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Optical characteristics of shallow lakes from the Pampa and Patagonia regions of Argentina

机译:阿根廷潘帕和巴塔哥尼亚地区浅湖的光学特征

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Sixteen Argentinean shallow lakes from the Pampa plains and the Patagonian steppe were characterized using optical properties and water-quality parameters. In this set of lakes a wide range in water transparency descriptors was observed [broadband vertical attenuation coefficient (kd PAR) varied from 0.40 to 47m1, Secchi disk depth (Sd) from 0.07 to 12.00m, and nephelometric turbidity (tn) from 0.50 to 103.70 NTU (710.00)]. Among Pampean lakes, highly turbid lakes presented significant higher kd PAR values (413m1) than clear-vegetated ones (<10m1), though all Patagonian lakes showed significant lower light attenuation (kd PAR<2.5m1). Our estimations of light scattering were supported by the significant relationship found between tn and Effler and Auer’s scattering coefficient estimate (best). Allowing for lakes with tno80 NTU, we obtained a significant linear regression with a slope close to the unity. However, when values of tn were higher than 80 NTU, no clear relationship was observed between tn and best. Although we found significant relationships between kd, Sd and tn over the whole range of underwater light scenarios, we noticed some disparities between Sd, tn and light attenuation in lakes with certain optical characteristics. Considering the whole data set, including clear and turbid lakes, as much as 92% of the variation observed in kd PAR could be explained by a regression model including absorption of chromophoric dissolved organic matter (CDOM) and tn. Our results showed that a suitable and practical method to estimate light attenuation could be the use of empirical models based on absorption coefficients and tn measured with bench top instruments. The direct measurement of paired values of Sd and tn, in addition with main absorbing components are a useful and precise way of describing underwater light availability and optical regimes. The latter, combined with occasional in situ measurements of kd would permit the development of highly accurate lake-specific models of light attenuation.
机译:利用光学特性和水质参数对来自潘帕平原和巴塔哥尼亚草原的十六个阿根廷浅湖进行了表征。在这组湖泊中,观察到了广泛的水透明性描述[宽带垂直衰减系数(kd PAR)从0.40到47m1不等,Secchi盘深度(Sd)从0.07到12.00m不等,浊度浊度(tn)从0.50到0.50不等。 103.70 NTU(710.00)]。在Pampean湖泊中,高浊度湖泊的kd PAR值(413m1)明显高于无植被湖泊(<10m1),尽管所有巴塔哥尼亚湖泊均表现出明显较低的光衰减(kd PAR <2.5m1)。 tn和Effler之间的显着关系以及Auer的散射系数估计(最佳)支持了我们对光散射的估计。考虑到tno80 NTU的湖泊,我们获得了显着的线性回归,其斜率接近于1。但是,当tn的值高于80 NTU时,tn与最佳值之间没有明显的关系。尽管我们发现在整个水下光场景中kd,Sd和tn之间存在显着关系,但我们注意到在具有某些光学特征的湖泊中,Sd,tn和光衰减之间存在一些差异。考虑到整个数据集,包括清澈和浑浊的湖泊,在kd PAR中观察到的多达92%的变化可以通过回归模型来解释,该模型包括发色溶解性有机物(CDOM)和tn的吸收。我们的结果表明,一种合适的,实用的估算光衰减的方法可能是使用基于吸收系数和台式仪器测得的tn的经验模型。除主要吸收成分外,直接测量Sd和tn的配对值是描述水下光可用性和光学状态的有用且精确的方法。后者与偶然的kd原位测量相结合,将可以开发出高度精确的特定于湖的光衰减模型。

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