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首页> 外文期刊>Environmental geology and water sciences >Daytime deposition and nighttime dissolution of calcium carbonate controlled by submerged plants in a karst spring-fed pool: insights from high time-resolution monitoring of physico-chemistry of water
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Daytime deposition and nighttime dissolution of calcium carbonate controlled by submerged plants in a karst spring-fed pool: insights from high time-resolution monitoring of physico-chemistry of water

机译:岩溶泉水池中淹没植物控制的碳酸钙在白天的沉积和夜间溶解:对水的物理化学的高分辨率监测

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Water temperature, dissolved oxygen (DO), pH, and specific conductivity (spc) were measured in a time interval of 15 min in a karst spring and the spring-fed pool with flourishing submerged plants in Guilin, SW China under dry weather for periods of 2 days. Measurements allowed calculation of calcium and bicarbonate concentrations ([Ca~(2+))] and [HCO_3~-]), and thus CO_2 partial pressure (P_(CO_2)) and saturation index of calcite (SIc). Results show that there were not any diurnal variations in the physico-chemical parameters of the water for the spring. However, during daytime periods, pool water PcO_2 decreased to far less than the spring water in a few hours, pH and SIc increased to greater than the spring, and [Ca~(2+)] and [HCOi] decreased to less than the spring. During nighttime periods, pool water P_(CO_2) returned to or even increased to greater than the spring, pH and SIc decreased to less than the spring, and [Ca~(2+)] and [HCO_3~-] increased to greater than the spring. The decrease in [Ca~(2+)] and [HCO_3~-] to less than the spring during daytime periods implies daytime deposition of calcium carbonate, while the increase in [Ca~(2+)] and [HCO_3~-] to greater than the spring during nighttime periods implies nighttime dissolution of calcium carbonate. The direction of the observed changes depended essentially on the illumination, indicating that daytime photosynthetic and nighttime respiratory activities in the pool aquatic plant ecosystem, which were further evidenced by the increase and decrease in DO during daytime and nighttime periods respectively, were the main processes involved. The large variations of the components of the carbonate system imply considerable changes of the capacities of CO_2 and O_2 in water. The finding has implications for water sampling strategy in slow-flowing karst streams and other similar environments with stagnant water bodies such as estuaries, lakes, reservoirs, and wetlands, where aquatic plant ecosystem may flourish.
机译:在喀斯特泉水和泉水池中,每15分钟测量一次水温,溶解氧(DO),pH和比电导率(spc)。 2天。通过测量可以计算出钙和碳酸氢盐的浓度([Ca〜(2+))]和[HCO_3〜-],从而计算出CO_2分压(P_(CO_2))和方解石饱和指数(SIc)。结果表明,春季水的理化参数没有任何昼夜变化。然而,在白天,池水PcO_2在数小时内降至远低于泉水,pH和SIc升高至高于泉水,[Ca〜(2+)]和[HCOi]降至低于泉水。弹簧。在夜间,池水P_(CO_2)返回到甚至高于春季,pH和SIc降至春季以下,[Ca〜(2+)]和[HCO_3〜-]增加至高于春季。春天。在白天,[Ca〜(2+)]和[HCO_3〜-]的减少小于春季,意味着碳酸钙在白天的沉积,而[Ca〜(2+)]和[HCO_3〜-]的增加。夜间高于春季则意味着碳酸钙在夜间溶解。观测到的变化方向主要取决于光照,表明池水生植物生态系统中白天的光合作用和夜间呼吸活动,分别由白天和夜间DO的增加和减少进一步证明,是所涉及的主要过程。 。碳酸盐体系中各组分的较大变化意味着水中CO_2和O_2的容量发生了显着变化。这一发现对缓慢流动的岩溶溪流和其他类似水体停滞的类似环境(如河口,湖泊,水库和湿地)的水采样策略具有重要意义,在这些环境中水生植物生态系统可能会蓬勃发展。

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