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Characteristics of small headwater wetlands in second-growth forests of Washington, USA

机译:美国华盛顿次生林中小型源头湿地的特征

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a- Headwater wetland features were common (60+ observed). a- The features show affinity with northerly aspects and perennial surface water. a- Feature origin may relate to recent large down channel wood rather than legacy wood. a- Cumulative headwater wetland area may be sizable, but is not typically surveyed prior to logging. In 2002, we initiated a study to clarify the response of headwater catchments to logging on timberlands in the Coast Range of Washington, USA. Most of the predominantly first-order streams studied (summer low flows typically<0.3Lsa degree 1) were hydrologically complex, consisting of a main surface channel connected to multiple, small wetlands. To better understand the forest management implications of headwater systems with two surface hydrology components of potentially differing areal extents (i.e., broad wetlands and narrow, channelized flow), we examined in more detail the wetlands associated with 30 headwater channels. On average, 2.3 wetlands occurred per channel. All 68 surveyed wetlands were, individually, smaller than 0.1ha, which is a minimum survey-and-manage size criterion for forested wetlands in use in the Pacific Northwest. Seventy-nine percent of the wetlands surveyed by the full-triad method met regional wetland triad criteria for wetland delineation (qualifying wetland soils, hydrology, and vegetation indicators). These headwater wetlands were associated with several landscape variables: (1) northerly-facing catchments, (2) perennial surface water, and (3) down, channel-associated large wood originating from adjacent riparian forest. Our results show that small forested wetlands are quite common and that the surface area of small wetlands can rival the surface area of the associated first-order streams. This initial effort to quantify characteristics of small headwater wetlands suggests small wetlands could dominate or influence headwater surface area processes including those associated with stream responses to disturbances such as logging.
机译:a-水源湿地特征很普遍(观察到60多个)。 a-这些特征显示出与北风和多年生地表水的亲和力。 a-特征起源可能与最近的大型下行通道木材有关,而不是与传统木材有关。 a-累积的源头湿地面积可能相当大,但通常在伐木之前不进行调查。 2002年,我们启动了一项研究,以弄清源头集水区对美国华盛顿海岸山脉林地伐木的反应。大多数被研究的一级流(夏季的低流量通常<0.3Lsa度1)在水文方面很复杂,由连接到多个小型湿地的主水道组成。为了更好地了解具有两个可能具有不同面积范围的地表水文学成分(即宽阔的湿地和狭窄的通道流)的源水系统的森林管理意义,我们更详细地研究了与30个源水通道相关的湿地。平均每个通道有2.3个湿地。所有68个被调查的湿地分别小于0.1公顷,这是西北太平洋地区使用的森林湿地的最低调查和管理规模标准。通过全黑社会方法调查的湿地中,有79%符合区域湿地黑社会对湿地划分的标准(使湿地土壤,水文和植被指标合格)。这些源头湿地与几个景观变量相关联:(1)朝北的集水区;(2)多年生地表水;以及(3)与河道相关的,来自相邻河岸森林的大木材。我们的结果表明,森林茂密的小湿地非常普遍,并且小湿地的表面积可以与相关一级流的表面积相媲美。量化小型上游水源湿地特征的初步努力表明,小型湿地可主导或影响上游水面过程,包括与河流对干扰(如伐木)的响应相关的过程。

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