Sunflower under conventional and organic farming systems: results from a long term experiment in Central Italy

Sunflower productivity under organic and conventional agricultural systems was studied between 2002 and 2004 in the frame of the MASCOT experiment (Mediterranean Arable Systems COmparison Trial), established in 2001. The aim was to compare organic and conventional management systems for a typical arable crop rotation of Central Italy in the long-term. Sunflower was cultivated as a part of a five-year stockless arable crop rotation (sugar beet-common wheatsunflower-pigeon bean-durum wheat). In the organic system, red clover (Trifolium pratense) is interseeded in common and durum wheat and used as a green manure for sunflower or sugar beet. Grain yield of organically-grown sunflower was lower by 41%, 17% and 44% in 2002, 2003 and 2004 respectively, but no significant differences in percent seed oil content were found between the conventional and organic sunflower in two years out of three

Localizzazione probabilistica 3D (NonLinLoc) applicata all’area calabro-peloritana

Sono presentati e discussi i risultati preliminari relativi ad una ri-localizzazione probabilistica non-lineare 3D dei terremoti dell’area compresa tra il Tirreno meridionale e l’Arco Calabro-Peloritano (Italia meridionale). Scopo del lavoro è dimostrare che l’applicazione di un’approccio probabilistico non-lineare nella localizzazione dei terremoti può fornire dei risultati più accurati ai fini della sorveglianza, ovviando al problema degli outlier, rispetto alle tecniche di localizzazione lineari (e.g. Hypoellipse), che minimizzano simultaneamente tutti i residui tra fasi osservate e calcolate. Il programma utilizzato è NonLinLoc [Lomax, et al., 2000; Lomax, et al., 2001; Lomax, 2005; http://www.alomax.net/nlloc; NonLinLoc di seguito] il quale permette di effettuare un’efficiente ricerca globale dello spazio dei parametri ipocentrali (coordinate spaziali e tempo origine) ottenendo una stima della funzione densità di probabilità (pdf, probability density function) a posteriori. La pdf fornisce una descrizione completa della localizzazione e delle sue incertezze; il campionamento dello spazio dei parametri ipocentrali è stato fatto mediante la tecnica Oct-tree nella regione compresa tra 37.75 e 39.40 N in latitudine e tra 14.80 e 16.80 E in longitudine, e utilizzando tutti gli eventi con profondità H ≤30 km. La struttura dell’Oct-tree è stata imposta in 100,000 celle ed un insieme di queste celle viene poi salvata in modo da poter rappresentare graficamente la pdf mediante nubi di punti a diversa densità. Il dataset utilizzato per le nostre analisi è composto da 1,304 terremoti, di 1.0<M<4.3, registrati nel periodo compreso tra il 1994 e il 2006; il modello di velocità 3D adottato è stato ottenuto da Barberi et al., 2008 [poster presentato a questo convegno] invertendo lo stesso dataset, mediante l’utilizzo del software TomoDD. I risultati ottenuti sono stati confrontati sia con le localizzazioni 1D (Hypoellipse) che con quelle 3D. Si evidenzia una maggiore clusterizzazione degli eventi e, soprattutto, un evidente miglioramento della qualità delle localizzazioni utilizzando il modello di velocità crostale 3D. Per cui riteniamo che, l’applicazione del metodo probabilistico associato ad un buon modello di velocità 3D, può essere utilizzato ai fini di sorveglianza

Localizzazione probabilistica 3D (NonLinLoc) applicata all’area calabro-peloritana

Sono presentati e discussi i risultati preliminari relativi ad una ri-localizzazione probabilistica non-lineare 3D dei terremoti dell’area compresa tra il Tirreno meridionale e l’Arco Calabro-Peloritano (Italia meridionale). Scopo del lavoro è dimostrare che l’applicazione di un’approccio probabilistico non-lineare nella localizzazione dei terremoti può fornire dei risultati più accurati ai fini della sorveglianza, ovviando al problema degli outlier, rispetto alle tecniche di localizzazione lineari (e.g. Hypoellipse), che minimizzano simultaneamente tutti i residui tra fasi osservate e calcolate. Il programma utilizzato è NonLinLoc [Lomax, et al., 2000; Lomax, et al., 2001; Lomax, 2005; http://www.alomax.net/nlloc; NonLinLoc di seguito] il quale permette di effettuare un’efficiente ricerca globale dello spazio dei parametri ipocentrali (coordinate spaziali e tempo origine) ottenendo una stima della funzione densità di probabilità (pdf, probability density function) a posteriori. La pdf fornisce una descrizione completa della localizzazione e delle sue incertezze; il campionamento dello spazio dei parametri ipocentrali è stato fatto mediante la tecnica Oct-tree nella regione compresa tra 37.75 e 39.40 N in latitudine e tra 14.80 e 16.80 E in longitudine, e utilizzando tutti gli eventi con profondità H ≤30 km. La struttura dell’Oct-tree è stata imposta in 100,000 celle ed un insieme di queste celle viene poi salvata in modo da poter rappresentare graficamente la pdf mediante nubi di punti a diversa densità. Il dataset utilizzato per le nostre analisi è composto da 1,304 terremoti, di 1.0<M<4.3, registrati nel periodo compreso tra il 1994 e il 2006; il modello di velocità 3D adottato è stato ottenuto da Barberi et al., 2008 [poster presentato a questo convegno] invertendo lo stesso dataset, mediante l’utilizzo del software TomoDD. I risultati ottenuti sono stati confrontati sia con le localizzazioni 1D (Hypoellipse) che con quelle 3D. Si evidenzia una maggiore clusterizzazione degli eventi e, soprattutto, un evidente miglioramento della qualità delle localizzazioni utilizzando il modello di velocità crostale 3D. Per cui riteniamo che, l’applicazione del metodo probabilistico associato ad un buon modello di velocità 3D, può essere utilizzato ai fini di sorveglianza

Double-difference tomography at Mt. Etna volcano

Double-difference tomography at Mt Etna volcano was realized by using the tomographic algorithm developped by Monteiller et al. (2005), in which the travel-time computation was performed using a finite-difference solution of the Eikonal equation (Podvin and Lecomte, 1991) and a posteriori ray-tracing. The inverse problem was solved using a probabilistic approach (Tarantola and Valette, 1982). The optimal a priori information (correlation length and a priori model variance) was found experimentally by performing tomographies for correlation lengths and variances varying in large intervals. This probabilistic approach allowed us to use a sech pdf for representing errors in differential times. Data were travel-times and time delays provided by a set of 329 earthquakes, well-recorded by the INGV-CT seismic network (50 stations) on the Mt Etna volcano during the seismo-volcanic crisis occurring between October 2002 and January 2003. Checkerboard tests realized with this geometry and earthquake pairs showed that the model can be correctly reconstructed in a significant area around Mt Etna volcano. Results of the P and S-wave double-difference tomography clearly evidenced two concentric features: a fast central cylindrical core, probably of intrusive origin, surrounded by a slow annealed body, which could be related to partial melting

Double-difference tomography at Mt Etna volcano: Preliminary results

We performed a preliminary double-difference tomographic study using earthquake data recorded by the INGV-Catania seismic network during the large seismic and eruptive crisis of 2002-2003 at Mt Etna volcano. Compared to previous models, first results presented from the inversion of travel-time differences, tend to show an increase in the velocity contrast between the fast core and the slow periphery of the volcano

Receiver Function Analysis at Stromboli Volcano (Italy)

This study focuses on constraining the crust and upper mantle discontinuities at Stromboli volcano by applying the receiver function (RF) analysis. This technique utilizes the waveforms of P-SV conversions generated by discontinuities to infer the structure beneath the seismic stations. RFs have been obtained by deconvolving the vertical component of teleseismic P-wave records from the corresponding rotate horizontal components applying the Multi-Taper Spectral Correlation technique. For this study the seismograms of about 125 teleseismic earthquakes (M greater than 6.0), recorded between 2004 and 2006 at 13 broad-band seismic stations deployed by the INGV, have been considered. A preliminar characterization of the structure beneath the stations has been inferred from the stacking of teleseismic Ps converted waves and multiply converted waves at the seismic interface. The analysis, at frequency of 1 and 2 Hz, show a horizontal seismic discontinuity at an average depth of about 17 km and a Vp/Vs ratio lower than 1.73. This discontinuity explains the positive pulses about 1.9 s and 7.5 s after the direct P arrival. These pulses can be interpreted as Ps and PpPs converted phases, respectively. The depth of this discontinuity is in agreement with the Moho-depth obtained in independent studies

Ordered interfaces for dual easy axes in liquid crystals

International audienceUsing nCB films adsorbed on MoS 2 substrates studied by x-ray diffraction, optical microscopy and Scanning Tunneling Microscopy, we demonstrate that ordered interfaces with well-defined orientations of adsorbed dipoles induce planar anchoring locked along the adsorbed dipoles or the alkyl chains, which play the role of easy axes. For two alternating orientations of the adsorbed dipoles or dipoles and alkyl chains, bi-stability of anchoring can be obtained. The results are explained using the introduction of fourth order terms in the phenomenological anchoring potential, leading to the demonstration of first order anchoring transition in these systems. Using this phenomenological anchoring potential, we finally show how the nature of anchoring in presence of dual easy axes (inducing bi-stability or average orientation between the two easy axes) can be related to the microscopical nature of the interface. Introduction Understanding the interactions between liquid crystal (LC) and a solid substrate is of clear applied interest, the vast majority of LC displays relying on control of interfaces. However this concerns also fundamental problems like wetting phenomena and all phenomena of orientation of soft matter bulk induced by the presence of an interface. In LCs at interfaces, the so-called easy axes correspond to the favoured orientations of the LC director close to the interface. If one easy axis only is defined for one given interface, the bulk director orients along or close to this axis [1]. It is well known that, in anchoring phenomena, two major effects compete to impose the anchoring directions of a liquid crystal, first, the interactions between molecules and the interface, second, the substrate roughness whose role has been analyzed by Berreman [2]. The influence of adsorbed molecular functional groups at the interface is most often dominant with, for example in carbon substrates, a main influence of unsaturated carbon bonds orientation at the interface [3]. In common LC displays, there is one unique easy axis, but modifications of surfaces have allowed for the discovery of promising new anchoring-related properties. For instance, the first anchoring bi-stability has been established on rough surfaces, associated with electric ordo-polarization [4] and the competition between a stabilizing short-range term and a destabilizing long-range term induced by an external field, can induce a continuous variation of anchoring orientation [5]. More recently, surfaces with several easy axes have been studied extensively. It has been shown that control of a continuous variation of director pretilt, obtained in several systems [6, 7], is associated with the presence of two different easy axes, one perpendicular to the substrate (homeotropic) and one planar [7, 8]. Similar models can explain the continuous evolution of anchoring between two planar orientations observed on some crystalline substrates [9]. However, in the same time, two easy axes can also lead to anchoring bi-stability [10, 11] or discontinuous transitions of anchoring [9], which is not compatible with the model established to interpret observed control of pretilt. In order to be able to predict if bi-stability or continuous combination of the two easy axes occurs for one given system, it becomes necessary to understand the microscopic origin of the easy axes

Organic farming systems for adaptation to and mitigation of climate change: Effects on soil fertility and resource use efficiency

Organic farming is pointed as one of the most sustainable farming practices in terms of environmental sustainability and climate change mitigation potential. At the core of organic farming practices there are practices aimed at improving soil fertility, increasing soil C content and enhancing system biodiversity. A long-term field experiment (LTE) (MASCOT) was started on 2001 in San Piero a Grado, Pisa (Italy) with the aim to compare two different cropping systems, one managed organically and one conventionally, in terms of agronomical, economic and environmental sustainability. In 2016, the MASCOT was redesigned as a full system trial and the organic system was reshaped according to up to date agroecological standards. Climate change adaptation capacity of the two systems is being assessed through agronomic and economic parameters, whilst greenhouse gas emission mitigation potential is mainly expressed in terms of soil C sequestration