The soils of Oregon / Thor Thorson, Chad McGrath, Dean Moberg, Matthew Fillmore, Steven Campbell, Duane Lammers, James G. Bockheim.
2022
S599.O7 T56 2022
Linked e-resources
Linked Resource
Concurrent users
Unlimited
Authorized users
Authorized users
Document Delivery Supplied
Can lend chapters, not whole ebooks
Details
Title
The soils of Oregon / Thor Thorson, Chad McGrath, Dean Moberg, Matthew Fillmore, Steven Campbell, Duane Lammers, James G. Bockheim.
Author
ISBN
3030900916 (electronic bk.)
9783030900915 (electronic bk.)
9783030900908
3030900908
9783030900915 (electronic bk.)
9783030900908
3030900908
Published
Cham, Switzerland : Springer, [2022]
Copyright
©2022
Language
English
Description
1 online resource (xix, 545 pages) : illustrations (chiefly color), maps (chiefly color).
Item Number
10.1007/978-3-030-90091-5 doi
Call Number
S599.O7 T56 2022
Dewey Decimal Classification
631.4/7795
Summary
This book is the only comprehensive summary of natural resources of Oregon and adds to World Soil Book Series state-level collection. Due to broad latitudinal and elevation differences, Oregon has an exceptionally diverse climate, which exerts a major influence on soil formation. The mean annual temperature in Oregon ranges from 0C in the Wallowa and Blue Mountains of northeastern Oregon to 13C in south-central Oregon. The mean annual precipitation ranges from 175 mm in southeastern Oregon to over 5,000 mm at higher elevations in the Coast Range. The dominant vegetation type in Oregon is temperate shrublands, followed by forests dominated by lodgepole pine, Douglas-fir, and mixed conifers, grasslands, subalpine forests, maritime Sitka spruce-western hemlock forests, and ponderosa pine-dominated forests. Oregon is divided into 17 Major Land Resource Areas, the largest of which include the Malheur High Plateau, the Cascade Mountains, the Blue Mountain Foothills, and Blue Mountains. The single most important geologic event in Oregon was the deposition of Mazama ash 7,700 years by the explosion of Mt. Mazama. Oregon has soil series representative of 10 orders, 40 suborders, 114 great groups, 389 subgroups, over 1,000 families, and over 1,700 soil series. Mollisols are the dominant order in Oregon, followed by Aridisols, Inceptisols, Andisols, Ultisols, and Alfisols. Soils in Oregon are used primarily for forest products, livestock grazing, agricultural crops, and wildlife management. Key land use issues in Oregon are climate change; wetland loss; flooding; landslides; volcanoes, earthquakes, and tsunamis; coastal erosion; and wildfires.
Bibliography, etc. Note
Includes bibliographical references and index.
Access Note
Access limited to authorized users.
Source of Description
Desciption based on online resource; title from PDF title page (viewed July 11, 2022).
Added Author
Series
World soils book series.
Available in Other Form
Print version: 9783030900908
Linked Resources
Record Appears in
Table of Contents
Introduction
History of soil studies in Oregon
Soil-forming factors
Elevation gradients in Oregon mountain ranges
General soil regions of Oregon
Diagnostic horizons and taxonomic structure of Oregon soils
Taxonomic soil regions of Oregon
Mollisols
Inceptisols
Aridisols
Andisols
Ultisols
Alfisols
Entisols, vertisols, spodosols, and histosols
Soil-forming processes in Oregon
Benchmark, endemic, rare, and endangered soils in Oregon
Land use in Oregon
Yields, soil conservation, and production systems
Summary.
History of soil studies in Oregon
Soil-forming factors
Elevation gradients in Oregon mountain ranges
General soil regions of Oregon
Diagnostic horizons and taxonomic structure of Oregon soils
Taxonomic soil regions of Oregon
Mollisols
Inceptisols
Aridisols
Andisols
Ultisols
Alfisols
Entisols, vertisols, spodosols, and histosols
Soil-forming processes in Oregon
Benchmark, endemic, rare, and endangered soils in Oregon
Land use in Oregon
Yields, soil conservation, and production systems
Summary.