ic.ucsc.edu Sytsma 2005 Attiwill et al. 1993.

Slides:



Advertisements
Similar presentations
Soil Erosion.
Advertisements

SOIL DEGRADATION WITHIN THE SOILCRITZONE CONCEPT by Winfried E.H. Blum and Svetla Rousseva.
Properties of Water.
Phosphorus Indices: an Understanding of Upper Mississippi Strategies John A. Lory, Ph.D. Division of Plant Sciences University of Missouri.
Phosphorus Index Based Management Douglas Beegle Dept. of Crop and Soil Sciences Penn State University
Togus Pond Development Surveys Lauren Wolpin. Development Overview Shoreland Zoning Regulations Wastewater Disposal Development Survey Buffer Strip Survey.
Agricultural Phosphorus and Eutrophication by Don Pitts Agricultural Engineer & Water Quality Specialist USDA, NRCS Champaign, IL.
Timber Harvest Planning Course Learning Objective: Be able to describe the harvest planning process including different levels (or types) of harvest plans,
David O. Wallin Department of Environmental Sciences Huxley College of the Environment Western Washington University Bellingham, WA
Erosion The transport of earth materials from one place to another.
Section 3: Stream Deposition
Surface Water Topics: Surface Water Movement Stream Development
Watershed Update, Kahler, ECF, 6/26/2014. The Kahler Challenge.
BEST Plots Small and Large Scale Measurements. We rely on Earth’s surface to supply most of what we need to live. Therefore, mapping and monitoring this.
Hydrology River Ecosystems and Humans. Dimensions of river ecosystems Longitudinal Lateral Vertical Temporal 2.
Forest Hydrology Issue: Interaction of forests, fish, and climate One of the dominant pathways by which land cover change affects freshwater fish habitat.
S. Fork Nooksack River, WA. Reasons for Land Clearing Agriculture Lumber Mining Urban Development.
Landslide Disturbance 1 – Landslides, also called debris flows, can rapidly change the landscape of riparian zones. 2 – The sudden movement of debris and.
Abstract Upland areas of the Willamette Basin are associated with a long history of logging and related road construction. Sediment derived from forested.
Using the Missouri P index John A. Lory, Ph.D. Division of Plant Sciences Commercial Agriculture Program University of Missouri.
Maintaining Watersheds. Next Generation Science/Common Core Standards addressed! HS‐ESS2‐5. Plan and conduct an investigation of the properties of water.
Some Major Problems In Managing Watersheds Of The Border Region Dr. M. Karl Wood, Director Water Resources Research Institute New Mexico State University.
The Effects of Nitrogen Fertilization on Nutrient Cycling and Forest Productivity By: Eric Sucre.
By Oliver Pickford. The number of trees that are being chopped down every year is around 3 billion up to 6 billion! Once the trees have been chopped down.
1 Erosion and Sedimentation Processes, Factors and Impacts on the Environment Issued May 2009 Level IA: Fundamentals Seminar Education and Training Certification.
Center for Watershed Protection USDA Forest Service, Northeastern Area, State and Private Forestry How to estimate future forest cover in a watershed.
Sanitary Engineering Lecture 11. Storm Water Runoff Storm water runoff is the precipitation which seeps into the ground if precipitation occurs faster.
Efficient/ non efficient use of ecosystem resources: first results from ecosystem capital accounts Jean-Louis Weber & Emil Ivanov.
Stream Processes and Habitat Ryan Johnson. Overview Watershed Processes – Factors and their effects on the watershed as a whole Stream Processes – Factors.
Nutrient Criteria for the plains regions of Missouri.
Forest Ecology Soil.  Time to Get Dirty Soils  For this presentation we are going to be ‘borrowing’ some information from the Oregon Envirothon.
Key Questions for Understanding Surface Water Section 9.1.
How do humans affect watersheds and the hydrologic cycle ?
2 pt 3 pt 4 pt 5pt 1 pt 2 pt 3 pt 4 pt 5 pt 1 pt 2pt 3 pt 4pt 5 pt 1pt 2pt 3 pt 4 pt 5 pt 1 pt 2 pt 3 pt 4pt 5 pt 1pt Water Cycle Free ResponseStream TablesRiver.
VFR Research - R. Hudson Basic Hydrology Streamflow: Hydrographs; Case studies of logging effects on streamflow; Peak flow.
Natural vs. Accelerated Soil Erosion Natural geologic erosion has occurred at a relatively slow rate since the earth was formed. Natural erosion produces.
The Flow of Fresh Water Chapter 11.
Erosion and Mass Movements RRB page Erosion Erosion: The carrying of sediment by wind, water, ice and other agents Erosion: The carrying of sediment.
A stream is a body of water that carries rock particles and dissolved ions and flows down slope along a clearly defined path, called a channel. Thus, streams.
How do humans affect watersheds and the hydrologic cycle ?
Weathering a mechanical or chemical surface process that break rock into smaller and smaller pieces Erosion the transportation of materials or sediment.
Section 3: Stream Deposition
Journal #5 What is a flood? Why are floods harmful? What can humans do to prevent floods?
11.1 The Active River. Do you think a river can have a source? Describe where you would expect to find a river’s source. The source of a river is where.
 Deforestation and defacing of landscape – Top soil as well as the vegetation is removed to get access to the deposit.  Soil erosion – also prone to.
EROSION CONTROL BY LAND MANAGMENT WHAT IS EROSION The detachment and transportation of soil particles from one place to other by running water, wind.
Precision Management beyond Fertilizer Application Hailin Zhang.
1 UIUC ATMOS 397G Biogeochemical Cycles and Global Change Lecture 18: Nitrogen Cycle Don Wuebbles Department of Atmospheric Sciences University of Illinois,
The Work of Streams Erosion – water causes loose particles to be moved through abrasion, grinding, or by dissolving soluble material. Sediment Transport.
SOIL LAB: Land Resources and Management. US land area: 9,161,966 km 2 3,537, square miles US arable land: 1,650,070 km 2 637,095,589 square miles.
Chapter 9 Review game Chapter review Packet.
11.1 The Active River.
HYDROSPHERE Surface Water.
Warm-up Turn in old warm-up sheet to the bin
Predicting the hydrologic and water quality implications of climate and land use change in forested catchments Dennis P. Lettenmaier Department of Civil.
Section 1: Surface Water Movement
Water Cycle It keeps cycling back
The Phosphorus Cycle.
Strategies to Reduce P Loading and Sedimentation on Forestry Operations in Vermont First few slides will provide some background information on what we.
Stream Erosion.
The Swedish National Forest Inventory
1ST YEAR OF ESO RIVERS PROFESOR TIERNO GALVÁN SECONDARY SCHOOL.
The Phosphorus Cycle Which Earth Systems Does Phosphorus Cycle Through?? How is This Different From the Cycling of Carbon??
Water Cycle It keeps cycling back
Human Activities on Mountainsides
The Phosphorus Cycle Which Earth Systems Does Phosphorus Cycle Through?? How is This Different From the Cycling of Carbon??
STREAMS AND THE EARTH Water Erosion
Freshwater.
4.5 Changes in Ecosystems pgs
Presentation transcript:

ic.ucsc.edu

Sytsma 2005

Attiwill et al. 1993

Janse et al. 1997

How does phosphate that stored in forest vegetation and soils move into lakes? Leaching and transport of soluble orthophosphate through ground or surface waters Transport of soil particles by erosion Transport of organic material (*)

Sytsma 2005

“For the 10 to 30 year old forests, three out of four study areas had lower landslide densities than found in mature forest, and two of four had reduced erosion volume. For the 31 to 100 year old forests, three out of four study areas had both lower landslides and erosion volume as compared to mature forests. Therefore, for the most erosion prone landscapes, these results also indicate that 10 to 30 year old forests have a 75 percent chance of having a lower landslide density than mature forests. In a similar light, 31 to 100 year old forests have a 75 percent chance of having both lower landslide density and erosion (sediment delivery to channels) as compared with mature forests.” ODF, 1996

Understory Vegetation Tree Foliage Forest Floor Uptake and Return Cole & Rapp, 1981

Sytsma 2005

USDA Forest Service

ODF 1996

“For the 10 to 30 year old forests, three out of four study areas had lower landslide densities than found in mature forest, and two of four had reduced erosion volume. For the 31 to 100 year old forests, three out of four study areas had both lower landslides and erosion volume as compared to mature forests. Therefore, for the most erosion prone landscapes, these results also indicate that 10 to 30 year old forests have a 75 percent chance of having a lower landslide density than mature forests. In a similar light, 31 to 100 year old forests have a 75 percent chance of having both lower landslide density and erosion (sediment delivery to channels) as compared with mature forests.” ODF, 1996

Google Maps

Possible Research Opportunities Road density vs. phosphorus loading Road densities can be obtained from aerial photographs. It may also be possible to determine when road systems were built by looking at old aerial photographs. Recently harvested or permanently cleared land area vs. phosphorus loading ODF maintains data for all harvest operations in Oregon. It may be possible to monitor a lake long-term to see if phosphorus loading changes as harvest activity increases or decreases in the watershed.