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Complexities in the stream temperature regime of a small mixed-use watershed, Blacksburg, VA

机译:弗吉尼亚州布莱克斯堡一个小型综合利用流域的河流温度状况的复杂性

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Stream temperature is a vital characteristic of stream ecosystems and has a strong control on chemical and biological processes. Water temperatures, particularly in small streams with low flows, can be affected by riparian vegetation and land cover. We designed a study using in situ temperature sensors to examine the annual thermal regime of Stroubles Creek, a small stream in Blacksburg, VA, across three land cover regions; urbanized, agricultural, and forested. During the warm sampling period, mean stream temperatures were: 17.8 degrees C (+/- 3.5 degrees C) in the urban reaches; 20.0 degrees C (+/- 3.0.C) in the agricultural region; and 20.4 degrees C (+/- 3.3 degrees C) in the forested area. Cold period daily stream temperatures were: 10.54 degrees C (+/- 3.1 degrees C) in the urban reaches; 8.5 degrees C (+/- 4.0 degrees C) in the agricultural region; and 7.7 degrees C (+/- 4.1 degrees C) in the forested area. Linear regression analyses suggest that weekly mean stream and air temperatures have a significant linear relationship throughout the Stroubles Creek watershed, regardless of land cover or period. During the warm period, mean stream temperatures increased by 5.9 degrees C downstream along 9 km of the main stem from the headwater spring to the forested outflow as groundwater was exposed to air temperatures and environmental heat fluxes. Local cooling of stream water occurred in agricultural and forested reaches at sites with higher canopy, and possibly strong stream water-groundwater interactions. Stream temperatures decreased during the cold period by 4.5 degrees C from headwaters to outflow, with groundwater inputs producing areas of local warming. Although the stream water-groundwater relationship of Stroubles Creek was not quantified in this study, analyses suggest that groundwater and hyporheic flow, along with riparian vegetation and canopy cover, could be controls on stream temperatures. Identifying sources of cooling for stream temperatures in the Stroubles Creek watershed, such as riparian vegetation and groundwater, could be useful for restoring the natural thermal regime, which has important implications for restoration of water quality and aquatic organism diversity in this mixed land use watershed. (C) 2014 Elsevier B.V. All rights reserved.
机译:溪流温度是溪流生态系统的重要特征,对化学和生物过程具有很强的控制力。水温,特别是在流量低的小溪中,会受到河岸植被和土地覆盖的影响。我们设计了一项使用原位温度传感器的研究,研究了弗吉尼亚州布莱克斯堡的一条小溪Stroubles Creek在三个土地覆盖区域的年度热状况。城市化,农业化和森林化。在温暖的采样期间,平均溪流温度为:城市河段17.8摄氏度(+/- 3.5摄氏度);农业地区20.0摄氏度(+/- 3.0.C);在林区中为20.4摄氏度(+/- 3.3摄氏度)。寒冷时期的每日溪流温度为:市区河段10.54摄氏度(+/- 3.1摄氏度);农业地区为8.5摄氏度(+/- 4.0摄氏度);林区为7.7摄氏度(+/- 4.1摄氏度)。线性回归分析表明,在整个Stroubles Creek流域,每周平均流量和气温均具有显着的线性关系,而与土地覆盖或时期无关。在温暖期,由于地下水暴露在空气温度和环境热通量的作用下,从上游水源到森林流出处,沿着主干的9 km,下游的平均河流温度升高了5.9°C。农业和森林河段的冠层较高,且溪流水与地下水的相互作用可能很强,因此溪流水局部冷却。在寒冷时期,河源温度从源头到出水下降了4.5摄氏度,而地下水输入使局部变暖。尽管斯特劳布尔斯溪的溪流水与地下水的关系在本研究中没有得到量化,但分析表明,地下水和低渗流以及河岸植被和冠层覆盖可以控制溪流温度。确定斯特劳布尔斯河流域的河流温度的冷却源,例如河岸植被和地下水,对于恢复自然热力状况可能是有用的,这对于恢复这一混合土地利用流域的水质和水生生物多样性具有重要意义。 (C)2014 Elsevier B.V.保留所有权利。

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