Between 1808 and 1814 England was committed to an expensive and bloody campaign against the French invasion of the Iberian Peninsula. The Peninsular War, as it came to be known, was initially celebrated as a war of national independence that attracted widespread support. Soon after, it was characterised by political scandal and public controversy. Literary scholars have devoted much attention to the political, social and cultural effects of the French Revolution, but have written surprisingly little about the later years of the campaign against Napoleonic France. The principle objective of this thesis is to offer the first in-depth study of English theatre during the Peninsular War. It considers the most popular plays in performance, and asks what their staging, publication, and reception history reveal about a nation’s literary tastes and its political self-awareness. Sheridan’s Pizarro, a play about the Spanish conquest of Peru, was one of the most successful plays on the Romantic stage. A close analysis of this play considers its popularity between 1799 and 1815, and what it suggests about the flexibility of the contemporary repertoire system. Audiences’ ability to ascribe topical inflections to old plays helps explain the demand for Shakespeare and the bard’s political import to wartime audiences. This thesis explores the London patent stages and popular minor theatres, where programmes were restricted to song, dance, and spectacle. It also offers a case study of provincial theatre in Bristol, underscoring the significant limitations in assumptions that the metropolitan stage was representative of national trends. Archival research on the London and Bristol stages has been crucial to this study, which is based on an examination of playbills, memoranda, letters, playtexts, and prints. The newsprint and cartoons discussed offer an important political and historical framework, suggestive of the cultural expectations likely to have influenced contemporary playgoers.

This thesis argues for the deep implication of William Wordsworth’s writings over the period 1794 to 1814 in contemporary discourses of the Gothic. My investigation pivots upon the analogy offered in the preface to The Excursion (1814) between the incomplete epic poem The Recluse and a ‘gothic Church’, and aims, through a reconstruction of its literary and historical contexts, to establish the interpretative value of this figure in reading Wordsworth. I begin with a survey of previous critical approaches to, and a new close reading of, Wordsworth’s Gothic figure for his œuvre. I then trace the history of Gothic as a term in British public discourse since the English Revolution, showing how its contested status in the Revolution controversy of the 1790s inflects such texts as the preface to Lyrical Ballads (1800), the ‘Liberty’ sonnets of Poems, in Two Volumes (1807), and the Preamble to The Prelude. I then move to a series of detailed historical readings of Wordsworth’s key Gothic texts, starting with Salisbury Plain (1794). Recovering the network of associations that made Salisbury Plain legible to Wordsworth in 1793-4 as a map of British history, I show how the poem first subverts and then restores the English Gothic narrative of ‘Celtic night’ giving way to ‘present grandeur’. I then turn to Wordsworth’s Burkean prose tract on the Napoleonic Wars in Spain, The Convention of Cintra (1809), reading it in the context of the Gothic imagery of the conflict, and then arguing on this basis that it forms a vital part of the ‘gothic Church’ of The Recluse. Building upon this reading, I then argue that The Excursion’s advocacy of Andrew Bell’s ‘Madras’ system of ‘tuition by the scholars themselves’ shows Wordsworth’s progressive Gothic politics in action. In concluding, I turn to reconsider, in the light of the preceding chapters, in what sense Wordsworth can be called a Gothic poet.

En la horticultura intensiva española la mayor parte de las exportaciones procede de los cultivos de invernadero, localizados en Almería, Murcia y Alicante, donde se ha centrado el presente estudio. Actualmente la posición competitiva no presenta amenazas muy graves pero tampoco muestra una etapa creciente. Exportaciones y precios soportan la competencia de otros países del área mediterránea, con los cuales España debe competir en capital y en tecnología elevando el nivel de equipamiento de los invernaderos. Ante unas exigencias de reestructuración de las instalaciones actuales, no aplazables, se plantea la presente tesis con el fin de conocer el estado actual de la tecnología y su evolución y, además, las características de las explotaciones y la actitud de sus titulares respecto a las innovaciones necesarias. Las fuentes de información se han basado en una toma de precios en origen del tomate y pimiento, como principales productos hortícolas, y en una encuesta, realizada en 242 explotaciones, mediante muestreo proporcional estratificado, en las zonas de El Ejido (Almería), Valle del Guadalentín y Campo de Cartagena (Murcia) y Sur de Alicante. El análisis de la información tuvo una primera parte dedicada a los precios, con el cálculo de la tendencia y la estacionalidad y la aplicación de modelos ARIMA. La finalidad ha sido conocer la evolución de las rentas de los productores, efectuar predicciones, y establecer una relación entre los precios y la tecnología adoptable. El tratamiento de los datos de la encuesta con sus resultados comprende la mayor parte del contenido del trabajo. Se aplicó el análisis estadístico univariante a las características estructurales de explotaciones e invernaderos y el bivariante, con contraste de independencia, para determinar relaciones de interés entre los factores que influyen en los procesos de innovación. / García Martínez, MDC. (2009). La adopción de tecnología en los invernaderos hortícolas mediterráneos [Tesis doctoral no publicada]. Universitat Politècnica de València. https://doi.org/10.4995/Thesis/10251/6472 / Palancia

Spanish Republican philosophers in exile defended the Second Republic, legally proclaimed on April 14, 1931. They embraced the anti-fascist cause rising in the 1920s and the 1930s in Europe. During the Civil War, which lasted three years, they stood among the people. 1939 saw the victory of General Francisco Franco, supported by Nazi Germany and the Italy of Mussolini. Threatened with death, they had no choice but to escape from Spain. Some intellectuals experienced French concentration camps but, for the most part, they found refuge in Latin America, especially in Mexico and Venezuela. In exile, they swore to remain loyal to the Second Republic and to the spirit of the Spanish people. Moved by liberal views and humane ideals, these philosophers belonged to the vanquished, as those everywhere in Europe who rose against Fascist barbarity. As a result, their respective works are still widely unknown today – despite relentless efforts made to promote their thought to a larger audience for over half a century. In addition to the historical context of crisis during the interwar period, the situation of Spanish philosophy itself is suggestive. Indeed, Spanish philosophy was institutionalised at the beginning of the twentieth century only: the Schools of Madrid and Barcelona were created. These politics of cultural and intellectual renovation are first bestowed upon the generation of philosophers I study, born in the 1900s. When the Spanish War erupts, they had become professionals of international recognition. This shows the actual limits of academic philosophy, incapable of acknowledging unorthodox ways of philosophising. The experience of exile itself serves in my opinion as a catalyst: Spanish Republican philosophers in exile seek emancipation from academic conventions to philosophise freely; that is, in Spanish and according to the spirit of the people. No doubt “poetic reason” – the true invention of Spanish Republican exile – stems from this ideal of autonomous thinking.

Evapotranspiration is a nexus for planetary energy and carbon cycles, as yet poorly constrained. Here I use stable isotopes of oxygen and hydrogen to partition flux of water due to plant transpiration from the direct evaporative flux from soils, water bodies and plant. The study areas, Langat and Kelantan watersheds represent examples of domains dominated by the respective Southwest and Northeast monsoons on the two sides of the main orographic barrier (Titiwangsa mountain range). Mean annual rainfall for the Langat watershed, obtained from 30 years of hydrological data, is 2145 ± 237 mm. Tentatively, 48% of this precipitation returns to the atmosphere via transpiration (T), with 33% partitioned into discharge (Q), 8% into interception (In), and 11% into evaporation (Ed). In the Kelantan watershed, the mean annual rainfall, also based on the 30 year hydrological data, is 2383 ± 120 mm. Similar to Langat, the T accounts for 43% of precipitation (P), 45% is discharged into South China Sea (Q), 12% partitioned into interception (In) and tentatively 0% for evaporation (Ed). Ed for the Langat watershed represents only a small proportion in terms of volumetric significance, up to almost ~11% with strong effect on the isotopic fingerprints of waters associated with the summer Southwest Monsoon (SWM). Note, however, that insignificant Ed for the Kelantan watershed may be an artefact of rain and river water sampling at only coastal downstream portion of the watershed. High humidity (80%) also was recorded for the Malaysian Peninsula watershed. T appropriates about half of all solar energy absorbed by the continents, here ~1000*103 g H2O m-2 yr-1 similar to other tropical regions at 900-1200*103 g H2O m-2 yr-1. The associated carbon fluxes are ~ 1300 g C m-2yr-1, independent of P. Vegetation responses to solar irradiance, via T and photosynthesis reflects the importance of stomatal regulation of the water and carbon fluxes. In order to maintain high transpiration in the tropical region, “constant” water supply is required for continuous pumping of water that delivers nutrients to the plant, suggesting that water and carbon cycle are co-driven by the energy of the sun. The existence of the water conveyor belt may be precondition for nutrient delivery, hence operation of the carbon cycle. Potentially, this may change our perspective on the role that biology plays in the water cycle. In such perspective, the global water cycle is the medium that redistributes the incoming solar energy across the planet, and the anatomical structures of plants then help to optimize the loop of energy transfer via evaporation and precipitation in the hydrologic cycle. The main features of aquatic geochemistry of the Langat and Kelantan rivers inferred from the Principal Component Analysis are controlled by three components that explain 80% and 82% of total variances. These components are reflecting of the geogenic factor with superimposed pollution, the latter particularly pronounced in urbanized sections of the Langat river and dominant in downstream of the Kelantan river. There is no correlation between seasonal variations in major ion chemistry and environmental variables such as precipitation, discharge, temperature or solar activity.

Evapotranspiration is a nexus for planetary energy and carbon cycles, as yet poorly constrained. Here I use stable isotopes of oxygen and hydrogen to partition flux of water due to plant transpiration from the direct evaporative flux from soils, water bodies and plant. The study areas, Langat and Kelantan watersheds represent examples of domains dominated by the respective Southwest and Northeast monsoons on the two sides of the main orographic barrier (Titiwangsa mountain range). Mean annual rainfall for the Langat watershed, obtained from 30 years of hydrological data, is 2145 ± 237 mm. Tentatively, 48% of this precipitation returns to the atmosphere via transpiration (T), with 33% partitioned into discharge (Q), 8% into interception (In), and 11% into evaporation (Ed). In the Kelantan watershed, the mean annual rainfall, also based on the 30 year hydrological data, is 2383 ± 120 mm. Similar to Langat, the T accounts for 43% of precipitation (P), 45% is discharged into South China Sea (Q), 12% partitioned into interception (In) and tentatively 0% for evaporation (Ed). Ed for the Langat watershed represents only a small proportion in terms of volumetric significance, up to almost ~11% with strong effect on the isotopic fingerprints of waters associated with the summer Southwest Monsoon (SWM). Note, however, that insignificant Ed for the Kelantan watershed may be an artefact of rain and river water sampling at only coastal downstream portion of the watershed. High humidity (80%) also was recorded for the Malaysian Peninsula watershed. T appropriates about half of all solar energy absorbed by the continents, here ~1000*103 g H2O m-2 yr-1 similar to other tropical regions at 900-1200*103 g H2O m-2 yr-1. The associated carbon fluxes are ~ 1300 g C m-2yr-1, independent of P. Vegetation responses to solar irradiance, via T and photosynthesis reflects the importance of stomatal regulation of the water and carbon fluxes. In order to maintain high transpiration in the tropical region, “constant” water supply is required for continuous pumping of water that delivers nutrients to the plant, suggesting that water and carbon cycle are co-driven by the energy of the sun. The existence of the water conveyor belt may be precondition for nutrient delivery, hence operation of the carbon cycle. Potentially, this may change our perspective on the role that biology plays in the water cycle. In such perspective, the global water cycle is the medium that redistributes the incoming solar energy across the planet, and the anatomical structures of plants then help to optimize the loop of energy transfer via evaporation and precipitation in the hydrologic cycle. The main features of aquatic geochemistry of the Langat and Kelantan rivers inferred from the Principal Component Analysis are controlled by three components that explain 80% and 82% of total variances. These components are reflecting of the geogenic factor with superimposed pollution, the latter particularly pronounced in urbanized sections of the Langat river and dominant in downstream of the Kelantan river. There is no correlation between seasonal variations in major ion chemistry and environmental variables such as precipitation, discharge, temperature or solar activity.