Lithologic Control on the Scaling Properties of the First-Order Streams of Drainage Networks: A Monofractal Analysis

The movement of water through the landscape can be investigated at different scales. This study dealt with the interrelation between bedrock lithology and the geometry of the overlying drainage systems. Parameters of fractal analysis, such as fractal dimension and lacunarity, were used to measure and quantify this relationship. The interrelation between bedrock lithology and the geometry of the drainage systems has been widely studied in the last decades. The quantification of this linkage has not yet been clearly established. Several studies have selected river basins or regularly shaped areas as study units, assuming them to be lithologically homogeneous. This study considered irregular distributions of rock types, establishing areas of the soil map (1:25,000) with the same lithologic information as study units. The tectonic stability and the low climatic variability of the study region allowed effective investigation of the lithologic controls on the drainage networks developed on the plutonic rocks, the metamorphic rocks, and the sedimentary materials existing in the study area. To exclude the effect of multiple in- and outflows in the lithologically homogeneous units, we focused this study on the first-order streams of the drainage networks. The geometry of the hydrologic features was quantified through traditional metrics of fluvial geomorphology and scaling parameters of fractal analysis, such as the fractal dimension, the reference density, and the lacunarity. The results demonstrate the scale invariance of both the drainage networks and the set of first-order streams at the study scale and a relationship between scaling in the lithology and the drainage network.

House of Would

Proyecto House of Would

Prefab wooden house, Pedrezuela

Proyecto wooden house

Hacia la nueva sociedad comunista: la casa de transición del Narkomfin, epílogo de una investigación = Towards the new communist society: the transition House of Narkomfin, a research epilogue

En el contexto de inestabilidad y cambio vivido en la URSS durante la década de 1920, un grupo de arquitectos dirigido por Moisei Ginzburg abordó el tema del alojamiento de masas. Su misión no sería sólo dar solución al problema de la vivienda, sino redefinirla como el marco adecuado para una sociedad sometida a un cambio sin precedentes. La respuesta se desarrolló a través de un proceso de investigación que duró más de cinco años, en tres aproximaciones sucesivas que culminaron con el edificio Narkomfin. La primera, de carácter conceptual, se formalizó en el Concurso Amistoso de 1926. La segunda se articuló a través de la investigación del Stroikom bajo premisas científicas y metodológicas. Finalmente, las conclusiones tipológicas alcanzadas en esta segunda etapa se materializaron en la construcción de algunos ejemplos, entre los que destacó el edificio Narkomfin. Este último acercamiento, de carácter empírico, ha sido tradicionalmente examinado por los expertos como un hecho aislado. Sin embargo, su estudio debe trascender necesariamente el genio del autor-creador en favor del proceso de investigación al que pertenece. Sólo desde este punto de vista cobra sentido la consideración de Ginzburg sobre su propio edificio como un medio propositivo y no impositivo: un proyecto concebido como una herramienta de transición hacia una sociedad más avanzada.

Geomorphological analysis and evolution of an altered floodplain drainage system. The case of the Partido Stream (Spain)

The Partido Stream is a small torrential course that flows into the marsh of the Doñana National Park, an area that was declared a World Heritage Site in 1994. Before 1981, floods occurred, and the stream overflowed onto a floodplain. As an old alluvial fan, the floodplain has its singular orography and functionality. Fromthe floodplain, several drainage channels, locally called caño, discharged into themarsh. The Partido Streamhad themorphology of a caño and covered approximately 8 km from the old fan to the marsh. The stream was straightened and channelised in 1981 to cultivate the old fan. This resulted in floods that were concentrated between the banks in the following years, which caused the depth of water and the shear stress to increase, thus, scouring the river bed and river banks. In this case, the eroded materials were carried towards the marsh where a new alluvial fan evolved. Control measures on the old fan were implemented in 2006 to stop the development of the new alluvial fan downstream over the marsh. Thus, the stream would partially recover its original behaviour that it had before channelisation, moving forwards in a new, balanced state. The present study describes the geomorphological evolution that channelisation has caused since 1981 and the later slow process of recovery of the original hydraulic-sedimentation regime since 2006. Additionally, it deepens the understanding of the original hydraulic behaviour of the stream, combining field data and 2D simulations.

The House of the Infinite

The House of the Infinite / Alberto Campo Baeza

Casa Guerrero. Zahora (Cádiz) = Guerrero House. Zahora (Cádiz)

Casa Guerrero. Zahora (Cádiz) = Guerrero House. Zahora (Cádiz) Texto en español e inglés.

Casa Asencio, Chiclana de la Frontera (España) = Asencio House, Chiclana de la Frontera (Spain)

Casa Asencio, Chiclana de la Frontera (España) = Asencio House, Chiclana de la Frontera (Spain) Texto en español e inglés

Casa de Blas, Sevilla la Nueva (Madrid) = De Blas House, Sevilla la Nueva (Madrid)

Casa de Blas, Sevilla la Nueva (Madrid) = De Blas House, Sevilla la Nueva (Madrid). Texto en español e inglés

Moliner House

Moliner House