Geological Survey Professional Paper
Author: Geological Survey (U.S.)
Publisher:
Published: 1966
Total Pages: 656
ISBN-13:
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Author: Geological Survey (U.S.)
Publisher:
Published: 1966
Total Pages: 656
ISBN-13:
DOWNLOAD EBOOKAuthor: George Irving Smith
Publisher:
Published: 1978
Total Pages: 64
ISBN-13:
DOWNLOAD EBOOKAuthor:
Publisher:
Published: 1965
Total Pages: 88
ISBN-13:
DOWNLOAD EBOOKAuthor: Geological Survey (U.S.)
Publisher:
Published: 1949
Total Pages: 260
ISBN-13:
DOWNLOAD EBOOKAuthor: Geological Survey (U.S.)
Publisher:
Published: 1988
Total Pages: 316
ISBN-13:
DOWNLOAD EBOOKAuthor: Benno P Warkentin
Publisher: Elsevier
Published: 2006-04-18
Total Pages: 573
ISBN-13: 0080477879
DOWNLOAD EBOOKThe history of science discipline is contributing valuable knowledge of the culture of soil understanding, of the conditions in society that fostered the ideas, and of why they developed in certain ways. This book is about the progressive "footprints made by scientists in the soil. It contains chapters chosen from important topics in the development of soil science, and tells the story of the people and the exciting ideas that contributed to our present understanding of soils. Initiated by discussions within the Soil Science Society of America and the International Union of Soil Sciences, this book uniquely illustrates the significance of soils to our society. It is planned for soils students, for various scientific disciplines, and for members of the public who show an increasing interest in soil. This book allows us to answer the questions: "How do we know what we know about soils? and "How did one step or idea lead to the next one?The chapters are written by an international group of authors, each with special interests, bound together by the central theme of soils and how we came to our present understanding of soils. Each concentrate on soil knowledge in the western world and draw primarily on written accounts available in English and European languages. Academics, graduate students, researchers and practitioners will gain new insights from these studies of how ideas in soil science and understanding of uses of soils developed.* Discusses tracing soils knowledge accumulated from Roman times, first by soil users and after 1800s by scientists* Offers ideas about how soils knowledge was influenced by the social context and by human needs* Combines the history of ideas with scientific knowledge of soils* Written by chapter authors who combine subject matter expertise with knowledge of practical soil uses, and provide numerous references for further study of the relevant literature
Author: Geological Survey (U.S.)
Publisher:
Published: 1988
Total Pages: 316
ISBN-13:
DOWNLOAD EBOOKAuthor:
Publisher:
Published: 1965
Total Pages: 1078
ISBN-13:
DOWNLOAD EBOOKAuthor: A. Kleber
Publisher: Elsevier Inc. Chapters
Published: 2013-02-26
Total Pages: 80
ISBN-13: 0128079428
DOWNLOAD EBOOKSlope deposits, which veil entire slopes or large parts of them in a rather uniform manner (cover beds), are ubiquitous in the subdued mountains of Central Europe (e.g., ). Here, we show that successions of cover beds are not restricted to this area but occur in many other regions of rather different natural inventories, such as the European Alps, the Russian Plain, south-central Turkey, and the western USA (Great Basin and Rocky Mountains). Cover beds usually form sequences of two or more distinct layers, and their distribution depends on the geomorphic, climate-driven processes of their formation. As they influence pedogenesis, they contribute to the understanding of soil properties and soil distribution: horizon boundaries occur at depths where cover-bed properties change. The properties of the layers and of the soils developed in them are different per region: in humid areas layers free of admixed loess components, thus being solely influenced by weathered local materials, are frequent, whereas in dry regions such layers have not yet been reported. In several areas studied in this chapter, paleosols either occur within cover-bed successions or have been reallocated and incorporated into the cover beds. This provides handles to the ages of layers. The layer successions slowly change with elevation but show a drastic break at around the timberline where Holocene rather than Pleistocene periglacial slope processes gained supremacy.