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Forests & Watersheds:Management & other Influences
Our daily water – 100+ gallons per person
Only about 5 percent of this
water is used for drinking
and food preparation
Commercial Bottled Water
Source: tap water from Clackamas River Utility
Most of Oregon’s major municipal water systems rely heavily on surface water supplies that originate on forest lands
Albany & Millersburg
water supply issue
Upper Pony Cr. Dam Project
Coos Bay-North Bend Water Board
Spillway raised 21 ft. for approx. 3x
storage increase (1.9 billion gallons)
P.W. Adams
Drift Creek Prime supply for area from
Lincoln City to Depoe Bay Prime habitat for wild salmon
The mind’s eye image: Clean, cool, abundant, easy-flowing water
from a pristine forest
OSU photo
An “ecosystem service”
But – both undisturbed and managed watershedshave important, and not always positive, influences
on water quality and quantity
P.W. Adams
Role of 10-15 year
climate cycles
Role of long-term
climate changes?
Fox Cr. (Bull Run)
Willamette NF (HJ
Umpqua NF (CC)
0 200 400 600 800
Pounds Per Acre
AVERAGE ANNUAL EROSION - UNDISTURBED FORESTSDissolved + Suspended + Bedload Sources
adapted from
Fredriksen & Harr 1979
P.W. Adams
Average Annual Erosion*
Undisturbed Forest Watersheds
*includes dissolved
+ suspended
+ bedload sedimentWillamette NF,Lane County
Umpqua NF, Douglas County
Bull Run, Clackamas CountyLocal Geology & Climate Matter!
> 500 ppm
No Roads, No Logging
Stream Suspended SedimentUndisturbed Coast Range (Lincoln County) Watershed
P.W. Adams
LANDSLIDES in MATURE FORESTS
Western Oregon
STUDY Slides per 1000 Acres
Swanson & others 1977 32
Ketcheson & Froehlich 1978 59
OR Dept. of Forestry 1997 18
Landslides happen!
P.W. Adams
Sediment Losses after Wildfire
(Helvey 1980)
1.875 tons per acre
Entiat Forest Washington
1971 + 1972
High Meadow Burn, 2000
Denver Municipal Watershed
Timbered Rock Burn
SW Oregon 2002
P.W. Adams
Biscuit Fire - Burn Severity
Low + Very Low +
Unburned
High + Moderate
www.biscuitfire.com/baer_photo.htm
BAER photo
Upper Chetco
Mod to high
severity burn:
71 sq miles
(24% of total)
Entire Biscuit
Mod to high
severity burn:
302 sq miles
Fire & Soil
Hydrophobicity
(water repellency)adapted from McNabb & others 1989
(light-mod. broadcast burn, SW Oregon)
burned*
unburned
*lowest rate observed
BAER photo (www.biscuitfire.com)
5 to 50% of soils tested in
the Biscuit Fire area had
moderate to strong water
repellency in the surface
mineral soilBiscuit Post-Fire Assessment (USDA For Ser, January 2003)
Wildfire Effects: Stream Nitrate Levels
adapted from 3
studies cited in
Tiedemann &
others, 1979
BAER photo (www.biscuitfire.com/baer_photo.htm)
BAER photo
biscuitfire.com
Stream
Length
Max Temp
Above
Max Temp
Below
6350 ft 58.3 F 70.0 F
Stream shading & maximum water temperature
following intense wildfire in headwater streams
in SW Oregon. Amaranthus et al., 1989.
Temperature increases were related
to post-fire shade levels.
Stream Shade Loss
Biscuit Fire:
• nearly 32,000 acres impacted
• up to 55% shade loss in 13 basins
• 6 basins had > 25% shade lossBiscuit Post-Fire Assessment
(USDA For Ser, Jan. 2003)
*Seaside Municipal Watershed
10 25 30 30 30 40 50 70
Water Color (Pt-Co units)
0
2
4
6
8
10
12
Dis
solv
ed O
xyge
n (p
pm)
WATER QUALITY IN ISOLATED POOL
South Fork Necanicum RiverSept. 9 to Nov. 4, 1981
Alder Leaf Fall & Low Streamflows
*
A natural influence (leaf fall) can impact water quality
adapted from Taylor & Adams 1986
Water Quality AnalysisUndisturbed, old-growth forest, W. OR
P.W. Adams
Ingredients:
purified water,
magnesium sulfate,
potassium chloride, salt
(sodium chloride)
Tasters can't tell difference between tap, bottled waterBy Susan Palmer, The Register-Guard, April 14, 2006
Funny thing about water. It tastes like ... water.
That was the consensus of 40 people who tried a
taste test pitting tap water against bottled water
Thursday at the University of Oregon. Thomas Brundage gets blindfolded before the taste test. KEVIN CLARK THE REGISTER-GUARD
Constituent Ave. concentration(mg/l or ppm)
Bicarbonate (HCO3) 3.7
Calcium (Ca) 2.8
Sodium (Na) 2.0
Magnesium (Mg) 0.8
Potassium (K) 0.3
Phosphate (PO4) 0.02
Ammonium (NH4) 0.003
Nitrate (NO3) 0.003
DEQ Temperature Standard (16o C) exceeded in
undisturbed forest watershed (Flynn Cr.)
Hale 2007
Paustian & Beschta 1979
What’s “natural” (good?)
water quality?
When & how many
samples needed to
determine this?
Brown 1985
Similar flows,
very different
sediment loads
Sediment loads in
this undisturbed
watershed varied
from 0 – 2000 ppm
What’s “good?” – What’s “normal?”Water quality varies by location, year, season, storm, etc.
Single storm
Several years
Falling
flows
Rising
flows
Total water loss due to forest cover, western Oregon:
About 18-20 inches, or about 20-50% of annual precip.
Annual
Interception
Losses:
6 - 15% of Total
Precipitation
The “cost” of relatively high quality water from forest lands: Water Loss
Annual Transpiration
Losses:
15 - 35% of Total
Precipitation
Planted forests and water in perspectiveForest Ecology and Management, Vol. 251 (2007): 1-9.
Afforestation is increasingly considered as a land use
activity that threatens water resources security. At the
same time, it is advocated for a wide range of other
water-related benefits… Current evidence suggests that
afforestation will typically reduce local average water
yield as well as low flows… …afforestation may increase
groundwater recharge and low flows due to improved
infiltration… Afforestation is not likely to reduce major
large-scale flooding or deep-seated landslides, but may
reduce shallow landslides and local ‘flash’ floods.
Journal of Soil and Water ConservationJuly-Aug. 1987: 274-276
Carbon sequestration programs… are gaining attention globally & will alter many ecosystem processes, including water yield... …results clearly demonstrate that reductions in runoff can be expected following afforestation of grasslands and shrublands and may be most severe in drier regions… The possibility that afforestation could cause or intensify water shortages in many locations is a tradeoff that should be explicitly addressed in carbon sequestration programs.
International concerns about effects of tree planting on water supplies
How can forest management practices
affect watersheds & water resources?
Insignificant
Neutral
Positive
Negative
Complex
Also important: Duration of Effects
"Simplicity cannot be willed upon the forest hydrologic system” - R.D. Harr, Forest Hydrologist, 1987
Needle Branch Watershed: Logged & Broadcast Burned 1966
Research that helped shape policy
OSU photo
Policy. (1) Forests make a vital contribution to Oregon by providing… social &
economic benefits, by helping to maintain… water resources & …habitat for…
aquatic life.
Therefore, it is...public policy of the State...to encourage economically
efficient forest practices that ensure the continuous growing & harvesting of
forest tree species… consistent with sound management of soil, air, water, fish
& wildlife resources… Oregon Revised Statutes 527.630
Oregon's
Forest Practices Act
The Forest Practices Act is used to meet water quality standards on
forest lands in Oregon. Under the Clean Water Act, forestry is a
nonpoint pollution source, thus allowing a “BMP” policy approach.
However, a recent (Aug. 2010) federal court ruling on a western
Oregon case said that forest roads did not fit this approach.
P.W. Adams
Policy that preceded research: Stream cleanup
Photos courtesy of Starker Forests
40 Years Later: Few or No Differences in Water Quality & Quantity
(Hale 2007)
P.W. Adams
National Forests & BLM Lands
Organic Act (1897)
“…for the purpose of securing favorable conditions
of water flows, & …a continuous supply of timber”
Federal Land Policy & Mgmt. Act (1976)
“…a combination of balanced & diverse resource
uses… including… timber, …watershed, … & fish”
“…in regions of heavy rainfall… [National] Forests… are created & maintained
to protect the timber &… to prevent the water from running off suddenly in
destructive floods.”
-Gifford Pinchot, The Use of the National Forests (1907)
O&C and Coos Bay Wagon Road Lands Act (1936)
“…providing a permanent source of timber supply,
protecting watersheds, regulating stream flow, &
…the economic stability of local communities”
A closer look at how management practices can affect water from forest lands
Timber Harvest
Forest Roads
Other
P.W. Adams
• Wide range of site conditions & harvest prescriptions
• Wide array of harvest systems, machines & operators
Expected Soil & Water Effects & Concerns:
Highly Operations- & Site-Specific!
Tires, tracks, suspensions, & reach Tree sizes, density & values
pressure & vibration
traction & control
pieces & efficiency
traffic patterns
slash
Photos, P.W. Adams
Pacific Coast RegionNeed to remove > 25% of forest cover within the entire watershedto detect a change in annual water yields (Stednick 1996)
Flow increases were proportional to the reductions in forest cover (b.a.) Largest flow increases occurred in late fall & winter
Coyote Creek Watershed - Douglas County (Harr & others 1979)
30% of watershed
Cut 50% basal area
Streamflow Patterns:
Rain vs. Snow
Water storage facilities may be critical in meeting peak
summer demands
Rothacher 1971
P.W. Adams
Soil Moisture in New* Clearcut & Adjacent Forest36-inch soil depth, SW Oregon – Hallin 1960
SO
IL M
OIS
TU
RE
(%
of
ove
nd
ry w
eig
ht)
Dry season: the clearcut had higher soil moistureWet season: the forest had higher soil moisture
*little plant cover & related soil water loss
Dry Season
Wet Season
Forest Revegetation & Soil Moisture – Oregon Cascades(Adams & others 1991)
•A strong, negative relationship between plant cover & soil moisture
(0-120 cm depth, linear regression statistical analysis)
•A burned clearcut had lower soil moisture than an adjacent mature
forest when its total plant cover exceeded about 35-40%
Less soil moisture than forest
More soil moisture
Rainfall reaching ground
under old-growth forest
after interception losses
Nov.-March, OR Cascades
(Rothacher 1963)
96%
8 to 16 inches
Soil water storage capacity
during wet weather
Upper 4 ft, 8 soil types, OR Cascades
(Rothacher et al. 1967)
Big Storms (over 8”)
Net result:Very high streamflows!
Water losses from forest & other
plant cover is greatest when:
• Evaporation is high • Soil moisture is high
Stream Temperatures - Coyote Cr. WatershedUmpqua National Forest (Adams & Stack 1989)
Patch Clearcut
Clearcut, No Buffer
Unlogged Control
Shelterwood Cut
Roads & Logging
1971-72
Shade recovery
Streamside shading matters,
but so do other local conditions
Duration of Effects
Patch Cut
Clearcut
• Revegetation
• Stabilization
• Shade
Road-related
landslide
Careful analysis is needed to help identify cost-effective solutions to watershed problems
sedimentsource?
Agricultural & urban/suburban areas are now major
sediment sources in important watersheds.
Some key findings:
During the 1996 flood,
natural erosion,
unique clays & non-
forest activities were
the primary cause of
turbidity problems in
Salem's water supply.
High-tech, geologic “fingerprinting” now helps identify sediment sources
Oregon water quality status based on Water Quality Index,by land use, Water Years 1990-1999 (Cude, undated)
New watershed studies
now underway are
evaluating the effects
of contemporary forest
practices on water
quality, quantity &
aquatic resources:
Photos & graphics courtesy of A.E. Skaugset
Hinkle Creek Paired Watershed Study, Douglas County
Initial entries, Aug. 05-Apr. 06• 5.5 mi new & reconstructed
roads, 17,325 yd3 rock • 12.2 MMbf harvested from
380 ac., 3,281 loads of logs
Max. Daily Stream Temperature
Hinkle Creek Paired Watershed Study, Douglas County
Slide courtesyof A.E. Skaugset
Streamflow Sediment Yield
Hinkle Creek Paired Watershed Study, Douglas County
Slide courtesyof A.E. Skaugset
Some local effects observed, primarily in first post-treatment wet season
Growth (mm/mm/day) for PIT Tagged CutthroatNorth & South Fork Hinkle 2002-07
0 1 2 3 4 5
Rela
tive
gro
wth
(m
m/m
m/d
)
0.0000
0.0005
0.0010
0.0015
0.0020
NF NF
SF SFn=64
n=102n=140 n=140
Mean -------
Median
Pre-
treatment
Post-
treatmen
Post-
treatmen
Pre-
treatment
Hinkle Creek Paired Watershed Study, Douglas County
Slide courtesyof A.E. Skaugset
Also, no apparent effectsof upstream logging on:• benthic invertebrates• amphibians
ODF RipStream Temperature Study(Summary presented at 9/8/10 Board of Forestry meeting)
Q1) Do forest streams meet the DEQ temperature standards after harvest?
Q2) What site characteristics are closely related to temperature changes?
A1) Some higher temps., but no strong
indication DEQ standards were exceeded
A2) Max. temps. are closely related to
post-harvest shade; length & gradient of
treatment area also are important
33 sites (18 pvt., 15 State), W. OR
Med. & Small Type F Streams
You can find an individual study
to support almost any opinion or
management preference
Seek relevant expertise for accurate interpretation
Look at wide range of both research & experience
Interpret for local conditions & current practices
Carefully evaluate facts & values in issues & info
To protect the watershed…
Management practices that maintain or help restore favorable soil conditions (especially high infiltration) are most important for good water quality & flow
...protect the soil
Beyond Regulation: Evolving PracticesOld timber, tractors, & disturbance
vs. New harvests, layouts, machines, etc.
OSU photoOSU photo
Some unique watershed concernswith fuel reduction treatments:
Soil compaction/disturbance (if more machine traffic)
Soil exposure (if high removal)
Truck traffic (if high utilization)
P.W. Adams
Potential for runoff & erosion from increases in:
Harvest System & Machine Selection
Compaction &
Disturbance
Tractors & Skidders
- / + Variable performance & use
Harvester/Processor & Forwarder
+ Log swinging reduces traffic
+ Slash can be added to trails
Feller Buncher & Grapple Skidder
- Traffic to each tree & stem
Rubber-tire skidder 10-30%
Crawler tractor 20-40%
Feller-buncher 25-50%
Harvester 35-50%
Forwarder 10-30%
Slope Limits*
*Approx. slope ranges due to differences in
design, payload, local soil conditions, etc.
P.W. Adams
Practices During Operations:
Awareness
Knowledge
Experience
Ability
Skill
Operator Selection & Supervision
Beyond Regulation: Evolving Practices II• Road design & location
• Drainage & stream crossings
P.W. Adams
OSU photoP.W. Adams
OSU photo
Legal Requirements for Forest Roads:Oregon’s Forest Practices Act & Rules
•Keep roads away from streams & other water*
•Provide for good surface drainage
•Prevent stream sedimentation & turbidity
•Provide for fish passage at crossing structures*
•Design structures to pass 50-year storm flow*
•Prevent road-related landslides
•Maintain all roads; stabilize closed roads
*primarily apply to new construction or major upgrades/repairs
(1) The purpose… is to reduce delivery of
fine sediment to streams caused by
the use of forest roads during wet
periods that may adversely affect
downstream water quality in Type F or
Type D streams.
(2) Operators shall use durable
surfacing or other effective
measures that resist deep rutting or
development of a layer of mud on top
of the road surface on road
segments that drain directly to
streams on active roads… used for
log hauling during wet periods.
(3) Operators shall cease active road
use where the surface is deeply
rutted or covered by a layer of mud
& where runoff from that road
segment is causing a visible
increase in the turbidity of Type F
or Type D streams as measured
above & below the effects of the road.
Wet Weather Road Use(ORS 629-625-0700)
P.W. Adams
Oregon Forest Practice Rules
Stream Crossing Structures(OAR 629-625-0320)
Minimize excavation of side slopes near the channel
Minimize volume of...the fill
Fills over 15 ft [require]... a written plan
Prevent erosion of...fill & channel
Pass a peak flow...50-yr return...adequate to [avoid] ponding
Allow migration of adult & juvenile fish upstream & downstream”
"Operators shall design & construct… structures to:
• Peak flows
• Stream power
• Culvert sizing
• Potential to clog
• Potential for scour
Erosion Potential at
Stream Crossings
Flow Capacity Circular Culverts
Diameter (in) Capacity (cfs) 24 5 - 11
36 21 - 31
48 47 - 64
60 88 - 113
72 145 - 178
Example: 75 cfs/mi2 x 4.9 miles = 368 cfs
Oregon's Forest Practice Rules
Required RMA widths: 20 - 100 feet
USDA Forest Service
State & Private Forestry Publication NA-TP-06-98
Slope of Land Between Road
and Stream (percent)
Recommended Buffer Width,
slope distance (feet)
0 - 10 50
11 - 20 51 - 70
21 - 40 71 - 110
41 - 70 111 - 150
Buffers for Roads
Consider wider buffers for erodible soils & slopes
82% of the surveyed segments with actual
or possible sediment delivery to streams
were over 150 feet in length
Sediment production was related to the
length & slope of road segments
Sediment Production from Forest Roads in Western ORLuce & Black 1999
Road Sediment & Drainage Monitoring
in Western OR - Skaugset & Allen 1998
AvoidLong,
SlopedSegments!
Road Inventory & AssessmentRMP Road Inventory Data Form OSU Ver. 11/15/02
Road
CondCondType
Stream
Crossings
Type
Ditch Relief Culverts
Road
Width CondSizeCondTypeCond% Notes
Ditch
Cond
Surface
Drainage
Corner
Condition
Clearing
Height
Clearing
Width
Grade
Surface
Material
Surface
Shape
Loc-
ationStation
Landowner: ___________________________________________________________________________________ Date:___________________
Road Name: _________________________________________________________________________________ Season/Type of Use: ___________________________
Page: ____ of ____
Luce & Black 1999
Sediment Production from Forest Roads in Western OregonLuce & Black 1999
Local soils & geology matter:
Sediment from rocked roads was about 9
times higher where constructed on silty clay
loam than on gravelly loam soils
Maintenance can be “overdone:”
Road segments where vegetation was
cleared from the cutslope & ditch produced
about 7 times more sediment than where
vegetation was retained
Watershed restoration projects vary widely
For information & assistance about riparian & stream habitat enhancement projects, contact your local Watershed Council or the Oregon Watershed Enhancement Board (OWEB)
http://www.oweb.state.or.us/
Oregon Watershed Enhancement Board
Both printed & web-based info. & assistance available