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MERCURY FLUX MEASUREMENTS OVER AIR AND WATER IN KEJIMKUJIK NATIONAL PARK, NOVA SCOTIA

机译:新斯科舍省凯吉姆库克国家公园空气和水上的汞通量测量

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Mercury flux measurements were conducted at two lakes and three soil sites in Kejimkujik National Park, located in the eastern Canadian province of Nova Scotia. One of the lakes had high levels of both mercury and Dissolved Organic Carbon (DOC). Two of the soil sites were located under the forest canopy, while the other was in a small clearing surrounded by forest. Flux measure- ments were performed using the dynamic chamber method. Mercury concentrations in the air were measured with a TEKRAN mercury analyzer. Mercury fluxes over the two lakes were most strongly correlated with solar radiation, although the flux was also significantly correlated with water temper- ature, air temperature, and negatively correlated with relative humidity. The flux from the high DOC lake (Big Dam West) was especially high when the conditions were both sunny and windy (wind speed greater than 1.3 m s~(-1)) and the average flux measured was 5.4 ng m~(-2) h~(-1). The mercury flux from this lake was well parameterized in terms of a simple expression involving solar radiation and a nonlinear dependence on wind speed. The flux measured from the low DOC lake (North Cranberry) tended to be lower than from the high DOC lake. The average flux measured was 1.1 ng m~(-2) h~(-1). but was again strongly correlated with solar radiation. The flux was low during windy conditions in the absence of sunlight, suggesting that wind enhances mercury evasion from lakes only in the presence of solar radiation. Mercury fluxes measured over the soil sites tended to be smaller than those over water (a range of-1. 4-4.3 ng m~(-2) h~(-1). At one of the forest sites, mercury flux was very strongly correlated with 0.5 cm soil temperature, and this dependence was well described by an Arrhenius-type expression with an activation energy of 14.6 kcal~(-1) mole, quite close to the heat of vaporization of mercury (14.5 kcal~(-1) mol~(-1) at 20℃). At the clearing, where there was direct exposure to the sun, the mercury flux was most strongly correlated with solar radiation.
机译:在加拿大东部新斯科舍省的Kejimkujik国家公园的两个湖泊和三个土壤场所进行了汞通量测量。其中一个湖泊的汞和溶解有机碳(DOC)含量很高。其中两个土壤场位于林冠下,另一个位于森林包围的小片空地中。通量的测量是使用动态室法进行的。用TEKRAN汞分析仪测量空气中的汞浓度。尽管两个通量的汞通量还与水温,空气温度显着相关,而与相对湿度负相关,但两个湖泊中的汞通量与太阳辐射的相关性最强。在晴天和大风天气(风速大于1.3 ms〜(-1))下,高DOC湖(大坝西)的通量特别高,测得的平均通量为5.4 ng m〜(-2)。 h〜(-1)。根据涉及太阳辐射的简单表达式以及对风速的非线性依赖性,可以很好地参数化来自该湖的汞通量。低DOC湖(北蔓越莓)测得的通量往往比高DOC湖的通量要低。测得的平均通量为1.1 ng m〜(-2)h〜(-1)。但是又与太阳辐射密切相关。在有风的条件下,在没有阳光的情况下,通量很低,这表明只有在有太阳辐射的情况下,风才能促进汞从湖泊中逸出。在土壤位点测得的汞通量往往比在水位更小(范围为-1。4-4.3 ng m〜(-2)h〜(-1)。在其中一个森林位点,汞通量非常高。与土壤温度0.5 cm密切相关,这种依赖性可以通过Arrhenius型表达式很好地描述,其活化能为14.6 kcal〜(-1)摩尔,非常接近汞的汽化热(14.5 kcal〜(-1 )(在20℃时为mol〜(-1))。在晴天,直接暴露在阳光下,汞通量与太阳辐射密切相关。

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