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首页> 外文期刊>Forest Ecology and Management >Phosphorus release from forest harvesting on an upland blanket peat catchment.
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Phosphorus release from forest harvesting on an upland blanket peat catchment.

机译:旱地覆盖的泥炭流域的森林中的磷释放。

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摘要

The aim of this study was to investigate the release of phosphorus (P) to receiving waters resulting from harvesting 34-year-old lodgepole pine trees in an upland peat catchment. The study site was within a 25.3-hectare (ha) area, and was drained by a stream that received flows from ploughed furrows, mainly, via collector drains, and discharged directly to the salmonid Shrahrevagh River, Burrishoole, Co. Mayo, Ireland. The study site was divided into two parts: the upstream part was left intact and the downstream part was harvested in early Autumn 2005 following implementation of forest guidelines. Good management practices such as proper use of brash mats and harvesting only in dry weather were implemented. Two instrumented stations were established - one just upstream (US) and the other just downstream (DS) of the clearfelled area. The measurement of P concentrations at the two stations commenced in May 2005, two months before the harvesting started. The daily mean P concentration at the DS station increased from about 6 micro g L-1 of total reactive phosphorus (TRP) during pre-clearfelling to 429 micro g L-1 in August 2006. By October 2009, four years after clearfelling, the P concentrations at the DS station had returned to pre-clearfelling levels. In the first three years after harvesting, up to 5.15 kg ha-1 of TRP was released from the harvested catchment to the receiving water; in the second year alone, 2.3 kg ha-1 of TRP was released. Linear regression can be used to describe the relationship between TRP load and water discharge. About 80% of the total phosphorus (TP) in the study stream was soluble and more than 70% of the P release occurred in storm events, indicating that traditional buffer strips with widths of 15-20 m might not be efficient for P immobilization. The P concentrations were affected by antecedent weather conditions and highest concentrations occurred during storm events following prolonged drought periods. The water extractable phosphorus (WEP) contents in the soil were significantly higher below windrow/brash material than in brash-free areas, and whole-tree harvesting should be studied as one of the means to decrease P export from blanket peats.
机译:这项研究的目的是调查磷在高地泥炭流域收获34岁的黑松树所致的接收水中的释放磷。研究场地位于25.3公顷(ha)区域内,被一条溪流排干,该溪流主要来自集水沟,来自犁过的犁沟,并直接排入爱尔兰梅奥市Burrishoole的鲑鱼Shrahrevagh河。研究地点分为两个部分:上游部分完好无损,下游部分是在遵循森林准则后于2005年秋季初收获的。实施了良好的管理规范,例如正确使用了草皮垫以及仅在干燥天气下进行收获。建立了两个仪器站,一个位于清除区域的上游(美国),另一个位于下游(DS)。这两个站的P浓度测量始于2005年5月,即开始收获前两个月。 DS站的日平均P浓度从清除前的总活性磷(TRP)的约6 micro g L -1 增加到429 micro g L -1 在2006年8月。到2009年10月,即清除后的第四年,DS站的P浓度已恢复到清除前的水平。收获后的前三年,从收获的流域向接收水释放了多达5.15 kg ha -1 的TRP。仅在第二年,就释放了2.3千克ha -1 的TRP。线性回归可用于描述TRP负荷与排水量之间的关系。研究流中约80%的总磷(TP)是可溶的,并且超过70%的P释放发生在暴风雨事件中,这表明宽度为15-20 m的传统缓冲带可能无法有效地固定P。磷的浓度受前期天气条件的影响,在长期干旱后的暴风雨事件中磷的浓度最高。土壤中的水可提取磷(WEP)含量比无bra的地区要高得多,比无bra地区要高,应研究整树采伐作为减少毯子泥炭中磷输出的一种方法。

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