Forest Road Hydrology
Forest Road Hydrology

Author: Elizabeth Myers Toman

Publisher:

Published: 2004

Total Pages: 156

ISBN-13:

DOWNLOAD EBOOK

The management of existing forest road systems is an issue of growing importance and public debate. Roads can alter the hydrologic processes in a watershed especially at stream crossing culverts where road ditches channel runoff directly into the stream. The objective of this study was to determine how surface runoff from roads augments natural stream flow at stream crossing culverts. This study took place within an 824 ha watershed in the foothills of the Oregon Coast Range approximately three miles west of Corvallis, Oregon. Sixteen stream crossing culverts were selected for study. Discharge was measured from October 2002 through May 2003 at each stream and at the adjoining ditch(es). Hydrographs for both stream flow and ditch flow were analyzed for five storms that occurred during the winter 2002-2003. The interaction of the road with subsurface flow from the hillslope caused the hydrology of the road segment to be classified as either "intermittent" or "ephemeral." Peak flow and total runoff at the stream crossing culverts was compared with the magnitude and timing of peak flow and total runoff in the adjoining ditch(es). Forest roads were found to alter the flow paths of water through the Oak Creek watershed. The road altered storm runoff and peak flow at the stream crossing culverts seventy-four times out of seventy-eight opportunities during five storms. The amount of the change depended primarily on whether or not the road cutslope intercepted subsurface flow. Contributions of intercepted subsurface runoff to the stream were greater than contributions of surface runoff by an order of magnitude. In the Oak Creek watershed, 56 percent of the road cutslopes adjacent to streams intercepted subsurface flow. Intercepted subsurface flow was more connected in time to stream flow than surface runoff. Ditch flow, on average, contributed the most volume on the rising limb of the stream hydrograph at the culvert. Flow responses at individual culvert locations were highly variable and could not be predicted using traditional topographic variables.

Forest Hydrology and Ecology at Coweeta
Forest Hydrology and Ecology at Coweeta

Author: Wayne T. Swank

Publisher: Springer Science & Business Media

Published: 2012-12-06

Total Pages: 463

ISBN-13: 1461237327

DOWNLOAD EBOOK

Coweeta is one of the oldest continuously operating laboratories of its type in the world. For the first time, a complete review and summary of more than 50 years study of the hydrological and ecological responses of baseline and managed Southern Appalachian hardwood forests at Coweeta is now supplied by this volume. The long-term research approach represents a continuum of theory, experimentation and application using watersheds as landscape units of investigation. Thus, the information encompasses a wide range of interpretations and interests. In addition to in-depth analyses of terrestrial and stream processes, the breadth of coverage includes historical perspectives and relevance of ecosystem science to management needs. In a broader sense, the Coweeta research effort is considered from a perspective of national and international forest hydrology and ecology programs.

Forest Hydrology
Forest Hydrology

Author: Mingteh Chang

Publisher: CRC Press

Published: 2006-05-25

Total Pages: 500

ISBN-13: 9780849353321

DOWNLOAD EBOOK

Although a few texts on forest hydrology are available, they cover very little, if any, background on water resources. On the other hand, books dealing with water resources do not cover topics on forest-water relations. The one exception to this is Forest Hydrology: An Introduction to Water and Forests. Now with the publication of a revised edition, this volume adds information from recent studies to go even further in providing an introduction to forest hydrology that brings water resources and forest-water relations into a single practical and comprehensive volume Focusing on processes and general principles, the first six chapters provide an introduction and basic background in water and water resources, while the last seven chapters look at the impact of forests on water. Between these two groupings is a chapter that serves as an entry to the study of forest impacts on water resources, describing forests and forest characteristics important to water circulation, sediment movement, and stream habitat. This second edition also features new information on forests and flooding, forest and stream habitat, snow vaporization processes, and GIS methods in hydrology research, examples on evaporation estimates, and a new appendix on forest interception measurements. Employing examples and case studies, the book provides tools to help natural resource managers play an active role in policymaking and land-use planning, and in developing partnerships with stakeholders. It also offers unique perspectives for addressing urban sprawl.

Forest Hydrology
Forest Hydrology

Author: Devendra Amatya

Publisher: CABI

Published: 2016-09-14

Total Pages: 309

ISBN-13: 1780646607

DOWNLOAD EBOOK

Forests cover approximately 26% of the world's land surface area and represent a distinct biotic community. They interact with water and soil in a variety of ways, providing canopy surfaces which trap precipitation and allow evaporation back into the atmosphere, thus regulating how much water reaches the forest floor as through fall, as well as pull water from the soil for transpiration. The discipline "forest hydrology" has been developed throughout the 20th century. During that time human intervention in natural landscapes has increased, and land use and management practices have intensified. The book will be useful for graduate students, professionals, land managers, practitioners, and researchers with a good understanding of the basic principles of hydrology and hydrologic processes.

Uncertainty in Forest Road Hydrologic Modeling and Catchment Scale Assessment of Forest Road Sediment Yield
Uncertainty in Forest Road Hydrologic Modeling and Catchment Scale Assessment of Forest Road Sediment Yield

Author: Christopher G. Surfleet

Publisher:

Published: 2009

Total Pages: 502

ISBN-13:

DOWNLOAD EBOOK

The goal of this study was to advance methods for assessment of forest road hydrologic response and sediment yield at a catchment scale. This research looked at the effect of soil depth estimation on the Distributive Hydrology Soil Vegetation Model (DHSVM), assessed the uncertainty and accuracy of hydrologic modeling of forest roads by DHSVM, and evaluated the use of road runoff and sediment sampling for catchment scale road sediment estimates. The influence of soil depth estimation on DHSVM varied by spatial scale and hydrologic process modeled. Soil depth measurement improved DHSVM simulated streamflow and road ditchflow for the rising limb of the hydrograph with no improvements during baseflow. For site specific or small scale modeling a deterministic soil depth model fit to field measurements was best. For larger scale simulations of streamflow mean soil depth provided as good or better estimates. Considerable uncertainty in estimates of road hydrologic response was observed from DHSVM. DHSVM over predicted individual road discharges. As the spatial scale and temporal scale was increased the uncertainty in DHSVM results decreased. This suggests that model structures chosen for DHSVM would be better determined with internal catchment data, at smaller scales. The GLUE assessment showed that change detection analysis with DHSVM will be limited to sites or scales of the catchment that behavioral model structures can be identified. From this research it was determined that only the catchment scale simulations and a few individual road locations could be used for change detection. The storm runoff volumes and peak flows from road ditchflow had linear relationships with storm sediment load. These relationships had to be developed by classes of road locations and types in an intensively managed forest due to variability in road design, hydrologic response, and road use. Sediment from roads estimated from field measurements used with SEDMODL2 or WARSEM provided substantially lower estimates than without field measured adjustments. The use of road runoff for sediment estimation provided even lower catchment scale sediment results. DHSVM simulated road runoff for sediment estimation provided catchment scale results similar to the sediment yield estimated from observed road runoff.

Forest Hydrology
Forest Hydrology

Author: Mingteh Chang

Publisher: CRC Press

Published: 2012-11-01

Total Pages: 587

ISBN-13: 1466586672

DOWNLOAD EBOOK

Due to its height, density, and thickness of crown canopy; fluffy forest floor; large root system; and horizontal distribution; forest is the most distinguished type of vegetation on the earth. In the U.S., forests occupy about 30 percent of the total territory. Yet this 30 percent of land area produces about 60 percent of total surface runoff, the

Hydrology of Small Forest Streams in Western Oregon
Hydrology of Small Forest Streams in Western Oregon

Author: Robert Dennis Harr

Publisher:

Published: 1976

Total Pages: 20

ISBN-13:

DOWNLOAD EBOOK

The hydrology of small forest streams in western Oregon varies by time and space in terms of both streamflow and channel hydraulics. Overland flow rarely occurs on undisturbed soils. Instead, water is transmitted rapidly through soils to stream channels by displacement of stored soil water. Drainage networks expand and contract according to the interaction between precipitation characteristics and soil's capability to store and transmit water. Drainage networks are more extensive in winter than in summer. Streamflow may he 1,000 to 5,000 times greater during winter storms than during summer low flow. A stream's kinetic energy varies along with streamflow. Channel width and depth, heterogeneity of bed materials, and the accumulation of large, organic debris affects the dissipation of kinetic energy. Clearcutting can increase relatively small peak flows, but forest roads and extensive areas of soil compacted by other means may increase larger peak flows. Both roadbuilding and clearcutting can cause soil mass movements, which can drastically alter a stream's channel hydraulics by adding debris or scouring the charnel to bedrock. Removal of naturally occurring organic debris that has become part of a stable channel can accelerate bed and bank erosion.

Land Use and Watersheds
Land Use and Watersheds

Author: Mark S. Wigmosta

Publisher: American Geophysical Union

Published: 2001-01-09

Total Pages: 246

ISBN-13:

DOWNLOAD EBOOK

Presents recent data on how forest management activities and urbanization have influenced the hydrologic and geomorphic responses of watersheds. Focusing on the Pacific Northwest, the 12 contributions discuss wetland processes, channel disturbance, changes in hydrology, and susceptibility to landslides in cities, and consider the effects of timber harvesting and road construction on stream flow, sediment yield, and erosion. Field studies of paired experimental/manipulated watersheds, plot studies, and spatially distributed models are provided. No index. c. Book News Inc.

Principles of Forest Hydrology
Principles of Forest Hydrology

Author: John D. Hewlett

Publisher: University of Georgia Press

Published: 1982

Total Pages: 193

ISBN-13: 0820323802

DOWNLOAD EBOOK

Students and professors of hydrology, ecology, land-use management, forest and range management, soil science, physical geography, soil and water conservation, and watershed management will welcome this revision of the 1969 edition of An Outline of Forest Hydrology by John D. Hewlett and Wade L. Nutter. The student pursuing a career in forest and wildland resources soon learns that no science is more fundamental to the art of land management than hydrology, but hydrology as a science traditionally has been subordinated to hydrology as technique. Older texts have focused on methods and applications to the exclusion of principle, occasionally leaving the hydrological effects of land use and vegetation to be interpreted from techniques rather than from knowledge of process. Soil, atmospheric, and vegetal phases of the hydrologic cycle of have neglected in many texts intended for the college student. Hewlett’s new book focuses on natural processes and is intended to guide further study and to serve as a base for class lectures. The subject matter is organized to introduce key ideas and principles and to provide consistent terminology and clear graphic material to aid the student in comprehending the complex literature of hydrology.