恢复蒙大拿州西部依赖火的黄松林

S. Arno, M. Harrington, C. Fiedler, C. Carlson
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引用次数: 84

摘要

|抑制。任何林业工作者和生态学家都认识到,黄松林频繁火灾的历史模式遭到破坏,导致了重大的生态变化,包括日益严重的野火和虫害和疾病流行(Weaver, 1943;Covington and Moore, 1992;穆奇等人,1993;埃弗雷特,1994)。由于认识到这一点,自然资源管理人员、生物学家和公众对将黄松林恢复到更自然和可持续的条件越来越感兴趣(美国森林,1995年)。山间研究站和蒙大拿大学林业学院与比特根国家森林和洛洛国家森林合作,一直在测试不同的造林和规定的火灾处理对恢复黄松林的有效性,我们将在这里报告一些观察结果和初步发现。但首先,我们将总结已经发生的生态变化,并描述我们的恢复措施。几千年来,火塑造了北美森林的组成和结构,有利于黄松(Pinus ponderosa)等物种,这些物种耐火,需要火来再生并与其他物种成功竞争(Pyne, 1982, Agee, 1993)。在内陆西部,纯黄松和混合黄松-冷杉类型是最广泛的火依赖森林。与黄松相关的不依赖火的树种有室内道格拉斯冷杉(pseudosuga menziesii var. glauca)、大冷杉(Abies grandis)、白杉(A. concolor)和香杉树(Calocedrus decurrens)。在美国西部,纯黄松和混合黄松类型覆盖了大约4000万英亩(1600万公顷),相当于华盛顿州的面积(van Hooser和Keegan, 1988)。在20世纪初之前,这些森林的特点是经常发生低到中等强度的火灾,主要是烧毁了很少的上层松树。从历史上看,在大多数地区,平均每隔5到30年发生一次火灾,使小树变薄,并有助于形成开放的、公园状的、防火的林分(Amo, 1988)。今天,许多这些森林发生了巨大变化,由于60-80年的禁火和砍伐上层松树,正在经历严重的健康问题。例如,俄勒冈州东部蓝山100多万英亩的土地现在大多是死亡或垂死的树木,主要是受到虫害和疾病流行影响的冷杉丛林(穆奇等人,1993年)。此外,以前在开阔的黄松林中很少发生的大规模破坏林分的野火,在由于防火而发展起来的茂密林分中变得很常见。茂密的树木也提供了燃料梯子,导致火灾强度增加并爬上树冠。1994年,黄松的严重火灾占据了西部内陆300万英亩土地的很大一部分。过去的伐木有选择地砍伐了大型松树,留下了林下树木,这使得针叶林得以迅速发展(Habeck, 1990)。广泛的案件,
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Restoring Fire-Dependent Ponderosa Pine Forests in Western Montana
| suppression. M any foresters and ecologists recognize that disruption of the historic pattern of frequent fires in ponderosa pine forests has resulted in major ecological changes, including increasingly severe wildfires and insect and disease epidemics (Weaver, 1943; Covington and Moore, 1992; Mutch and others, 1993; Everett, 1994). In response to this realization, there is increasing interest among natural resource managers, biologists, and the public in restoring ponderosa pine forests to more natural and sustainable conditions (American Forests, 1995). The Intermountain Research Station and the University of Montana’s School of Forestry, in cooperation with the Bitterroot and Lolo National Forests have been testing the effectiveness of different silvicultural and prescribed-fire treatments for restoring ponderosa pine forests, and we will report some observations and initial findings here. But first we will summarize ecological changes that have occurred and describe our restoration treatments. For thousands of years fire shaped the composition and structure of North American forests, favoring species such as ponderosa pine (Pinus ponderosa) that are fireresistant and require fire to regenerate and compete successfully with other species (Pyne, 1982, Agee, 1993). In the inland West, pure ponderosa pine and mixed ponderosa pine-fir types are the most extensive of the fire-dependent forests. Non-fire-dependent species associated with ponderosa pine are interior Douglas-fir (Pseudotsuga menziesii var. glauca), grand fir (Abies grandis), white fir (A. concolor), and incensecedar (Calocedrus decurrens). Pure and mixed ponderosa pine types cover about 40 million acres (16 million hectares) in the western United States, an area equal to that of the state of Washington (van Hooser and Keegan, 1988). Prior to the early 1900s these forests were characterized by frequent lowto moderate-intensity fires, mostly underbums that killed few overstory pines. Historically, fires at intervals averaging five to 30 years in most areas thinned small trees and helped produce open, park-like, fire-resistant stands (Amo, 1988). Today many of these forests have changed dramatically and are experiencing critical health problems as a result of 60-80 years of fire exclusion and logging of overstory pines. For example, more than a million acres in eastern Oregon’s Blue Mountains now consist mostly of dead or dying trees, primarily fir thickets impacted by insect and disease epidemics (Mutch and others, 1993). Also, large stand-destroying wildfires, formerly rare in the open ponderosa pine forests, have become common in the dense stands that have developed as a result of fire exclusion. Dense stands also provide fuel ladders that cause fires to increase in intensity and climb into tree crowns. Severe fires in ponderosa pine made up a large portion of the three million acres that burned in the inland West during 1994. Past logging, which selectively removed large pines and left understory trees has allowed rapid development of conifer thickets (Habeck, 1990). Extensive coni-
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