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作为一种保存技术对冷冻用于分析地表水样品中溶解有机碳、氮和磷的评估。

An evaluation of freezing as a preservation technique for analyzing dissolved organic C, N and P in surface water samples.

作者信息

Fellman Jason B, D'Amore David V, Hood Eran

机构信息

Institute of Arctic Biology, University of Alaska Fairbanks, Fairbanks, AK 99775, USA.

出版信息

Sci Total Environ. 2008 Mar 25;392(2-3):305-12. doi: 10.1016/j.scitotenv.2007.11.027. Epub 2007 Dec 31.

Abstract

Techniques for preserving surface water samples are recently in demand because of the increased interest in quantifying dissolved organic matter (DOM) in surface waters and the frequent collection of samples in remote locations. Freezing is a common technique employed by many researchers for preserving surface water samples; however, there has been little evaluation of the effects of freezing on DOM concentrations. Ten streams were sampled in southeast Alaska with a range of dissolved organic carbon (DOC) concentrations (1.5 to 39 mg C L(-1)) to evaluate the influence of freezing (flash and standard freeze) and filter pore size (0.2 and 0.7 mum nominal pore size) on dissolved organic C, N and P concentrations. We report a significant decrease in DOC (p<0.005) and total dissolved P (p<0.005) concentrations when streamwater samples were frozen, whereas concentrations of dissolved organic N did not significantly decrease after freezing (p=0.06). We further show that when surface water samples were frozen, there was a decrease in the specific ultraviolet absorbance (SUVA) of DOC that is particularly evident with high concentrations of DOC. This finding suggests that spectroscopic properties of DOC have the potential to be used as indicators of whether surface water samples can be frozen. Our results lead us to recommend that surface water samples with high DOC concentrations (>5 mg C L(-1)) and/or samples with high SUVA values (>3.5-4 L mg-C(-1) m(-1)) should be analyzed immediately and not frozen.

摘要

由于对地表水中溶解有机物(DOM)进行量化的兴趣增加以及在偏远地区频繁采集样本,目前对地表水样本保存技术的需求很大。冷冻是许多研究人员用于保存地表水样本的常用技术;然而,对于冷冻对DOM浓度的影响,几乎没有相关评估。在阿拉斯加东南部对10条溪流进行了采样,这些溪流的溶解有机碳(DOC)浓度范围为1.5至39毫克碳/升,以评估冷冻(快速冷冻和标准冷冻)和滤膜孔径(标称孔径0.2和0.7微米)对溶解有机碳、氮和磷浓度的影响。我们报告称,当溪水样本被冷冻时,DOC(p<0.005)和总溶解磷(p<0.005)浓度显著下降,而溶解有机氮浓度在冷冻后没有显著下降(p=0.06)。我们进一步表明,当地表水样本被冷冻时,DOC的特定紫外吸光度(SUVA)会下降,在高浓度DOC时尤其明显。这一发现表明,DOC的光谱特性有可能用作地表水样本是否可冷冻的指标。我们的结果促使我们建议,DOC浓度高(>5毫克碳/升)和/或SUVA值高(>3.5 - 4升/毫克碳·米)的地表水样本应立即进行分析,而不要冷冻。

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