Granulometry, biogenic silica content, magnetic susceptibility and bulk densities of ODP Site 188-1165

The Prydz Bay area is a key region for studying and understanding the history of the eastern Antarctic Continental Ice Sheet (O'Brien, Cooper, Richter, et al., 2001, doi:10.2973/odp.proc.ir.188.2001). Ocean Drilling Program (ODP) Site 1165 is situated in a water depth of 3357 m on the continental rise offshore from Prydz Bay and lies in front of the outlet for the Lambert Glacier-Amery Ice Shelf system that today drains 22% of East Antarctica. The site was drilled into mixed pelagic and hemipelagic sediments from the southwestern side of the Wild Drift. The drift is an elongate sediment body formed by the interaction of sediment supplied from continental shelf and slope with westward-flowing bottom currents. The sedimentary sequence is characterized by alternations between a generally gray to dark gray facies and a green to greenish gray facies. The greenish facies are structureless diatom-bearing clays with common bioturbation and larger amounts (>15%-20%) of biogenic silica, dispersed clasts, and lonestones than the dark gray facies, which are mostly less bioturbated clay with some silt laminations (Shipboard Scientific Party, 2001, doi:10.2973/odp.proc.ir.188.103.2001). High-quality advanced piston corer and extended core barrel cores containing nearly complete sections of middle Miocene to early Pliocene age allow a detailed characterization of sedimentary cycles and can provide indications for ice advances of the Lambert Glacier system into Prydz Bay, for the extent of sea ice, and for changes in oceanic circulation. The purpose of this work is to provide a data set of coarse-fraction mass percentage (>63, >125, and >250 µm) and biogenic silica content measured on sediments of late Miocene to early Pliocene age drilled at Site 1165. Additionally, high-resolution records of magnetic susceptibility (MS) and gamma ray attenuation (GRA) bulk density are presented. These shipboard data sets were edited postcruise. Furthermore, I provide a high-resolution dry bulk density record that is derived from GRA bulk density and can be used for the calculation of mass accumulation rates. These sedimentological and physical parameters will be used in future work to understand the depositional pattern of alternating biogenic and terrigenous sediments that was observed at Site 1165 (Shipboard Scientific Party, 2001, doi:10.2973/odp.proc.ir.188.103.2001).

EPICA Dronning Maud Land EDML ice core drilling protocol

We report on the EPICA Dronning Maud Land (East Antarctica) deep drilling operation. Starting with the scientific questions that led to the outline of the EPICA project, we introduce the setting of sister drillings at NorthGRIP and EPICA Dome C within the European ice-coring community. The progress of the drilling operation is described within the context of three parallel, deep-drilling operations, the problems that occurred and the solutions we developed. Modified procedures are described, such as the monitoring of penetration rate via cable weight rather than motor torque, and modifications to the system (e.g. closing the openings at the lower end of the outer barrel to reduce the risk of immersing the drill in highly concentrated chip suspension). Parameters of the drilling (e.g. core-break force, cutter pitch, chips balance, liquid level, core production rate and piece number) are discussed. We also review the operational mode, particularly in the context of achieved core length and piece length, which have to be optimized for drilling efficiency and core quality respectively. We conclude with recommendations addressing the design of the chip-collection openings and strictly limiting the cable-load drop with respect to the load at the start of the run.

Paleomagnetism at DSDP Leg 85 Holes

On Leg 85, 16 holes were cored at five sites. Thirteen of the holes were cored with the hydraulic piston corer (HPC) or the variable-length hydraulic piston corer (VLHPC) or both; the remainder were rotary drilled. Partially duplicating stratigraphic sections were successfully recovered by hydraulic piston coring at Sites 572 to 575. Sub-bottom penetration was deepest (about 210 m) at HPC Hole 575A, which bottomed in lower Miocene sediments. Penetration by hydraulic piston coring was limited at all sites not by the failure of the corer to stroke out but by the excessive force (overpull) necessary to retrieve the core barrel from the hole. The sediments recovered are relatively uniform siliceous-calcareous oozes to calcareous ooze-chalks. Paleomagnetic measurements were made at all stratigraphic levels, but magnetostratigraphic sequences could be resolved only for the Pleistocene-Pliocene and for brief upper, middle, and lower Miocene sections. In the younger and less consolidated sediments, the declination often shows large-scale azimuthal rotations downcore. These smooth trends vary from core to core, indicating either rotation between the sediment and the core liner or the rotation of the core barrel during the coring or retrieval process. Thus, azimuthal orientation of the samples was impossible even though a Kuster azimuthal orientation tool was used during the hydraulic piston coring. At all sites, the downhole shift from mainly siliceous to mainly calcareous ooze-chalk coincided with a decrease in NRM intensity of at least one order of magnitude, to 1.0*10**-8 G. Diagenesis is the probable reason for this behavior, although the dilution of magnetic carriers as the result of higher accumulation rates may also be a factor. A tectonic analysis using data from samples with stable remanence indicates a northward plate motion of about 0.3 deg/m.y. during the last 18 m.y., a rate that agrees with most previous reconstructions of Pacific Plate motion.

Geochemistry and isotopes at DSDP Site 68-503

Nodules occur in the siliceous calcareous ooze and siliceous marl at Site 503 in the eastern equatorial Pacific. They are present below a depth of about 11 meters throughout the green-colored reduced part of the section down to 228 meters, although they are most abundant between 30 and 85 meters. They are cylindrical or barrel-shaped, up to 70 mm long, and usually have an axial channel through them or are hollow. They appear to have formed around and/or within burrows. XRD studies and microprobe analyses show that they are homogeneous and consist of calcian rhododrosite and minor calcite; Mn is present to the extent of about 30%. Isotopic analyses of the carbonate give carbon values which range from -1.2 per mil to -3.8 per mil, and oxygen isotope compositions vary from +4.0 per mil to +6.0 per mil. These values are different from those for marine-derived carbonates as exemplified by the soft sediment filling of a burrow: d13C, -0.26 per mil; d18O, +1.05 per mil. The carbon isotope data indicate that carbonate derived (possibly indirectly) from seawater was mixed with some produced by organic diagenesis to form the nodules. The d18O values suggest that although they formed near the sediment surface, some modification or the introduction of additional diagenetic carbonate occurred during burial.

Stable foraminifer isotope composition and age of ODP Sites 184-1147 and 184-1148, South China Sea

Sites 1147 (18°50.11'N, 116°33.28'E; water depth = 3246 m) and 1148 (18°50.17'N, 116°33.94'E; water depth = 3294 m) are located on the lowermost continental slope off southern China near the continent/ocean crust boundary of the South China Sea Basin. Site 1147 is located upslope ~0.45 nmi west of Site 1148. Three advanced piston corer holes at Site 1147 and two extended core barrel holes at Site 1148 were cored and combined into a composite (spliced) stratigraphic section, which provided a relatively continuous profile for the lower Oligocene to Holocene (Wang, Prell, Blum, et al., 2000, doi:10.2973/odp.proc.ir.184.2000; Jian, et al., 2001, doi:10.1007/BF02907088) for studying stratigraphy and paleoceanography. A total of 1047 planktonic foraminifers stable isotope measurements were performed on 975 samples covering the upper 409.58 meters composite depth (mcd) at ~42-cm intervals (Tables T1, T2), and a total of 1864 benthic foraminifers measurements were performed on 1650 samples in the upper 837.11 mcd at ~51-cm intervals (Tables T3, T4). We significantly improved the time resolution of the benthic stable isotope record in the upper 476.68 mcd by reducing the average sample spacing to ~29 cm. This translates into an average sampling resolution of ~16 k.y. for the Miocene sequence and ~8 k.y. for the Pliocene-Holocene interval, assuming a change in sedimentation rates from ~1.8 to ~3.5 cm/k.y., as suggested by shipboard stratigraphy. These data sets provide the basis for upcoming studies to establish an oxygen isotope stratigraphy and examine the Neogene evolution of deep and surface water signatures (temperature, salinity, and nutrients) in the South China Sea.

Geochemistry and isotopes at DSDP Site 76-533

Concentrations and d34S and d13C values were determined on SO4, HCO3, CO2, and CH4 in interstitial water and gas samples from the uppermost 400 m of sediment on the Blake Outer Ridge. These measurements provide the basis for detailed interpretation of diagenetic processes associated with anaerobic respiration of electrons generated by organic- matter decomposition. The sediments are anaerobic at very shallow depths (<1 m) below the seafloor. Sulfate reduction is confined to the uppermost 15 m of sediment and results in a significant outflux of oxidized carbon from the sediments. At the base of the sulfate reduction zone, upward-diffusing CH4 is being oxidized, apparently in conjunction with SO4 reduction. CH4 generation by CO2 reduction is the most important metabolic process below the 15-m depth. CO2 removal is more rapid than CO2 input over the depth interval from 15 to 100 m, and results in a slight decrease in HCO3 concentration accompanied by a 40 per mil positive shift in d13C. The differences among coexisting CH4, CO2, and HCO3 are consistent with kinetic fractionation between CH4 and dissolved CO2, and equilibrium fractionation between CO2 and HCO3. At depths greater than 100 m, the rate of input of CO2 (d13C = -25 per mil) exceeds by 2 times the rate of removal of CO2 by conversion to CH4 (d13C of -60 to -65 per mil). This results in an increase of dissolved HCO3 concentration while maintaining d13C of HCO3 relatively constant at +10 per mil. Non-steady-state deposition has resulted in significantly higher organic carbon contents and unusually high (70 meq/l) pore-water alkalinities below 150 m. These high alkalinities are believed to be related more to spontaneous decarboxylation reactions than to biological processes. The general decrease in HCO3 concentration with constant d13C over the depth interval of 200 to 400 m probably reflects increased precipitation of authigenic carbonate. Input-output carbon isotope-mass balance calculations, and carbonate system equilibria in conjunction with observed CO2-CH4 ratios in the gas phase, independently suggest that CH4 concentrations on the order of 100 mmol/kg are present in the pore waters of Blake Outer Ridge sediments. This quantity of CH4 is believed to be insufficient to saturate pore waters and stabilize the CH4*6H2O gas hydrate. Results of these calculations are in conflict with the physical recovery of gas hydrate from 238 m, and with the indirect evidence (seismic reflectors, sediment frothing, slightly decreasing salinity and chlorinity with depth, and pressure core barrel observations) of gas-hydrate occurrence in these sediments. Resolution of this apparent conflict would be possible if CH4 generation were restricted to relatively thin (1-10 m) depth intervals, and did not occur uniformly at all depths throughout the sediment column, or if another methanogenic process (e.g., acetate fermentation) were a major contributor of gas.

Inorganic geochemistry, epoch and water content in sediments at DSDP Site 91-596

Originally, we had planned to piston core at Site 595 in order to meet the sedimentologic and biostratigraphic objectives outlined in the introductory chapter. However, consultation with our colleagues, Thomas Jordan and John Orcutt on board Melville, indicated that coring near the ocean bottom seismometer (OBS) array around Hole 595B could alter the programmed signal to noise ratio above which teleseisms trigger recording in the OBSs. They requested that we core no closer than about 8 km from three OBSs nearest Hole 595B, and selected a target for us about that distance to the west. Since a new beacon was required at this distance, a new site number, 596, was designated. Briefly, we planned to obtain oriented hydraulic piston cores to the top of the cherts, then core through the cherts using the extended core barrel (XCB) to basement. With improved recovery, we hoped to reach the sediment/basalt contact, and thus obtain a reliable biostratigraphic determination of the basement age. We planned to obtain at least one core in basement, perhaps more, with time permitting. We planned no geophysical program for the hole.

Density of alkyl esters and its mixtures

Biodiesel density is a key parameter in biodiesel simulations and process development. In this work we selected, evaluated and improved two density models, one theoretical (Rackett-Soave) and one empirical (Lapuerta's method) for methanol based biodiesels (FAME) and ethanol based biodiesel (FAEE). For this purpose, biodiesel was produced from vegetable oils (sunflower, rapeseed, soybean, olive, safflower and other two commercial mixtures of vegetable oils) and animal fats (edible and crude pork fat and beef tallow) using both methanol and ethanol for the transesterification reactions, and blended to get 21 FAME and 21 FAEE, reporting their density and detailed composition. Bibliographic data have also been used. The Rackett-Soave method has been improved by the use of a new acentric factor correlation, whereas the parameters of the empirical one are improved by considering a bigger density data bank. Results show that the evaluated models could be used to estimate the biodiesel density with a good grade of accuracy but the performed modifications improve the accuracy of the models: ARD (%) for FAME; 0.33, and FAEE; 0.26, both calculated with the modification of Rackett-Soave method and ARD (%) for FAME; 0.40 calculated with the modification of the Lapuerta's method).

Paleomagnetic reconstructions of sediments at ODP Sites 135-840 and 135-841

The geometry of the Tonga Arc implies that it has rotated approximately 17° clockwise away from the Lau Ridge as the Lau Basin formed in between. Questions have arisen about the timing of the opening, whether the arc behaved rigidly, and whether the opening occurred instead from motion of the Lau Ridge, the remanent arc. We undertook to address these questions by taking paleomagnetic samples from sediment cores drilled on the Tonga Arc at Sites 840 and 841, orienting the samples in azimuth, and comparing the paleodeclinations to expected directions. Advanced hydraulic piston corer (APC) cores from Holes 840C and 841A were oriented during drilling with a tool based on a magnetic compass and attached to the core barrel. Samples from Hole 841B were drilled with a rotary core barrel (RCB) and therefore are azimuthally unoriented. They were oriented by identifying faults and dipping beds in the core and aligning them with the same features in the Formation MicroScanner (FMS) wireline logs, which were themselves oriented with a three-axis magnetometer in the FMS tool. The best results came from the APC cores, which yielded a mean pole at -69.0°S, 112.2°E for an age of 4 Ma. This pole implies a declination anomaly of 20.8° ± 12.6° (95% confidence limit), which appears to have occurred by tectonic rotation of the Tonga Arc. This value is almost exactly that expected from the geometry of the arc and implies that it did indeed rotate clockwise as a rigid body. The large uncertainty in azimuth results from core orientation errors, which have an average standard deviation of 18.6°. The youngest cores used to calculate the APC pole contain sediments deposited during Subchron 2A (2.48-3.40 Ma), and their declinations are indistinguishable from the others. This observation suggests that most of the rotation occurred after their deposition; this conclusion must be treated with caution, however, because of the large azimuthal orientation errors. Poles from late and early Miocene sediments of Hole 841B are more difficult to interpret. Samples from this hole are mostly normal in polarity, fail a reversal test, and yield poles that suggest that the normal-polarity directions may be a recent overprint. Late Miocene reversed-polarity samples may be unaffected by this overprint; if so, they imply a declination anomaly of 51.1° ± 11.5°. This observation may indicate that, for older sediments, Tonga forearc rotations are larger than expected.

Composite depth scales, ash layer correlations and splice tie points of ODP Site 186-1151

We present composite depth scales for the multiply cored intervals from Sites 1150 and 1151. These new depth scales place coeval strata recovered in cores from different holes at a single site into a common stratigraphic framework. At Site 1150, double coring between Holes 1150A and 1150B occurred over only a short interval between ~703 and 713 meters below seafloor (mbsf), but this is sufficient to tie the upper portion of the stratigraphic section cored in Hole 1150A to the lower portion cored in Hole 1150B. The upper ~100 m of the sedimentary section at Site 1151 was double cored with the advanced piston corer and partially cored with the rotary core barrel, resulting in the complete recovery of this interval. The composite depth scales were constructed using Splicer software to vertically adjust the relative depths of various cores from one hole to the depths from another hole so as to align distinct physical properties measured on cores. The magnetic susceptibility data was the physical property most easily correlated between holes, and therefore primarily used to create a composite depth scale and spliced stratigraphic section. The spliced section is a continuous stratigraphic section constructed from representative cored intervals from the holes at a site. Both the splice and the composite depth scale can be applied to other data sets from Site 1151 to provide a stratigraphically continuous and laterally consistent basis for interpreting lithologic features or data sets. The resulting composite scale showed a 30% improvement in correlation of the magnetic susceptibility data relative to the original mbsf depth scale, and comparable improvement when applied to the other data sets.

Annotated record of the detailed examination of Mn deposits from the Albatross 1884 stations

he exploration of the Gulf Stream region was continued in 1884, under nearly the same conditions as in 1883, by the steamer Albatross, Lieut. Z. L. Tanner, commander. During the four trips, between July 20 and Sept. 13, sixty nine dredgings (at stations 2170 to 2238) were made. The results were highly satisfactory, both in the way of physical observatidns and zoological discoveries. In some localities, in 1000 to 1600 fathoms, the bottom was found covered with 0or largely composed of hard, very irregular, flattened, crust-like concretions of clay and iron-oxide, with more or less manganese?oxide in the crevices and worm-burrows with which they are filled. Sometimes a barrel-full, or more, of such masses were brought up, varying in size from a few ounces up to 20 pounds or more in weight alld from one inch to six inches in thickness.

Wedges and plate-bandes: mechanical theories after De la Hire

Plate-bandes are straight masonry arches (they are called, also, flat arches or lintel arches). Ideally they have the surfaces of extrados and intrados plane and horizontal. The stones or bricks have radial joints converging usually in one centre. The voussoirs have the form of wedges and in French they are called "claveaux". A plate-bande is, in fact, a lintel made of several stones and the proportions of lintels and plate-bandes are similar. Proportions of plate-bandes, that is the relationship between the thickness t and the span s (t/s)varies, typically between 1/4–1/3 in thick plate-bandes, and is less than 1/20 in the most slender ones. A ratio of circa 1/8 was usual in the 18th Century and follows a simple geometrical rule: the centre form with the intrados an equilateral triangle and the plate-bande should contain an arc of circle. The joints are usually plane, but in some cases present a «rebated» or «stepped» form. Plate-bandes exert an inclined thrust as any masonry arch. This thrust is usually very high and it requires either massive buttresses, or to be built in the middle of thick walls. Master builders and architects have tried since antiquity to calculate the abutment necessary for any arch. A modern architect or engineer will measure the arch thrust in units of force, kN or tons. Traditionally, the thrust has been measured as the size of the buttresses to resist it safely. Old structural rules, then, addressed the design problem establishing a relationship between the span and the depth of the buttress. These were empirical rules, particular for every type of arch or structure in every epoch. Thus, the typical gothic buttress is 1/4 of the vault span, but a Renaissance or baroque barrel vault will need more than 1/3 of the span. A plate-bande would require more than one half of the span; this is precisely the rule cited by the French engineer Gautier, who tried unsuccessfully to justify it by static reasons. They were used, typically, to form the lintels of windows or doors (1-2 m, typically); in Antiquity they were used, also, though rarely, at the gates of city walls or in niches (ca. 2 m, reaching 5.2 m). Plate-bandes may show particular problems: it is not unusual that some sliding of the voussoirs can be observed, particularly in thick plate-bandes. The stepped joints on Fig. 1, left, were used to avoid this problem. There are other «hidden» methods, like iron cramps or the use of stone wedges, etc. In seismic zones these devices were usual. Another problem relates to the deformation; a slight yielding of the abutments, or even the compression of the mortar joints, may lead to some cracking and the descent of the central keystone. Even a tiny descent will convert the original straight line of the intrados in a broken line with a visible «kink» or angle in the middle. Of course, both problems should be avoided. Finally, the wedge form of the voussoirs lead to acute angles in the stones and this can produce partial fractures; this occurs usually at the inferior border of the springers at the abutments. It follows, that to build a successful plate-bande is not an easy matter. Also, the structural study of plate-bandes is far from simple, and mechanics and geometry are related in a particular way. In the present paper we will concentrate on the structural aspects and their constructive consequences, with a historical approach. We will outline the development of structural analysis of plate-bandes from ca. 1700 until today. This brief history has a more than purely academic interest. Different approaches and theories pointed to particular problem, and though the solution given may have been incorrect, the question posed was often pertinent. The paper ends with the application of modern Limit Analysis of Masonry Structures, developed mainly by professor Heyman in the last fifty years. The work aims, also, to give some clues for the actual architect and engineer involved in the analysis or restoration of masonry buildings.

Characterization of underground cellars in the Duero Basin by GNSS, LIDAR and GPR techniques

The underground cellars of the Duero River basin are part of spread and damaged agricultural landscape which is in danger of disappearing. These architectural complexes are allocated next to small towns. Constructions are mostly dug in the ground with a gallery down or "barrel" strait through which you access the cave or cellar. This wider space is used to make and store wine. Observation and detection of the winery both on the outside and underground is essential to make an inventory of the rural heritage. Geodetection is a non-invasive technique, suitable to determinate with precision buried structures in the ground. The undertaken works include LIDAR survey techniques, GNSS and GPR obtained data. The results are used to identify with centimetric precision construction elements forming the winery. Graphic and cartographic obtained documents allow optimum visualization of the studied field and can be used in the reconstruction of the place.

Problemática estructural y de funcionamiento de la cadena de valor del jamón ibérico de bellota: el caso de Guijuelo en España

El sector porcino ibérico es un sector típicamente español. La imagen que asocia el consumidor a los productos ibéricos es la correspondiente a los productos elaborados a partir de cerdos ibéricos en explotaciones extensivas, (dehesas), y cebados en montanera. Sin embargo, según los datos publicados por el Ministerio de Agricultura, Alimentación y Medio Ambiente, más de un 70 por ciento de los cerdos ibéricos que se producen en España son criados en granjas intensivas. El sector porcino ibérico está en pleno proceso de cambio, tanto por las variaciones que se derivan de la crisis que sufre el sector, como por las modificaciones que se esperan en la norma de calidad, recientemente acordadas. En este entorno en el que existe una reducción importante de los márgenes comerciales en todos los eslabones de la cadena de valor del jamón ibérico de bellota, adquiere importancia el estudio de su estructura y funcionamiento, la determinación de los aspectos que mejoran la eficiencia económica a lo largo de la misma y su concordancia a lo largo de ella. Así mismo, un sector de los consumidores comienza a buscar productos de calidad, se interesa por productos con determinados etiquetados que garantizan la calidad o unas determinadas prácticas de producción y elaboración, como sucede con los productos ecológicos. Existen numerosos estudios sobre distintos aspectos del sector porcino ibérico, realizados por distintas instituciones, como universidades, instituciones privadas y proyectos europeos. En general, se centran en la mejora de la producción de los cerdos ibéricos o en la mejora de la elaboración de los jamones. La novedad de la investigación realizada en la presente Tesis Doctoral reside en el estudio de los aspectos que determinan la mayor eficiencia económica de la cadena de valor del jamón ibérico de bellota de la denominación de origen de Guijuelo, y en las características que aporta al jamón ibérico de bellota la producción ecológica frente a la convencional. Resumen Los objetivos planteados en esta investigación son la mejora de la cadena de valor del jamón ibérico de bellota de la denominación de origen de Guijuelo, mediante el estudio de la problemática estructural y de funcionamiento de la misma. Como objetivos específicos se proponen la mejora de la eficiencia económica en las relaciones comerciales entre los distintos eslabones de la cadena de valor, y el impulso de la oferta de los productos ecológicos de ibérico, mediante el estudio comparativo de las producciones convencionales y ecológicas. Para alcanzar estos objetivos la metodología utilizada es la cadena de valor agroalimentaria, utilizando como herramientas de análisis el método Delphi y la realización de un análisis DAFO del sector porcino ibérico. Las fuentes de información primarias utilizadas proceden por una parte de la colaboración realizada en el proyecto europeo Q-Porkchains, coordinado por el Dr. Jacques H. Trienekens, y por otra parte de los cuestionarios especialmente diseñados para el análisis Delphi realizado. Las fuentes de información secundarias proceden de artículos académicos publicados, de artículos de revistas especializadas en el sector y de informes y estadísticas publicados por el Ministerio de Agricultura, Alimentación y Medio Ambiente. Las conclusiones de la investigación son las siguientes. Las relaciones comerciales de la cadena de valor estudiada están gestionadas, ya que se otorga gran valor a las relaciones comerciales basadas en la confianza, tanto en el aprovisionamiento de productos como en la venta de los mismos en cada eslabón. Sin embargo, no se gestiona adecuadamente la gama de productos que se oferta a lo largo de la cadena de valor, puesto que los eslabones de la misma obtienen diferente eficiencia económica para el mismo producto. Por otra parte, aunque la denominación de origen de Guijuelo es una marca conocida por el consumidor, el esfuerzo por tener una marca colectiva de calidad no ha sido totalmente satisfactorio, en especial para el eslabón de la distribución. Por esta razón, es importante resaltar que es recomendable la creación de una marca propia que cuide la calidad con especial atención, modificando incluso las empresas integrantes de la cadena de valor si el objetivo de calidad no coincide. Es importante garantizar la calidad del producto al consumidor, mediante la trasmisión la información generada por los informes de inspección y certificación realizados por las entidades correspondientes en relación a la norma de calidad de los productos de cerdo ibérico y por el Consejo Regulador de Guijuelo. Se requiere un estudio detallado de los posibles nichos de mercado para llegar a los clientes que buscan un producto de calidad diferenciada como es el jamón ibérico de denominación de origen de Guijuelo. Dentro de los posibles clientes debe tenerse en consideración al colectivo de personas alérgicas, ya que no se encuentran con facilidad en el mercado productos cárnicos de cerdo libres de alérgenos. Por último, la innovación es muy importante en este sector, y pueden ofertarse nuevos productos que ayuden al acortamiento de la cadena de valor, como podría ser la carne fresca de cerdo ibérico de bellota. La producción ecológica de porcino ibérico, en la actualidad no es significativa. El manejo que se realiza de los cerdos ibéricos convencionales de bellota es muy similar al manejo que se realiza de los cerdos ecológicos, salvo en la alimentación que reciben los cerdos ibéricos antes del cebo en montanera y en los medicamentos permitidos en ambas producciones. La producción de porcino ecológico de bellota puede ser interesante para la exportación. Los jamones ibéricos de bellota dispondrían de un sello que garantiza un manejo tradicional –como se realiza en muchas explotaciones extensivas de cerdos ibéricos de bellota-, y que es apreciado por los consumidores de otros países, dispuestos a pagar por productos de calidad diferenciada. Este tipo de producción quizá podría solventar la limitación al ámbito nacional de la norma de calidad de los productos de cerdo ibérico. La falta de claridad y unanimidad en el sector sobre la calidad de los productos de ibéricos que se percibe en los cambios previstos en la legislación, y el interés del eslabón de la industria elaboradora de jamones en calidades no ligadas a producciones extensivas sino intensivas, por su mayor volumen de ventas y sus mejores rendimientos, mueven a los productores de “ibérico puro de bellota” a desmarcarse del sector “ibérico”, donde el peso del producto ibérico cruzado de pienso tiene mucho peso en las decisiones que se toman. The Iberian pork industry is a typically Spanish industry. The associated image by the consumer to these products corresponds to products made from Iberian pigs in extensive farms (meadows), and fattened in open range. However, according to data released by the Ministry of Agriculture, Food and Environment, more than 70 percent of the Iberian pigs produced in Spain are raised on factory farms. The Iberian pork industry is in process of change, both by modifications resulting from the crisis in the sector, and the expected ones in the quality standard, recently agreed. In this environment where there is a significant reduction in trade margins in all links of the value chain of Iberian ham, becomes important to study its structure and operation, identifying the aspects that improve economic efficiency along the value chain and their concordance along it. Likewise, part of the consumers begins searching for quality products, they are interested in certain products that guarantee some sort of quality or production and processing practices, like organic products. There are several studies on various aspects of the Iberian pork industry, made by different institutions, such as universities, private institutions and some European projects. In general, their goal is focused on improving the Iberian hog production or on improving the elaboration of hams. The novelty of the research conducted in this PhD thesis lies in the study of the aspects that determine the economic efficiency of the value chain of Iberian ham from Guijuelo designation of origin, and the comparison between the features that organic or conventional production of Iberian ham brings to it. The objectives propound in this research are the improvement of the value chain of Iberian ham from Guijuelo designation of origin, through the study of its structural and operational problematic. The proposed specific objectives are the improvement of the economic efficiency Resumen in trade relations between the different links in the value chain, and the promotion of the supply of Iberian organic pork products, through the comparative study of conventional and organic productions. In order to achieve these objectives, the used methodology is the agrifood value chain, using as analysis tools the Delphi method, and a SWOT analysis of the Iberian pork industry. The primary sources of information come partly from the collaboration in the European project Q-Porkchains, coordinated by Dr. Jacques Trienekens, and partly from the questionnaires specially designed for the Delphi analysis performed. The secondary sources come from published academic papers, specialized journal articles and reports published by the Ministry of Agriculture, Food and Environment. The research conclusions are as follows. Trade relations in the studied value chain are managed, as it is granted a great value to business relationships based on trust, both in the supply of products and in the sale in each link. However, the portfolio that is offered throughout the value chain is not properly managed, since the economic efficiency obtained for the same product is different in each link. Moreover, although the designation of origin of Guijuelo is a well-known brand, the effort made to acquire a collective quality trademark has not been entirely satisfactory, especially in the distribution link. Due to it, it is important to highlight that it is recommended to create a brand focused on quality, and indeed to change the firms integrating the vale chain, if the goal is not shared by all the companies. It is essential to ensure the quality of the product to the consumer, through the transmission of the available information related to the quality standard of Iberian pork products and of the Guijuelo Regulating Council. A detailed study of potential niche markets is required, in order to reach customers looking for a differentiated quality product as Iberian ham of Guijuelo designation of origin. It should be taken into consideration the group of allergy sufferers as potential customers, as they do not easily find pork products in the market free of allergens. Innovation is very important in this industry, and new products could be commercialized that help to shorten the value chain, as fresh acorn Iberian pork. Nowadays, the organic production of Iberian pork products is not significant. The operation is very similar in both conventional and organic production of Iberian pork products, except in the food received by Iberian hogs and the sort of medicinal treatments allowed in each production. The organic acorn Iberian pork production could be interesting for export. Acorn Iberian hams would have a well-known hallmark, which guarantees a traditional production, -as it is done in many extensive holdings of Iberian acorn-pigs-, and that is appreciated by consumers in other countries This niche of consumers could pay for differentiated quality products. Perhaps, this sort of production could solve the limitation to national scope of the quality standard of Iberian pork products. The lack of clarity and unanimity in the industry on the quality of Iberian pork products has been perceived in the agreed changes of the legislation as well as the interest of the processing industry in hams of quality categories which are not linked to extensive but intensive productions, due to their higher sales volume and better yields. This situation pushed "acorn pure Iberian " pigs farmers to split from the Iberian industry, where the importance of cross Iberian pig from intensive farms is growing so high that they can influence the negotiations and decisions taken inside and outside the industry.