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This is a little bit about what can be found inside. The book provides an introduction to the discipline of hydrology, with its different branches and related technologies, including surface and groundwater hydrology; water quality; groundwater aquifers; hydrogeology; and surface water lakes, rivers and wetlands. It also discusses natural sources of water such as rain and snowfall, as well as how they affect the environment. The reader will come to know not only how to identify problems in these areas - by their causes or consequences - but also how to provide solutions through the use of hydrological techniques such as mathematical modeling (in terms of both theory and practice). I think it is a well-written book, although I have to say that reading it isn't so easy. Solucionario Ven Te Chow Hidrologia Aplicada by Ricardo Pozo Pozo PREFACE. The course of this work has been shaped by the following considerations. First, the hydrological science has grown continuously throughout history, now proposed as a unified discipline, which will have an important role in the development of industry and agriculture. This fact has required that its principles be studied thoroughly to evaluate ways of applying them for this purpose and that they be classified according to their application. This is the reason why the application of hydrology to engineering problems has been investigated. Second, hydraulic studies are often invalidated by lack of precision in knowing the precise state of the waters. When this happens it requires that precise knowledge be obtained about these waters, their levels and basins. Third, in hydrological engineers there exists a lack of development regarding physical methods for solving problems which are emphasized in other domains, such as in physics and mechanics. Within this context it is necessary to study not only theoretical models but also how they can be applied to engineering problems. PREFACE Regarding natural freshwater, surface water reservoirs may be divided into two categories: "freshwater lakes" and "freshwater wetlands. The lakes are often large bodies of water, with many islands and small bays, with the surface usually unbroken by rapids or shallow channels. The lakes are constituted by streams which drain into them, and which create several levels of "freshwater lakes" where the highest level is the "lakeshore". A "freshwater swamp", or "moist bog" is a wetland formed by slow-moving rivers which drain to coastal estuaries; they differ from freshwater marshes because they lose water to the ocean. Freshwater marshes are composed of 1) open lagoons, often without islands; 2) lakes, either partly or completely surrounded by marshland; or 3) large areas of swamp. Unlike rivers, streams have the highest average speed occurring near the location of their origin. The average speed of a stream is lower than that of a river. The annual mean velocity for fresh water rivers is around 0.6 meters per second and for lake and stream channels it is about 0.17 meters per second: freshwater streams and rivers flow with a velocity sufficient to overcome the impact of waves and currents resulting in erosion and sedimentation. Solucionario Ven Te Chow Hidrologia Aplicada cfa1e77820