首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Effectiveness of prescribed fire to re-establish sagebrush steppe vegetation and ecohydrologic function on woodland-encroached sagebrush rangelands, Great Basin, USA: Part I: Vegetation, hydrology, and erosion responses
【24h】

Effectiveness of prescribed fire to re-establish sagebrush steppe vegetation and ecohydrologic function on woodland-encroached sagebrush rangelands, Great Basin, USA: Part I: Vegetation, hydrology, and erosion responses

机译:规定火灾重新建立Sagebrush STAGEPE植被的有效性和林地侵犯Sagebrush牧场的生态流学功能,美国伟大的盆地,伟大的盆地:第一部分:植被,水文和侵蚀反应

获取原文
获取原文并翻译 | 示例
           

摘要

Pinyon (Pinus spp.) and juniper (Juniperus spp.) woodland encroachment has imperiled a broad ecological domain of the sagebrush steppe (Artemisia spp.) ecosystem in the Great Basin Region, USA. As these conifers increase in dominance on sagebrush rangelands, understory vegetation declines and ecohydrologic function can shift from biotic (vegetation) controlled retention of soil resources to abiotic (runoff) driven loss of soil resources and long-term site degradation. Scientists, public land management agencies, and private land owners are challenged with selecting and predicting outcomes to treatment alternatives to improve ecological structure and function on these rangelands. This study is the first of a two-part study to evaluate effectiveness of prescribed fire to re-establish sagebrush steppe vegetation and improve ecohydrologic function on mid- to late-succession pinyon-and juniper-encroached sagebrush sites in the Great Basin. We used a suite of vegetation and soil measures, small-plot (0.5 m(2) ) rainfall simulations, and overland flow experiments (9 m(2) ) to quantify the effects of tree removal by prescribed fire on vegetation, soils, and rainsplash, sheetflow, and concentrated flow hydrologic and erosion processes at two woodlands 9-yr after burning. For untreated conditions, extensive bare interspace (87% bare ground) throughout the degraded intercanopy (69-88% bare ground) between trees at both sites promoted high runoff and sediment yield from combined rainsplash and sheetflow (similar to 45 mm, 59-381 g m(-2) ) and concentrated flow (371-501 L, 2343-3015 g) processes during high intensity rainfall simulation (102 mm h(-1) , 45 min) and overland flow experiments (15, 30, and 45 L min(-1) , 8 min each). Burning increased canopy cover of native perennial herbaceous vegetation by > 5-fold, on average, across both sites over nine growing seasons. Burning reduced low pre-fire sagebrush canopy cover ( < 1% to 14% average) at both sites and sagebrush recovery is expected to take > 30 yr. Enhanced herbaceous cover in interspaces post-fire reduced runoff and sediment yield from high intensity rainfall simulations by > 2-fold at both sites. Fire-induced increases in herbaceous canopy cover (from 34% to 62%) and litter ground cover (from 15% to 36%) reduced total runoff (from 501 L to 180 L) and sediment yield (from 2343 g to 115 g) from concentrated flow experiments in the intercanopy at one site. Sparser herbaceous vegetation (49% cover) and litter cover (8%) in the intercanopy at the other, more degraded site post-fire resulted in no significant reduction of total runoff (371 L to 266 L) and sediment yield (3015 g to 1982 g) for concentrated flow experiments. Areas underneath unburned shrub and tree canopies were well covered by vegetation and ground cover and generated limited runoff and sediment. Fire impacts on vegetation, ground cover, and runoff and sediment delivery from tree and shrub plots were highly variable. Burning litter covered areas underneath trees reduced perennial herbaceous vegetation and increased invasibility to the fire-prone annual cheatgrass (Bromus tectorum L.). Cheatgrass cover increased from < 1% prefire to 16-30%, on average, post-fire across the sites and was primarily restricted to areas around burned trees. High herbaceous cover (73%) under burned trees at the less degraded site resulted in similar low total runoff and sediment from concentrated flow experiments as prefire (136-228 L, 204-423 g).
机译:拼音(Pinus SPP。)和杜松(Juniperus SPP)林地侵占在美国伟大的盆地地区的山宫草原(Artemisia SPP)的广泛生态领域。由于这些针叶树在山萧牧场的主导地位增加,较大的植被下降和生态中的功能可以从生物(植被)控制的土壤资源对非生物(径流)驱动的土壤资源丧失和长期站点退化。科学家,公共土地管理机构和私立土地所有者受到选择和预测治疗替代方案的挑战,以改善这些牧场的生态结构和功能。本研究首先,评估规定火灾的有效性重新建立Sagebrush Steppe植被,并在伟大的盆地中的前后连续丛生丛生的生态功能改善生态学功能。我们使用了一套植被和土壤措施,小图(0.5米(2))降雨模拟,以及陆上流动实验(9米(2)),量化规定的火灾对植被,土壤和土壤的效果在燃烧后,两个林地9-YR的Risoplash对于未经处理的条件,两种裸露的树木之间的裸露间隙(87%裸机)在两个地点之间的树木之间的裸露(69-88%裸机)促进了从汇率平台和片状流出的高径流和沉积物产量(类似于45 mm,59-381 GM(-2))和浓缩流(371-501L,2343-3015g)在高强度降雨模拟期间(102mm H(-1),45分钟)和陆上流动实验(15,30和45升)分钟(-1),每次8分钟)。在九个生长季节的两个地点,平均地,燃烧天然多年生草本植物的冠层覆盖的天然多年生草本植物覆盖。燃烧的低火灾山脉顶篷覆盖(<1%至14%)在两个地方和Sagebrush恢复都预计将采用> 30年。在射击后的间隙中增强了草本覆盖物,降低了径流和沉积物产量,在两个地方的高强度降雨模拟中从高强度降雨模拟。未诱导的草本植物覆盖物(34%至62%)和垃圾接地盖(15%至36%)降低总径流(从501升到180升)和沉积物产量(从2343g到115g)从一个地点的嵌段中浓缩流实验从嵌段中进行。在另一个更加降解的地方的嵌段中稀疏草本植物(49%覆盖)和垃圾覆盖(8%),导火后的更加降解的部位导致总径流的显着降低(371升至266升)和沉积物产量(3015 g至1982g)用于集中的流动实验。未燃烧的灌木和树木檐下方的区域被植被和地面覆盖覆盖,并产生有限的径流和沉积物。火灾对植被,地面覆盖和径流和树木划分的影响以及灌木和灌木地块的影响很大。树木下面的燃烧凋落物覆盖区域降低了多年生草本植物,并增加了对火灾的年度小包包(Bromus Tectorum L)的侵入性。作弊覆盖率从<1%的前盖增加到16-30%,平均,在该地点的火灾后,主要限于烧焦树木周围的区域。在较低的降解的位点下烧成的树木下的高草本覆盖(73%)导致浓缩的流动实验中的浓度相似的低总径流和沉积物(136-228L,204-423g)。

著录项

相似文献

  • 外文文献
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号