Large Rivers: Geomorphology and Management explores an important topic in geomorphology and sedimentology: the form and function of major rivers. Our knowledge of the big rivers of the world is limited. It is currently difficult to recognise large rivers of the past from relict sedimentary deposits or to structure management policies for long international rivers.
This exciting book brings together a set of papers on large rivers of the world, as a unique introduction to a demanding subject. The book includes thirty chapters and is organised into three sections. The first part is on the environmental requirements for creating and maintaining a major river system. The second is a collection of case studies on 14 large rivers from different continents, covering a range of physical environments. The third section includes chapters on the measurement and management of large rivers.
Die Inhaltsangabe kann sich auf eine andere Ausgabe dieses Titels beziehen.
Avijit Gupta, School of Geography, University of Leeds, UK, and Visiting Scientist, Centre for Remote Imaging, Sensing and Processing, National University of Singapore.
Large Rivers: Geomorphology and Management explores an important topic in geomorphology and sedimentology: the form and function of major rivers. Our knowledge of the big rivers of the world is limited. It is currently difficult to recognise large rivers of the past from relict sedimentary deposits or to structure management policies for long international rivers. This volume brings together a substantial number of chapters on large rivers to form possibly the first structured introduction to this demanding subject. The distinguished contributors to Large Rivers have a long association with rivers of considerable dimensions.
The book includes thirty chapters organised into three sections. The first part is on the environmental requirements for creating and maintaining a major river system. The second is a collection of case studies on 14 large rivers from different continents, covering a range of physical environments. The third section includes chapters on the measurement and management of large rivers.
This comprehensive volume should be essential reading for postgraduate students and researchers in fluvial geomorphology, hydrology, sedimentary geology, and river management. It will be of relevance to engineers and environmental consultants in the private and public sectors working on major rivers of the world. Large Rivers is a pioneering study that hopefully will generate enough interest and controversy to push the boundaries of our knowledge related to big rivers. It may even contribute towards preventing their channels and basins from random or organised mismanagement.
Large Rivers: Geomorphology and Management explores an important topic in geomorphology and sedimentology: the form and function of major rivers. Our knowledge of the big rivers of the world is limited. It is currently difficult to recognise large rivers of the past from relict sedimentary deposits or to structure management policies for long international rivers. This volume brings together a substantial number of chapters on large rivers to form possibly the first structured introduction to this demanding subject. The distinguished contributors to Large Rivers have a long association with rivers of considerable dimensions.
The book includes thirty chapters organised into three sections. The first part is on the environmental requirements for creating and maintaining a major river system. The second is a collection of case studies on 14 large rivers from different continents, covering a range of physical environments. The third section includes chapters on the measurement and management of large rivers.
This comprehensive volume should be essential reading for postgraduate students and researchers in fluvial geomorphology, hydrology, sedimentary geology, and river management. It will be of relevance to engineers and environmental consultants in the private and public sectors working on major rivers of the world. Large Rivers is a pioneering study that hopefully will generate enough interest and controversy to push the boundaries of our knowledge related to big rivers. It may even contribute towards preventing their channels and basins from random or organised mismanagement.
Avijit Gupta
School of Geography, University of Leeds, Leeds LS2 9JT, UK and Centre for Remote Imaging, Sensing and Processing, National University of Singapore, Singapore 119260
1.1 A BOOK ON LARGE RIVERS
Large rivers are important components of continental landforms. A number of them have been associated with the growth and development of human civilization in their fertile valleys. The structured water utilization in the Nile Valley is an excellent example. Several have been impounded, starting from the second quarter of the twentieth century. The Hoover Dam over the Colorado is one of the early huge engineering structures, the Three Gorges Dam over the Changjiang (Yangtze) the most recent one.
In spite of these rivers being physical marvels and resources utilized by a large number of people, our knowledge about their form, evolution or function remains limited. This is possibly due to logistical problems, as case studies in the fields of geomorphology, sedimentology or river ecology are generally on smaller rivers that are easier to investigate, model or manage. For example, direct measurements of sediment are not regularly available for a number of these big rivers, requiring indirect estimates of sediment load. Our knowledge of these rivers also varies. A lot more is known about the Mississippi or the Colorado than the Zambezi. The Nile has been measured for thousands of years but not the Congo. The Amazon is attracting a very large number of researchers from a wide range of institutions, countries, and specializations but such large-scale national or international endeavours are rare for other tropical rivers. Over the last four decades, a compilation of information on channel form, sediment, and mobility of the Lower Brahmaputra has built up, a dataset not available for its upper course. We have started to comprehend the interconnection between the flood pulse, sediment flux, and riverine ecology in these rivers. But the coverage is not uniform and for a number of major rivers our knowledge is inadequate for both generalization and planning. For example, at the current level of understanding, it is difficult to predict the effect of the expected climate changes on large rivers, a task that will undoubtedly become essential for the next generation of scholars.
This book is an attempt to bring together a number of papers on big rivers. It is not a complete coverage but provides an introduction to geomorphology and the management of rivers of large dimension. Certain rivers and topics have been hard to cover because of their complexity and location and a couple of the chapters originally planned did not arrive, but overall this is a unique volume not attempted before at this scale.
The book is designed in three sections. The first section is on the environmental requirements for creating and maintaining a large river. In that sense, the chapters included are valuable generalizations based on existing knowledge. The second section is a collection of case studies on big rivers flowing through a range of physical environments. The third section is on the measurement and management of large rivers and their basins. Almost all chapters have been rather demanding to write, but the end product is a bold pioneering volume that hopefully will generate enough interest and controversy to push the boundary of our knowledge related to large rivers. It may even contribute towards saving their channels and basins from both random and organized mismanagement.
1.2 WHAT IS A LARGE RIVER?
If we are to list the largest rivers in the world, all of us would probably list the same 15 or 20 rivers, but a proper definition is elusive. Potter, in his 1978 paper on the significance and origin of big rivers, listed four properties that could be considered for this purpose: size of the drainage basin, length of the river, volume of sediment transported, and water discharge. He used river length and drainage basin size to identify the 50 largest rivers of the world. All except one of these rivers were more than [10.sup.3] km long and the smallest drainage basin was [10.sup.5] [km.sup.2]. These 50 streams collectively drain about 47% of the continental surface, excluding Greenland and Antarctica (Potter, 1978). Inman and Nordstrom (1971) listed rivers with drainage areas above [10.sup.5] [km.sup.2], with the Amazon ranked as 1 and the Po as the last one to qualify at rank 58.
Quality data on the two other criteria of large rivers, discharge of water and especially discharge of sediment, are not always available. Meade (1996) listed the first 25 rivers for both water and average suspended sediment discharges to the coastal zone. It is difficult to determine the total sediment load of a large river and, as Meade has pointed out, bed load is especially difficult to measure. The two lists, however, do not coincide, as certain rivers such as the Zambezi or Lena carry a large water discharge but their sediment loads are low. Impoundments have reduced the sediment load of rivers such as the Mississippi-Missouri, and almost removed it for the Nile or the Colorado. Impoundments have also reduced the water discharge of a number of major rivers (Meade, 1996). The Huanghe now does not reach the sea for about half the year. A river that should be in the list because of its former glory may not qualify on current performance. Recently Hovius tabulated the morphometric, climatic, hydrologic, transport and denudation data for 97 river basins, all of which measured above 2.5 x [10.sup.4] [km.sup.2] (Hovius, 1998). Miall raised the question of identifying big rivers of the past, and attempted to define the 'bigness' in rivers based on previous studies (Miall, 2006).
Qualitatively, therefore, a large river carries a very big discharge, is long, has a large drainage basin and, commonly, but not always, annually transports a large volume of sediment. Of these, a huge volume of water flowing down the channel is probably the commonest expectation of a large river in a natural state, but given the variations that occur among three other properties, a rigorous definition is impossible. Instead it is expedient to list the top twenty or so and base our discussion on their characteristics. Table 1.1, compiled from various sources, is a comparison of the top 24 rivers of the world, selected on basis of their discharge. The discharge figures are from Meade (1996). Other measurements have been derived from a range of sources that are listed below Table 1.1. These measurements, however, differ between sources, especially regarding the area of the basins which has been resolved by rounding off to [10.sup.6] [km.sup.2]. Even at this scale there are discrepancies. Given the scale, perhaps it is inevitable that different figures will be quoted by different authors. A relationship exists between river length and drainage basin areas (Leopold et al., 1964; Potter, 1978) but not between the other variables. Variations in basin geology, relief, and hydrology are responsible for the scatter.
The great length of these rivers allows them to flow across a range of environments. The Changjiang, Mekong, and Zambezi, for example, flow in and out of rock gorges into alluvial basins. Morphological and behavioural adjustments happen at each...
„Über diesen Titel“ kann sich auf eine andere Ausgabe dieses Titels beziehen.
Anbieter: Phatpocket Limited, Waltham Abbey, HERTS, Vereinigtes Königreich
Zustand: Good. Your purchase helps support Sri Lankan Children's Charity 'The Rainbow Centre'. Ex-library, so some stamps and wear, but in good overall condition. Our donations to The Rainbow Centre have helped provide an education and a safe haven to hundreds of children who live in appalling conditions. Bestandsnummer des Verkäufers Z1-H-014-02358
Anzahl: 2 verfügbar