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Fire ecology of forests and woodlands in Utah PDF

138 Pages·1992·12.6 MB·English
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Historic, Archive Document Do assume not content reflects current scientific l<nowleclge, policies, or practices. United States Fire Ecology of Forests Department of Agriculture and Woodlands Forest Service Utah in Intermountain Research Station General Technical Anne Bradley F. Report INT-287 Nonan Noste V. June 1992 William C. Fischer CP . \ -« ^3 THE AUTHOF United States Department of Agriculture Page ANNE BRADI F. 1 specialist forthe 1 Staff of the Fore! 6 in San Francisco r Tree Species to Fire 6 occurred while a; pulus tremuloides) 6 Effects: Prescrib 'nus ponderosa) 7 unit at the Internr otsuga menziesii) 7 tain Fire Science {Picea engelmannii) 8 earned a B.A. de nus contorta) 8 and an M.A. deg s lasiocarpa) 8 Montana. Early National Agricultural Library ncoloi) 9 naturalist for the \pungens) 9 biological techni( e {Pinus longaeva) 9 Intermountain St_ ^'giiriugrrnrciFTTTpg flexilis) 10 NONAN V. NOSTE (retired) was a forester, Inter- Gambel Oak {Quercusgambelii) 10 mountain Research Station, Intermountain Fire Pinyon {Pinus edulis) and Singleleaf Pinyon Sciences Laboratory, Missoula, MT. During his Forest Pinus monophylla) 10 ( Service career, Nonan was involved in fire control Utah Juniper {Juniperus osteosperma) 11 research in Alaska; silviculture research in Wisconsin, Rocky Mountain Juniper and fire technology and fire effects and use research {Juniperus scopulorum) 11 in Missoula. He earned B.S. and M.F. degrees in Undergrowth Response to Fire 11 forestry from the University of Montana. Wildlife Response to Fire 18 WILLIAM C. FISCHER is a research forester and Fire Use Considerations 30 Fuels 30 team leader for the Fire Effects work unit at the Predicting Fire Mortality 32 Intermountain Research Station, Intermountain Fire Crown Damage and Insect Attack 34 Sciences Laboratory, Missoula, MT. He is a graduate Frequency of Burning 34 of Paul Smith's College and the University of Michigan Large Woody Debris 34 (B.S., B.S.F. 1956). Priorto joining the staff at the Fire Sciences Laboratory, he was employed in a variety of Heat Effects on Soil 35 fire and resource management assignments with the Prescribed Fire Planning 35 Fire Group Zero: Miscellaneous Special Habitats ....35 Boise National Forest in Idaho. Scree 35 Forested Rock 35 RESEARCH SUMMARY Wet Meadow 35 Mountain Grassland 36 This report summarizes available information on fire Deciduous Riparian Communities 36 as an ecological factor for forest habitat types and the unclassified pinyon-juniper and oak-maple woodlands Fire Group One: Pinyon-Juniper Woodlands 36 Vegetation 36 occurring in Utah. Habitat types and the unclassified Forest Fuels 37 vegetative communities are assigned to Fire Groups based on fire's potential role in forest succession. Role of Fire 38 Woodland Succession 39 For each Fire Group, the authors discuss (1) the relationships of major tree species to fire, (2) forest Fire Management Considerations 41 Fire Group Two: Montane Maple-Oak Woodlands...41 fuels, (3) the natural role of fire, (4) fire's hypothetical role in forest succession, and (5) fire management Vegetation 41 Fuels 42 considerations. intermountain Research Station 324 25th Street Ogden, UT 84401 Page Page Role of Fire 43 Fire Group Eight: Habitat Types with Brushland Succession 44 Persistent Lodgepole Pine 79 Fire Management Considerations 44 Habitat Types, Phases 79 Fire Group Three: Ponderosa Pine Habitat Types ...45 Vegetation 79 Habitat Type, Phase 45 Forest Fuels 79 Vegetation 46 Role of Fire 82 Forest Fuels 47 Forest Succession 85 Role of Fire 48 Fire Management Considerations 87 Forest Succession 49 Fire Group Nine: Climax Stands Dominated by Fire Management Considerations 52 Limber Pine or Western Bristlecone 89 Fire Group Four: Drier Douglas-fir Habitat Types ....54 Habitat Types, Phases 89 Habitat Types, Phases 54 Vegetation 89 Vegetation 54 Forest Fuels 90 Forest Fuels 54 Role of Fire 90 Role of Fire 55 Forest Succession 91 Forest Succession 56 Fire Management Considerations 91 Fire Management Considerations 58 Fire Group Ten: Dry, Lower Subalpine Fire Group Five: Cool or Moist Douglas-fir Habitat Types 92 Habitat Types 59 Habitat Types, Phases 92 Habitat Types, Phases 59 Vegetation 93 Vegetation 59 Forest Fuels 93 Forest Fuels 59 Role of Fire 94 Role of Fire 59 Forest Succession 94 Forest Succession 61 Fire Management Considerations 99 Fire Management Considerations 64 Fire Group Eleven: Moist to Wet Subalpine Fire Group Six: White Fir and Blue Spruce Habitat Types 99 Habitat Types (Mixed Conifer Types) 64 Habitat or Community Types 99 Habitat Types, Phases 64 Vegetation 99 Vegetation 64 Forest Fuels 100 Forest Fuels 66 Role of Fire 100 Role of Fire 67 Forest Succession 101 Forest Succession 67 Fire Management Considerations 101 Fire Management Considerations 69 Fire Group Twelve: Cold, Upper Subalpine Fire Group Seven: Aspen-Dominated Habitat Habitat Types 102 and Community Types 70 Habitat Types, Phases 102 Stable Community Types (Probably Vegetation 102 Climax Habitat Types) 70 Forest Fuels 102 Community Types (and Cover Types) Role of Fire 102 Probably Serai to Coniferous Habitat Types 70 Forest Succession 103 Community Types Probably Grazing Fire Management Considerations 104 Disclimaxes 71 References 104 Vegetation 71 Appendix A: Forest and Woodland Habitat Forest Fuels 71 and Community Types Assigned to Role of Fire 72 Utah Fire Groups 120 Forest Succession 74 Appendix B: Common and Scientific Fire Management Considerations 75 Names Mentioned in Text 125 — Fire Ecology of Forests and Woodlands Utah In Anne F. Bradley Nonan V. Noste William C. Fischer INTRODUCTION major topics presented in this report are organized into sections, described below. This report summarizes the available fire ecology and management information relating to forest Relationship ofMajor Tree Species to Fire habitat types, montane oak-maple woodlands, and This section discusses each principal tree species in pinyon-juniper woodlands ofUtah. Specifically, the Utah forests with regard to its resistance or suscep- report covers the Wasatch-Cache, Dixie, Fishlake, tibility to fire and its role as a successional compo- Manti-La Sal, Ashley, and Uinta National Forests nent offorest communities. Particular attention is and the Raft River Mountain portion ofthe Sawtooth given to special adaptations to fire, such as corky bark, serotinous cones, or seeds that require mineral National Forest, but it is also applicable to the for- ested portions ofZion and Bryce Canyon National soil for germination. — Parks and Cedar Breaks National Monument. The Undergrowth Response to Fire This section primary purpose ofthis report is to promote the un- summarizes the effect offire on the response ofim- derstanding offire's role, particularly its influence portant grass, forb, and shrub species associated on succession in the forests, pinyon-juniper wood- with the major conifer species. Particular attention lands, and oak-maple brushlands ofUtah, is given to fire-adaptive traits or survival strategies The habitat types recently described by Mauk that determine whether fire generally increases or and Henderson (1984), Youngblood and Mauk decreases species cover in the immediate postfire (1985), and to a limited extent the community types period. described by Padgett and others (1989) and by — Wildlife Response to Fire This section con- Mueggler (1989) are assigned to 13 "Fire Groups" tains briefsummaries ofthe general effects offire on based on the response ofdominant tree species to common Utah mammals, reptiles, amphibians, and fire and similarity ofdevelopment in postfire succes- birds. Fire response ofwildlife is largely inferred sion. In Utah, neither pinyon-juniper woodlands nor from expected changes in habitat as a result offire. montane woodlands dominated by Gambel oak or — bigtooth maple have been classified by habitat type. Fire Use Considerations This section summa- These woodlands therefore have been assigned to rizes cautions that apply to the use offire for re- Fire Groups on the basis ofcover type. Both pinyon- source management purposes. Emphasis is on effec- juniper and oak-maple cover large acreages in the tive use offire, site protection, minimizing damage State. to residual stand, and wildlife habitat protection. The successional path taken by any given site fol- Fire Groups—The Fire Groups (FG's) are defined lowing fire depends on many variables. The preburn with reference to "Coniferous Forest Habitat Types vegetation, size and severity ofthe fire, topography, ofNorthern Utah" (Mauk and Henderson 1984), "Co- climate and soil, and chance all contribute to the niferous Forest HabitatTypes ofCentral and South- process. Thus, a single habitat type may be a mem- em Utah" (Youngblood and Mauk 1985), "Aspen ber ofmore than one Fire Group. The individual Community Types ofthe Intermountain Region" land manager must evaluate conditions on a site by (Mueggler 1989), and "Riparian Community Types site basis to determine the most likely results offire. ofUtah and Southeastern Idaho" (Padgett and oth- The groups defined in this report are offered as a ers 1989). Generally, a habitat type or habitat type general guide, not a definitive treatment. phase is assigned to only one Fire Group. Where exceptions to this rule occur, the exception is noted Format and explained. The foresthabitat types assigned to the Utah Fire Groups are listed in appendix A and This report is patterned after "Fire Ecology of summarized in table 1. General descriptive litera- Montana Forest Habitat Types East ofthe Conti- ture was used to identify pinyon-juniper woodlands nental Divide" (Fischer and Clayton 1983). The (FG 1) and oak-maple woodlands (FG 2), because 1 — Table 1 Summary of Utah habitat type Fire Groups (see appendix A forformal listing of habitattypes) Habitat type Habitat type Habitat type FIRE GROUP ZERO PIPU/BERE PICOA/ASC Misc. special habitats PIPU/JUCO PIENA/AGA PIENA/ASC FIRE GROUP ONE FIRE GROUP SEVEN Pinyon-juniper woodlands POTR/AMAI_/PTAQ FIRE GROUP NINE FIRE GROUP TWO POTR/AMAI_/TALL FORB PIFL/BERE POTR/AMAI7THFE PIFUCELE Montane maple-oak POTR/AMAUCARU FIRE GROUP TEN FIRE GROUP THREE POTR/AMAL-SYORATALL FORB ABLA/ACGL PIPO/ARPA POTR/ARTR ABLA/BERE-CAGE PIPO/ARNO POTR/CARU ABLA/BERE-JUCO PIPO/CAGE POTR/CARO ABLA/BERE-PIEN PIPO/CELE POTR/FETH ABLA/BERE-PIFL PIPO/FEiD-ARPA POTR/TALL FORB ABLA/BERE-PSME PIPO/FEID-ARTR POTR/JUCO/CAGE ABLA/BERE-RIMO PIPO/FEID-FEID POTR/JUCO/LUAR ABLA/BERE-BERE PIPO/MUMO POTR/PTAQ ABLA/CAGE PIPO/PUTR POTR/SARA ABLA/CARO PIPO/QUGQ-SYOR POTR/STCO ABLA/CARU PIPO/QUGQ-QUGA POTR/SYOR/CARO ABLA/JUCO PIPO/SYOR POTR/SYOR/CARU ABLA/OSCH POTR/SYOR/THFE FIRE GROUP FOUR ABLA/PERA-PSME POTR/SYOR/FETH PSME/ARPA ABLA/PERE-PERA POTR/SYOR/TALL FORB PSME/BERE-CAGE ABLA/PHMA POTR/VECA PSME/BERE-PlPO ABLA/RIMO-MEAR POTR-ABLA/AMAL PSME/CELE ABLA/RIMO-PICO POTR-ABLA/CAGE PSME/CEMO ABLA/RIMO-THFE POTR-ABLA/CARO PSME/QUGA ABLA/RIMO-RIMO POTR-ABLA/JUCO PSME/SYOR ABLAA/ACA POTR-ABLA/SYOR/THFE FIRE GROUP FIVE POTR-ABLA/SYOR/TALL FORB ABLAA/ACA-PIEN ABLAA/AGL PSME/ACGL POTR-ABLA/TALL FORB ABLAA/AMY PSME/BERE-JUCO POTR-ABCO/ARPA ABLAA/ASC-ARLA PSME/BERE-SYOR POTR-ABCO/POPR ABLAA/ASC-CAGE PSME/BERE-BERE POTR-ABCO/SYOR ABLAA/ASC-VASC PSME/CARU POTR-PIPU PSME/OSCH-PAMY POTR-PICO FIRE GROUP ELEVEN PSME/PHMA POTR-PICO/CAGE ABLA/ACCO PSME/PHMA-PAMY POTR-PSME/AMAL ABLA/ACRU FIRE GROUP SIX POTR-PSME/JUCO ABLA/CACA ABCO/ACGL POTR/ASMI ABLA/STAM POTR/BRCA PIEN/EQAR ABCO/ARPA ABCO/BERE-JUCO POTR/JUCO/ASMI PIEN/CALE PIPU/EQAR ABCO/BERE-SYOR FIRE GROUP EIGHT CONIFER/COSE ABCO/BERE-BERE ABLAA/ACA CONIFER/ACCO ABCO/CELE ABLA/VASC-VASC ABCO/JUCO PICO/ARUV FIRE GROUP TWELVE ABCO/OSCH PICO/BERE ABLA/RIMO-TRSP ABCO/PHMA PICO/CACA ABLAA/ASC-VASC ABCO/QUGA PICO/CARO PIEN/RIMO ABCO/SYOR PICO/JUCO PIENA/ACA PIPU/AGSP PiCOA/ACA PIENA/ASC 2 classification ofthese vegetation types in Utah is not Abies concolor, white fir (ABCO) complete. Abies lasiocarpa, subalpine fir (ABLA) Habitat types and community types are desig- Acergrandidentatum, bigtooth or canyon maple nated in the standard format of"series/type-phase," (ACGR) in which "series" designates the potential climax Juniperus osteosperma, Utahjuniper (JUGS) dominant tree, "type" designates a definitive under- Juniperus scopulorum, Rocky Mountainjuniper growth species, and "phase" provides a further sub- (JUSC) division where needed. Picea engelmannii, Engelmann spruce (PIEN) — Piceapungens, blue spruce (PIPU) Vegetation Following the list ofhabitat types Pinus contorta, lodgepole pine (PICO) that comprise each Fire Group, we describe the Pinus edulis, pinyon pine or two-needle pinyon characteristic overstory and undergrowth vegetation (PIED) for that Group. Climax and serai tree species are Pinusflexilis, limber pine (PIFL) identified. — Pinus longaeva, Western bristlecone (PILO) Forest Fuels The fuels likely to occur in each Pinus monophylla, singleleafpinyon (PIMO) Fire Group are characterized in this section. The Pinusponderosa, ponderosa pine (PIPO) emphasis is on downed and dead woody fuels. Live Populus tremuloides, aspen (POTR) and standing dead fuels are also discussed where Pseudotsuga menziesii, Douglas-fir (PSME) they contribute significantly to fire hazard. To date, Quercusgambelii, Gambel oak (QUGA) there are no published summaries offuel loadings — Fire Severity For the purpose ofthis report by cover type or habitat type for coniferous forests three levels offire severity are recognized: low or and woodlands in Utah. Consequently, ifapplicable, cool, moderate, and high or severe. A low-severity or fuel estimates fi*om surrounding States are pre- sented. For each Fire Group, we discuss the kind cool fire is one that has minimal impact on the site. and amount ofdead, woody material likely to be It burns in surface fuels consuming only the litter, herbaceous fuels, and foliage and small twigs on found on the forest floor. — woody undergrowth. Very little heat travels down- Role of Fire Information on the ecology ofthe ward through the duff. A moderate fire burns in important trees, fuel characteristics, and the results surface fuels also but may involve a tree understory offire history studies are integrated to describe the as well. It consumes litter, upper duff, understory historical (presettlement period, generally prior to plants, and foliage on understory trees. Individual the mid-1800's) role offire in shaping the vegetative and groups ofoverstory trees may torch out iffuel composition ofa particular Fire Group. This section ladders exist. Aseverefire is one that burns through is mainly a literature review covering succession and the overstory and consumes large woody surface fire within the appropriate habitat types or plant fuels, or removes the entire dufflayer, or both, over communities. much ofthe area. Heat from the fire impacts the — Forest Succession For each Fire Group, succes- upper soil layer and often consumes the incorpo- sional pathway flow charts represent a synthesis of rated soil organic matter. both knowledge and speculation about the effects of The amount ofsoil heating is critical to the sur- fire at several points in the life history ofa stand. vival oftree roots and resprouting undergrowth spe- They illustrate the many possible influences fires of cies. Observing soil surface characteristics after fire varying severities have on stands ofdiffering ages, can help make predictions ofpostbum plant re- densities, and species composition. The flow charts sponse more accurate. Ryan and Noste (1985) have follow the method suggested by Kessell and Fischer presented some easily observable soil and fuel char- acteristics to determine the relative depth ofchar in (1981). How trees respond to fire often depends on their different vegetation types (table 2). — size. Tre—e size classes used in our flow charts are: Fire Management Considerations This sec- saplings 2 to 4 inc—hes in diameter at breast height tion discusses how the preceding information can be (d.b.h—.); small poles trees 4 to 8 inches d.b.h.; large used to develop fire management plans that support poles 8 to 12 inches d.b.h. (Society ofAmerican land and resource management objectives. Sugges- Foresters, 1958). tions given are offered as an aid to decision making, The tree species names are symbolized in order to but for specific situations the manager must rely on simplify the diagrams and flow charts. The symbols personal experience to best determine how to use in- are defined as follows: formation presented in this document. 3 — Table 2 Visual character of ground char from observation of depth of burn^ (Ryan and Noste 1985) Ground char Site class Timber/slash Shrub fields Grasslands Unburned The fire did not burn on the See timber/slash See timber/slash forest floor. Some damage may occurto vegetation due to radiated or convected heatfrom adjacent areas. Ten to 20 percent of the area within slash burns is commonly unburned.^ There is a wide range in the percent of unburned area within fires in natural fuels. Light Leaf litter is charred or Leaf litter is charred or Litter is charred or ground consumed. consumed, and some leaf consumed, but some plant char structure is still discernible. parts are still discernible. Upper duff may be charred, but the duff layer is not The surface is predomi- Charring may extend slightly altered overthe entire depth. nantly black, although some into the soil surface, but gray ash may be present the mineral soil is not The surface generally appears immediately afterthe fire. othenwise altered. black immediately after the fire. Gray ash soon becomes Some plant parts may still Woody debris is partially burned. inconspicuous. be standing. Some small twigs and much of the Charring may extend slightly Bases of plants are not branch wood remain. into soil surface where deeply burned and are still leaf litter is sparse, but recognizable. Logs are scorched or blackened the mineral soil is not but not charred. otherwise altered. Surface is predominantly black immediately afterthe Crumbled, rotten wood is Some leaves and small twigs burn, butthis soon becomes scorched to partially burned. remain on the plants. Burns inconspicuous. are irregular and spotty. Light ground char commonly makes Burns may be spotty to up 0-100 percent of burned areas Less than 60 percent ofthe uniform, depending on the with natural fuels and 45-75 brush canopy is commonly continuity ofthe grass. percent of slash areas. consumed. Moderate Litter is consumed.^ Surface leaf litter is Litter is consumed, and the ground consumed. surface is covered with char Duff is deeply charred or con- gray or white ash immediately sumed butthe underlying mineral Some charred litter may afterthe burn. soil is not visibly altered. remain but is sparse. Ash soon disappears, leaving Light-colored ash prevails Charring extends upto bare mineral soil. immediately after the fire. 0.5 inch into mineral soil but does not otherwise unarring exienas siigniiy Woody debris is largely consumed. alterthe mineral soil. into mineral soil, but the plant parts are no longer Some branch wood is present, but Gray orwhite ash is con- discernible, no plant parts no foliage or twigs remain. spicuous immediately after standing, and the bases of the burn, but this quickly plants are burned to ground Logs are deeply charred. disappears. level. (con.) 4

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