Unit 10 Fuel Moisture.

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Presentation transcript:

Unit 10 Fuel Moisture

Unit 10 Objectives Define critical live fuel moisture and the thresholds for various fuel types. Identify three methods for obtaining live fuel moisture. Describe the relationships between relative humidity, wind, and moisture content of fine and large fuels.

Unit 10 Objectives Explain how the amount and duration of precipitation and soil moisture affect moisture content of fine and large fuels. Define the fuel moisture timelag concept and its value to firefighters and fire managers. Describe how fuel moisture is determined for dead fuels in each of the four timelag categories.

Unit 10 Objectives Define moisture of extinction, how it varies in natural fuel complexes, and how it affects wildland fire ignition and spread. Determine fuel moisture content for fine dead 1-hour timelag fuels from fuel moisture tables during daylight conditions.

When fuel moisture is high, fires ignite and burn poorly; when it is low, fires start easily, and spread and burn rapidly. Fuel moisture will fluctuate with changes in weather, seasons, and topography. 10-5-S290-EP

Fuel Moisture Fuel moisture content is the amount of water in a fuel expressed as a percent of the oven dry weight of that fuel. Wet Weight - Dry Weight Dry Weight

Types of Fuel Moisture LIVE fuel moisture: DEAD fuel moisture: Found in living plants Ranges from 30% to 300% Varies over space, species and seasons DEAD fuel moisture: Found in dead plants, forest litter, slash, etc. Ranges from 2% to 30% Can change quickly over time and space

Fuel Moisture Affects Combustion Before a fuel can burn, the moisture in it must be converted to vapor through the heat process. The greater the moisture content, the higher the heat temperatures required to dry the fuel. The presence of moist fuel can affect the rate and direction that a wildland fire spreads.

Fuel moisture is one of the seven wildland environmental factors which must be continuously monitored for safety reasons.

Critical Live Fuel Moisture and the Thresholds for Various Fuel Types

Different physiological properties Different chemical contents Herbaceous Annuals Perennials Live Fuels Coniferous Woody Deciduous

Variations in Live Fuels Change seasonally Differences based on species and fuel model Vary in relation to aspect, elevation Big picture influences: Drought, frost kill, insects, diseases

Annual Trend of Jack Pine Foliar Moisture 300 280 260 240 220 200 180 160 140 120 100 80 Moisture Content (percent) New Foliage Old Foliage March Oct Month of Year

10-14-S290-EP

Moisture Content of Cheatgrass 250 Coloration 200 150 green Moisture content (percent) 100 purple 50 30 straw Spring Summer 10-15-S290-EP

Fuel Models with Live Fuels Herbaceous FM 2 Timber with grass understory Woody FM 4 Chaparral 6 ft. FM 5 Brush 2 ft. FM 7 Southern rough FM 10 Timber with litter understory

Fuel Model 2 10-17-S290-EP

Fuel Model 4 10-18-S290-EP

Fuel Model 5 10-19-S290-EP

Fuel Model 7 10-20-S290-EP

Fuel Model 10

Rate of Spread Based on Live Fuel Moisture

Crown Fires Crown fires are live-fuels fires. Can include large trees, but also the canopies of shrubs (oak brush and manzanita). Need sufficiently low live fuel moisture to be a significant component to fire behavior. Need adequate dead fuels to initiate a crown fire.

Critical Live Fuel Moisture The moisture content at which sustained, fast spreading, high intensity wildfires occur. Gambel Oak 130% Sagebrush 100% Conifers 100% Manzanita 80% Chamise 60%

Three Methods for Obtaining Live Fuel Moisture

Live Fuel Moisture Content Stage of Vegetative Development Moisture Content (Fireline Handbook, Appendix B) Fresh foliage, annuals developing, early in growing cycle. Leaf-out, bud-break, early June. 300% Maturing foliage, still developing with full turgor Late June. 200% Mature foliage, new growth complete and comparable to older perennial foliage. July to early August. 100% Entering dormancy, coloration starting, some leaves may have dropped from stem. Mid-August - September. 50% <30% Completely cured. Treat as dead fuel.

Live Fuel Sampling Collect relative sample from your area of concern. Be sure to sample the fresh new growth of the year as well as the perennial older growth. Once collected, weigh it, dry it, weigh it again. Use formula.

On-line Data Sources

Relationships Between Relative Humidity, Wind, and Moisture Content of Fine and Large Fuels

Moisture Balance Water moves from higher concentrations to lower concentrations

Moisture Exchange in Wildland Fuels Humidity Evaporation Dew Precipitation Evaporation Ground moisture 10-31-S290-EP

Equilibrium Moisture Content Occurs when there is no net loss or gain of moisture between fuels and the surrounding air. Moisture content attained when subjected to a constant temperature and humidity condition for an indefinite length of time.

Environmental Factors Influencing Fuel Moisture ELEVATION REALTIVE HUMIDITY FUEL MOISTURE PRECIPITATION WIND INDIRECT INFLUENCES DIRECT INFLUENCES TEMPERATURE SHADED UNSHADED SOLAR RADIATION SLOPE ASPECT CANOPY CLOUDS NIGHT 10-33-S290-EP

Shaded vs. Unshaded Effects on Fuel Moisture Air Temperature 85o 85o Fuel Moisture 8% 110o 3% 160o Surface Temperature 10-34-S290-EP

Aspect Affects Fuel Moisture 15 10 5 East slope North slope South slope Moisture content (percent) West slope 0 0600 1200 1800 Time of day

Elevation Affects Fuel Moisture (Daytime) Temperature RH Fuel Moisture 69° 73° 76° 80° 83° 87° 39% 35% 31% 27% 25% 22% 8% 7% 6% 5% 4% 6000 feet 5000 feet 4000 feet 3000 feet 2000 feet 1000 feet 10-36-S290-EP

Slope Percent Affects Solar Heating 10-37-S290-EP

Wind Affects Fuel Moisture 10-38-S290-EP

Wind Affects Fuel Moisture Wind can accelerate the rate at which a fuel reaches its moisture equilibrium. During calm air conditions, the air next to the fuels tends to become saturated with water vapor, decreasing the evaporation rate of moisture from the fuel. Wind removes this saturated air, continually replacing it with drier air and thus speeding up the evaporation process.

How the Amount and Duration of Precipitation and Soil Moisture Affect Moisture Content of Fine and Large Fuels

Fine Dead Fuels Fine, dead fuels react very rapidly to precipitation. Additional rainfall has little effect on the fuels. Rainfall can be responsible for wetting the soils in contact with fuels.

Duration of Precipitation and Fuel Moisture 1-hour 10-hour 100-hour Fuel Moisture Content (percent) Hours of continuous precipitation 10-42-S290-EP

The Fuel Moisture Timelag Concept and its Value to Firefighters and Fire Managers

Timelag is the time it takes dead fuel to reach 63% of the difference between its current moisture content and that it would reach at EMC (maintained at steady environmental conditions). Timelag is an indication of the rate fuel gains or loses moisture due to changes in its environment. It is expressed as the rate (hours) at which the fuel type approaches the moisture equilibrium of its surrounding atmosphere.

Timelag and Fuel Size Relationships 100 60 40 20 10 4 2 1 About 40 days Timelag (days) 1.4 2 4 6 8 10 Branchwood diameter (inches)

Reaction Time of Fuels to Wetting and Drying 12” log 1/2” sticks Moisture content Day Last before day of 1 2 3 4 5 6 Days after Precipitation 10-46-S290-EP

A fuel complex of homogeneous fuel is never seen. A pure grass stand comes closest to being a homogeneous fuel.

Dead Fuel Timelag Categories 1-hour timelag fuels: 0 to 1/4 diameter 10-hour timelag fuels: 1/4” to 1” diameter 100-hour timelag fuels: 1” to 3” diameter 1000-hour timelag fuels: 3” to 8” diameter

Daily Relationship of Relative Humidity to Fine Dead Fuel Moisture RH & moisture percent Moisture content 12PM 6AM NOON 6PM 12PM

How Fuel Moisture is Determined for Dead Fuels in Each of the Four Timelag Categories

Determining Dead Fuel Moisture 1-hour Calculate from fuel moisture charts NFDRS outputs Measure - drying oven and scales 10-hour Fuel moisture sticks NFDRS outputs

Determining Dead Fuel Moisture 100-hour NFDRS outputs Measure - drying oven and scales Calibrated moisture meter 1000-hour NFDRS outputs

Moisture of Extinction: How it Varies in Natural Fuel Complexes and How it Affects Wildland Fire Ignition and Spread

Moisture of Extinction Fuel moisture content at which a fire will not spread or spreads only sporadically and in a non-predictable manner. Dependent upon: Fuel loading Size and shape Arrangement Chemical content 10-58-S290-EP

Moisture of Extinction Fuel Model 1 - Short grass ...........12% Fuel Model 2 - Timber .................15% Fuel Model 3 - Tall grass ..............25% Fuel Model 4 - Chaparral ..............20% Fuel Model 5 - Brush ....................20% Fuel Model 6 - Dormant brush ......25% Fuel Model 7 - Southern Rough ....40%

Moisture of Extinction Fuel Model 8 - Closed timber litter ......30% Fuel Model 9 - Hardwood litter............25% Fuel Model 10 - Timber ..............….....25% Fuel Model 11 - Light slash ................15% Fuel Model 12 - Medium slash ............20% Fuel Model 13 - Heavy slash ...............25%

Determining Fuel Moisture Content in Fine Dead Fuels (1-hour timelag) Dry Bulb Temperature Relative Humidity Reference Fuel Moisture (RFM) + Month Shaded or Unshaded Time of Day Site Location Aspect Slope Fuel Moisture Correction Value (FMC) = Adjusted Fine Dead Fuel Moisture (FDFM) 10-61-S290-EP

Fine Dead Fuel Moisture Worksheet 10-62-S290-EP

Table 2 Reference Fuel Moisture (daytime 0800-1959) Input Line 6 Go to Tables 3, 4, or 5 for corrections. 10-63-S290-EP

Table 3 Fine Dead Fuel Moisture Content Corrections (daytime 0800-1959) May, June, July Input Line 13 Note: B = 1,000 to 2,000 feet below site L = + 1,000 feet of site location A = 1,000 to 2,000 feet above site 10-64-S290-EP

Table 4 Fine Dead Fuel Moisture Content Corrections (daytime 0800-1959) Feb.-Apr., Aug.-Oct. Input Line 13 Note: B = 1,000 to 2,000 feet below site L = + 1,000 feet of site location A = 1,000 to 2,000 feet above site 10-65-S290-EP

Table 5 Fine Dead Fuel Moisture Content Corrections (daytime 0800-1959) November, December, January Input Line 13 Note: B = 1,000 to 2,000 feet below site L = + 1,000 feet of site location A = 1,000 to 2,000 feet above site 10-66-S290-EP

Temperature & Humidity Selection 2,000 feet Above Site (A) New T°/RH% Prediction 1,000 feet Site Location (L) T°/RH% Prediction No adjustment needed 0 feet 1,000 feet Below Site (B) New T°/RH% Prediction 2,000 feet

REFERENCE FUEL MOISTURE DAY (0800-1959) Table 2 REFERENCE FUEL MOISTURE DAY (0800-1959) Input Line 6 Example: Dry Bulb temp: 85o RFM: 3 Relative Humidity: 22 10-68-S290-EP

Fine Dead Fuel Moisture Worksheet 85 22 3 60 62 8 10-69-S290-EP

Table 4 – Fine Dead Fuel Moisture Content Corrections, Day (0800-1759) February, March, April, August, September, October Example: Month: August 20 S/U: Shaded Time: 1200 Elevation: Mid-slope Aspect: East Slope: -- FMC%: 4% 10-70-S290-EP

Fine Dead Fuel Moisture Worksheet Aug May 1200 1400 E S -- 20 4 10-71-S290-EP

REFERENCE FUEL MOISTURE DAY (0800-1959) Table 2 REFERENCE FUEL MOISTURE DAY (0800-1959) Input Line 6 Example: Dry Bulb temp: 92o RFM: 2 Relative Humidity: 16 10-72-S290-EP

Table 5 – Fine Dead Fuel Moisture Content Corrections, Day (0800-1759) November, December, January Example: Month: November S/U: Unshaded Time: 1500 Elevation: 1500 Above Aspect: West Slope: 40% FMC%: 3% B = 1000 to 2000 feet below site location L = +/- 1000 feet of site location A = 1000 to 2000 feet above site location 10-73-S290-EP

Solution to Question 3.a. 5 3a 92 --- 16 2 Nov 1500 W 40 3 10-74-S290-EP

Solution to Question 3.b. 8 3b 75 --- 28 4 Oct 1700 N 20 4 10-75-S290-EP

Solution to Question 3.b. 4 5 6 B L A 80 80 80 20 20 20 3 3 3 Aug Aug 1600 1600 1600 N N N 20 20 20 1 2 3 4 5 6 10-76-S290-EP

Severe Fire Behavior Potential Related to Relative Humidity and Fuel Moisture Content (For Western US only) 10-77-S290-EP

Review Unit 10 Objectives Define critical live fuel moisture and the thresholds for various fuel types. Identify three methods for obtaining live fuel moisture. Describe the relationships between relative humidity, wind, and moisture content of fine and large fuels.

Review Unit 10 Objectives Explain how the amount and duration of precipitation and soil moisture affect moisture content of fine and large fuels. Define the fuel moisture timelag concept and its value to firefighters and fire managers. Describe how fuel moisture is determined for dead fuels in each of the four timelag categories.

Review Unit 10 Objectives Define moisture of extinction, how it varies in natural fuel complexes, and how it affects wildland fire ignition and spread. Determine fuel moisture content for fine dead 1-hour timelag fuels from fuel moisture tables during daylight conditions.