen und forstlich genutzten Beständen verschiedener Waldgesellschaften systematisch beobachtet. Das Untersuchungsgebiet ist der Bialowieza-Wald im äußersten Osten Polens, wo in enger räumlicher Nachbarschaft Natur- und Wirtschaftswaldflächen bearbeitet werden konnten. Die Beobachtungen erfolgten zwischen Anfang März 1999 und Ende Februar 2001 und wurden zu allen Jahreszeiten durchgeführt. Vier der insgesamt sechs Probeflächen repräsentieren die wichtigste Laubwaldgesellschaft des Gebietes, das Tilio-Carpinetum, die übrigen zwei die wichtigste Nadelwaldgesellschaft, das Peucedano-Pinetum. Die Hälfte der zwischen 42 und 54 ha großen Probeflächen lag im streng geschützten Urwaldreservat des Bialowieza-Nationalparkes, die übrigen in forstlich genutzten Waldbeständen. Zusätzlich wurde ein 2,5 km langes Transekt durch bewirtschafteten Erlen-Eschen-Auenwald und sehr naturnahen Erlenbruch bearbeitet. Die Probeflächen wurden in ein Raster aus 50x50m großen Quadranten unterteilt. Zur Beobachtung der Spechte beim Nahrungserwerb erfolgten 21 Begehungen je Probefläche bzw. Transekt. Die Probeflächen wurden dazu auf parallelen Linien mit Abständen von je 100m begangen, Startpunkt und Startrichtung wurden variiert. Zur Charakterisierung der Vegetation und Bestandesstruktur erfolgten Erhebungen zur Baumartenzusammensetzung, Größenklassenverteilung der Bäume, Totholzanteil und Krautvegetation. 1332 Beobachtungen von Spechten beim Nahrungserwerb konnten ausgewertet werden. Der Buntspecht wurde in allen Flächen am häufigsten gesehen. Mittel-, Weißrücken- und Kleinspecht wurden überwiegend in den Tilio-Carpineten beobachtet, in den Naturwäldern häufiger als in den bewirtschafteten Beständen. Der Dreizehenspecht wurde im Nadelwald und stärker mit Fichten durchmischtem Laubwald angetroffen. Bei Schwarz- und Grauspecht konnte keine klare Vorliebe für bestimmte Waldgesellschaften ermittelt werden. Der Buntspecht ernährte sich vor allem im Herbst und Winter überwiegend von fetthaltigen Samen und wurde dann meist beim Bearbeiten von Fichten- oder Kiefernzapfen in Schmieden beobachtet. Der Mittelspecht suchte als "Sammelspecht" seine Nahrung vor allem an den Oberflächen der Stämme und Äste. Klein-, Weißrücken-, Dreizehen- und Schwarzspecht traten als Hackspechte in Erscheinung. Die wenigen Daten zum Grauspecht reichen nicht zur Ermittlung der bevorzugten Nahrungserwerbstechnik aus. Bei Bunt-, Mittel- und Weißrückenspecht konnte eine deutliche Vorliebe für die Stieleiche als Nahrungsbaum nachgewiesen werden. Der Dreizehenspecht ist jedoch die einzige der beobachteten Arten mit einer weitgehenden Spezialisierung auf eine bestimmte Baumart, er nutzte in allen Waldgesellschaften meist die Fichte. Insgesamt bevorzugten die Spechte Bäume mit großen Stammdurchmessern, beim Kleinspecht ist diese Vorliebe allerdings nur schwach ausgeprägt. Totholz wurde von Weißrücken-, Dreizehen- und Kleinspecht bei der Nahrungssuche bevorzugt, vom Mittelspecht jedoch nur gelegentlich genutzt. Beim Buntspecht zeigte der Totholz-Nutzungsanteil erhebliche Unterschiede zwischen verschiedenen Baumarten. Liegendes Totholz spielte in den Tilio-Carpineten im Vergleich zu stehendem Totholz und toten Teilen lebender Bäume nur eine geringe Rolle für Nahrung suchende Spechte.

Recent patterns of change in vegetation structure and tree composition of British broadleaved woodland: evidence from large-scale surveys

Evidence is presented of widespread changes in structure and species composition between the 1980s and 2003–2004 from surveys of 249 British broadleaved woodlands. Structural components examined include canopy cover, vertical vegetation profiles, field-layer cover and deadwood abundance. Woods were located in 13 geographical localities and the patterns of change were examined for each locality as well as across all woods. Changes were not uniform throughout the localities; overall, there were significant decreases in canopy cover and increases in sub-canopy (2–10 m) cover. Changes in 0.5–2 m vegetation cover showed strong geographic patterns, increasing in western localities, but declining or showing no change in eastern localities. There were significant increases in canopy ash Fraxinus excelsior and decreases in oak Quercus robur/petraea. Shrub layer ash and honeysuckle Lonicera periclymenum increased while birch Betula spp. hawthorn Crataegus monogyna and hazel Corylus avellana declined. Within the field layer, both bracken Pteridium aquilinum and herbs increased. Overall, deadwood generally increased. Changes were consistent with reductions in active woodland management and changes in grazing and browsing pressure. These findings have important implications for sustainable active management of British broadleaved woodlands to meet silvicultural and biodiversity objectives.

Antioxidant capacity and phenolic composition of different woods used in cooperage

This study has investigated the antioxidant capacity of different woods used in cooperage and the effect of the botanical species of wood on this capacity. Quercus robur and Castanea sativa were the species with the highest antioxidant capacity, due to their relatively high content of phenolic compounds. However, the phenolic content of Prunus avium samples was very low, also reflected in its antioxidant capacity. All measurements of antioxidant capacity were consistent with the content and composition of the phenolic compounds detected in the wood samples. The major contributors to the antioxidant capacity were identified as phenolic acids, including gallic, protocatechuic, p-coumaric and ellagic acid and all the ellagitannins, due to their characteristic structure.

Relationships between Oak powdery mildew incidence and severity and commensal fungi

Oak (Quercus robur) powdery mildew is a common and damaging fungal disease. In a local survey at Reading, UK, oak powdery mildew was common on trees of all height classes but was most common on trees of 3-9m. A variety of other fungal species were commonly found growing in association with oak powdery mildew colonies. The abundance of such fungi was estimated through stratified sample surveys for 2.5 years. The taxa most commonly associated with oak powdery mildew were Acremonium sp., Trichoderma sp., Ampelomyces/Phoma sp. and Leptosphaerulina australis. Nearly 90% of mildew colonies were associated with L. australis, which is not generally considered as a mycoparasite or antagonist, in contrast with the other three fungi. Abundance varied between June and October surveys. Acremonium sp. abundance was greater in summer samplings whereas L. australis and Trichoderma sp. abundances were greater in autumn samplings. Ampelomyces/Phoma sp. was never observed in the absence of powdery mildew. Relationships between the mildew-associated fungi and oak powdery mildew appeared curved and differed significantly between sampling years. L. australis was positively correlated with the other three associated fungi studied when powdery mildew was also present. The variety and high population densities of the mildew associated fungi suggest that they may be important in determining the final density of oak mildew and the damage caused by it.

Effect of air-drying pre-treatment on the characterization of forest soil carbon pools

Archived soils could represent a valuable resource for the spatio-temporal inventory of soil carbon stability. However, archived soils are usually air-dried before storage and the impact of a drying pretreatment on physically and chemically-defined C fractions has not yet been fully assessed. Through the comparison of field-moist and corresponding air-dried (at 25oC for 2 weeks) forest soil samples, we examined the effect of air-drying on: a) the quantity and the quality of cold- (CWEC) and hot-water (HWEC) extractable C and b) the concentration of C in physically isolated fractions (free- and intra-aggregate light and organo-mineral). Soil samples were collected from the organic (O) and mineral (A and B) horizons of three different forest soils from southeastern England: (i) Cambisol under Pine (Pinus nigra); (ii) Cambisol under Beech (Fagus sylvatica) and (iii) Gleysol under oak (Quercus robur). CWEC concentrations for dry samples were up to 2 times greater than for corresponding field moist samples and had significantly (p < 0.001) higher phenolic content. However, the effect of drying pretreatment on HWEC, its phenolic content was not significant (p > 0.05) for most samples. Dried soils had significantly (p < 0.001) higher concentrations of free light-C while having lower concentrations of intra-aggregate-C when compared to moist samples (p < 0.001). However, fine silt and clay fractions were not significantly affected by the drying pretreatment (p=0.789). Therefore, based on the results obtained from gleysol and cambisol forest soils studied here, C contents in hot-water extractions and fine particle size physical fractions (< 25µm) seem to be robust measurements for evaluating C fractions in dried stored forest soils. Further soil types should be tested to evaluate the wider generality of these findings.

Ekens förekomst i Ludvikatrakten

Ekens (Quercus robur) nordgräns sägs gå vid Dalälven, Limes Norrlandicus – den biologiska Norrlandsgränsen. Ludvikabygden skiljer sig naturgeografiskt och topografiskt från övriga Dalarna och tillhör Mälarens avrinningsområde. Trakten runt sjön Väsman har ett varmare klimat och fler soltimmar än den övriga bygden. För mellan 5.000-8.000 år sedan vandrade eken in i Sverige efter den senaste istiden. Det tog 3.000 år för den att sprida sig över hela Sverige som då hade en medeltemperatur 2-3? högre än idag.Ekens vegetationsperiod – när dygnsmedeltemperaturen överstiger 5? – är ca 7 månader för att ekollonen skall bli groningsdugliga och därmed kunna föröka sig naturligt. I Ludvikatrakten är vegetationsperioden ca 6 månader. Dalarnas skogar består av ? 1% ek. Årsmedeltemperaturen har i Mellansverige ökat ungefär 1? de senaste 30 åren. I framtiden får vi räkna med temperaturhöjningar på mellan 2-6? beroende på hur stort utsläpp som sker till atmosfären. Detta innebär att vi på dessa breddgrader får ett klimat liknande det i Centraleuropa med längre odlingssäsong. Det innebär också ökande skador på skog och växtlighet samt fler och mer extrema väderväxlingar.Syftet med den här undersökningen är att se om etablering av ek har skett i Ludvikatrakten de senaste decennierna samt vilka faktorer som kan påverka detta. Två separata områden om vardera 1,0 ha undersöktes. På område 1 i nordvästsluttning registrerades 20 exemplar av ek. På område 2 i västsluttning registrerades 28 exemplar av ek. Gamla ekar är en nyckelbiotop för sällsynta insekter och kryptogamer. Ek är stormfast p g a dess djupa rotsystem. Blandskog motverkar parasit-, insektsangrepp och rotröta samt gynnar biologisk mångfald och etablering av fältskikt. Ekens virke är dessutom eftertraktat då det är hårt och slitstarkt.

Enraizamento de plantas cultivadas in vitro

The adventitious rooting process of in vitro cultured plantlets is a technique that has been employed for the vegetative propagation of a significant number of native and exotic species. Many factors are associated with the rooting stage influencing positive and/or negatively the establishment of micropropagation protocols. The objective of this work was a literature review of the main inherent factors concerning in vitro rooting process including the correlation among others the endogenous and exogenous auxins levels, juvenility, genotype, mineral nutrition, culture medium conditions, addition of growth regulators and other substances as phenolic compounds and active coal besides growth environmental conditions of in vitro cultures. Although the complete elucidation of all processes involved with rooting of in vitro cultured plants has not been achieved so far, a comprehensive study of the main factors that interfere on rooting is fundamental for the establishment of new researches that might contribute for the rooting of economically important plants.

Uso sostenibile dei suoli forestali di ambiente costiero in relazione ai fattori di pressione esistenti

Oggetto di studio del dottorato sono stati i suoli forestali in ambiente litoraneo della Regione Emilia-Romagna. In particolare sono state considerate quattro zone di studio in Provincia di Ravenna: Pineta di San Vitale, aree boscate di Bellocchio, Pineta di Classe e Pineta di Pinarella di Cervia. Lo studio in una prima fase si è articolato nella definizione dello stato del sistema suolo, mediante la caratterizzazione pedologica delle zone di studio. A tale scopo è stata messa a punto un’adeguata metodologia d’indagine costituita da un’indagine ambientale e successivamente da un’indagine pedologica. L’indagine ambientale, mediante fotointerpretazione ed elaborazione di livelli informativi in ambito GIS, ha permesso di individuare ambiti pedogenetici omogenei. L’indagine pedologica in campo ha messo in luce l’elevata variabilità spaziale di alcuni fattori della pedogenesi, in particolar modo l’andamento microtopografico tipico dei sistemi dunali costieri e la profondità della falda freatica del piano campagna. Complessivamente sono stati aperti descritti e campionati 40 profili pedologici. Sugli orizzonti diagnostici di questi sono state eseguite le seguenti analisi: tessitura, pH, calcare totale, carbonio organico, azoto kjeldahl, conduttività elettrica (CE), capacità di scambio cationico (CSC) e calcare attivo. I suoli presentano, ad eccezione della tessitura (generalmente grossolana), un’elevata variabilità delle proprietà chimico fisiche in funzione della morfologia, della profondità e della vicinanza della falda freatica. Sono state riscontrate diverse correlazioni, tra le più significative quelle tra carbonio organico e calcare totale (coeff. di correlazione R = -0.805 per Pineta di Classe) e tra calcare totale e pH (R = 0.736), dalle quali si è compreso in che misura l’effetto della decarbonatazione agisce nei diversi ambiti pedogenetici e tra suoli con diversa età di formazione. Il calcare totale varia da 0 a oltre 400 g.kg-1 e aumenta dalla superficie in profondità, dall’entroterra verso la costa e da nord verso sud. Il carbonio organico, estremamente variabile (0.1 - 107 g.kg-1), è concentrato soprattutto nel primo orizzonte superficiale. Il rapporto C/N (>10 in superficie e molto variabile in profondità) evidenzia una efficienza di umificazione non sempre ottimale specialmente negli orizzonti prossimi alla falda freatica. I tipi di suoli presenti, classificati secondo la Soil Taxonomy, sono risultati essere Mollic/Sodic/Typic Psammaquents nelle zone interdunali, Typic Ustipsamments sulle sommità dunali e Oxiaquic/Aquic Ustipsamments negli ambienti morfologici intermedi. Come sintesi della caratterizzazione pedologica sono state prodotte due carte dei suoli, rispettivamente per Pineta di San Vitale (scala 1:20000) e per le aree boscate di Bellocchio (scala 1:10000), rappresentanti la distribuzione dei pedotipi osservati. In una seconda fase si è focalizzata l’attenzione sugli impatti che le principali pressioni naturali ed antropiche, possono esercitare sul suolo, condizionandone la qualità in virtù delle esigenze del soprasuolo forestale. Si è scelta la zona sud di Pineta San Vitale come area campione per monitorarne mensilmente, su quattro siti rappresentativi, le principali caratteristiche chimico-fisiche dei suoli e delle acque di falda, onde evidenziare possibili correlazioni. Le principali determinazioni svolte sia nel suolo in pasta satura che nelle acque di falda hanno riguardato CE, Ca2+, Mg2+, K+, Na+, Cl-, SO4 2-, HCO3 - e SAR (Sodium Adsorption Ratio). Per ogni sito indagato sono emersi andamenti diversi dei vari parametri lungo i profili, correlabili in diversa misura tra di loro. Si sono osservati forti trend di aumento di CE e degli ioni solubili verso gli orizzonti profondi in profili con acqua di falda più salina (19 – 28 dS.m-1) e profonda (1 – 1.6 m dalla superficie), mentre molto significativi sono apparsi gli accumuli di sali in superficie nei mesi estivi (CE in pasta satura da 17.6 a 28.2 dS.m-1) nei profili con falda a meno di 50 cm dalla superficie. Si è messo successivamente in relazione la CE nel suolo con diversi parametri ambientali più facilmente monitorabili quali profondità e CE di falda, temperatura e precipitazioni, onde trovarne una relazione statistica. Dai dati di tre dei quattro siti monitorati è stato possibile definire tali relazioni con equazioni di regressione lineare a più variabili. Si è cercato poi di estendere l’estrapolabilità della CE del suolo per tutte le altre casistiche possibili di Pineta San Vitale mediante la formulazione di un modello empirico. I dati relativi alla CE nel suolo sia reali che estrapolati dal modello, sono stati messi in relazione con le esigenze di alcune specie forestali presenti nelle zone di studio e con diverso grado di tolleranza alla salinità ed al livello di umidità nel suolo. Da tali confronti è emerso che per alcune specie moderatamente tolleranti la salinità (Pinus pinea, Pinus pinaster e Juniperus communis) le condizioni critiche allo sviluppo e alla sopravvivenza sono da ricondursi, per la maggior parte dei casi, alla falda non abbastanza profonda e non tanto alla salinità che essa trasmette sull’intero profilo del suolo. Per altre specie quali Quercus robur, Populus alba, Fraxinus oxycarpa e Ulmus minor moderatamente sensibili alla salinità, ma abituate a vivere in suoli più umidi, la salinità di una falda troppo prossima alla superficie può ripercuotersi su tutto il profilo e generare condizioni critiche di sviluppo. Nei suoli di Pineta San Vitale sono stati inoltre studiati gli aspetti relativi all’inquinamento da accumulo di alcuni microtossici nei suoli quali Ag, Cd, Ni e Pb. In alcuni punti di rilievo sono stati osservati moderati fattori di arricchimento superficiale per Pb e Cd riconducibili all’attività antropica, mentre le aliquote biodisponibili risultano maggiori in superficie, ma all’interno dei valori medi dei suoli italiani. Lo studio svolto ha permesso di meglio conoscere gli impatti sul suolo, causati dalle principali pressioni esistenti, in un contesto dinamico. In particolare, si è constatato come i suoli delle zone studiate abbiano un effetto tampone piuttosto ridotto sulla mitigazione degli effetti indotti dalle pressioni esterne prese in esame (salinizzazione, sodicizzazione e innalzamento della falda freatica). Questo è dovuto principalmente alla ridotta presenza di scambiatori sulla matrice solida atti a mantenere un equilibrio dinamico con le frazioni solubili. Infine le variabili ambientali considerate sono state inserite in un modello concettuale DPSIR (Driving forces, Pressures, States, Impacts, Responces) dove sono stati prospettati, in via qualitativa, alcuni scenari in funzione di possibili risposte gestionali verosimilmente attuabili, al fine di modificare le pressioni che insistono sul sistema suolo-vegetazione delle pinete ravennati.

Measurement of nonmethane organic carbon

The present dissertation focuses on the measurement of nonmethane organic carbon compounds (NMOC) and their exchange by biosphere-atmosphere interactions. To access the accuracy, precision, and reproducibility of NMOC analysis, two intercomparison experiments were carried out during the present study. These experiments comprised the sampling of NMOCs on graphitised carbon blacks, followed by gas-chromatographic analysis. Furthermore, they comprised the sampling of short chain carbonyl compounds on solid phase extraction cartridges and their analysis by high pressure liquid chromatography. To investigate the exchange of NMOCs between vegetation and the atmosphere, plant enclosure studies were performed on two European deciduous tree species. These measurements were conducted during two consecutive summer seasons by utilisation of the above specified techniques on sunlit and shaded leaves of European beech (Fagus sylvatica L., monoterpene emitter) and sunlit leaves of English oak (Quercus robur L., isoprene emitter). According to its broad geographical distribution, the impact of European beech on the European monoterpene budget was characterized by a model simulation. Complementary an instrument was developed, that is capable of measuring the amount of total NMOC that is exchanged by biosphere-atmosphere interactions. The instrument was tested under laboratory conditions and was evaluated versus an independent method performing branch enclosure measurements.

Untersuchungen zum Austausch von Stickstoffdioxid (NO 2) zwischen Pflanzen und Atmosphäre

Der Austausch der NO2-Konzentration zwischen der Atmosphäre und verschiedenen Bäumen (Betula pendula, Fagus sylvatica, Quercus robur, Quercus ilex und Pinus sylvestris) wurde mit einer Dynamischen Küvette gemessen. Die NO2-Konzentrationen wurden mit einem CLD 780 TR Analysator in Verbindung mit einem PLC 762 gemessen. Die experimentellen Untersuchungen wurden im Dunkeln und unter zwei Lichtintensitäts-Niveaus (PAR, 450 und 900 µmol m-2 s-1) und sechs verschiedene NO2-Konzentrationen zwischen 0 - 5.0 ppb durchgeführt. Der stomatäre Einfluss wurde unter Einsatz des Hormons Abscisinsäure untersucht. Die Umgebungsparameter (Lufttemperatur und Luftfeuchtigkeit) wurden konstant gehalten. Die Daten zeigten klar und deutlich den dominanten Einfluss der jeweiligen Baumspezies auf die NO2-Konzentrationen innerhalb der Küvette. Die Ergebnisse dieser Arbeit belegen bei allen Spezies eine lineare Abhängigkeit der NO2-Austauschrate mit der NO2-Umgebungskozentration und mit der stomatären Leitfähigkeit. Das Vorhandensein eines Kompensationspunkt wird nicht bestätigt.