在过去的四千年里,德国东北部低地河流的营养物质浓度是如何变化的?-对洪泛区沉积物的古湖泊学研究

IF 0.6 Q4 GEOSCIENCES, MULTIDISCIPLINARY Studia Quaternaria Pub Date : 2004-01-01 DOI:10.18452/9393
I. Schonfelder, E. Christian, W. Steinberg
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引用次数: 13

摘要

本文重点研究了两条低地河流(德国哈维尔河、施普雷河、勃兰登堡州)古河漫滩沉积物和河流沉积物作为定量古湖泊重建档案和未来河流管理策略的潜在基础的可行性。所提出的结果为区分河流的自然富营养化和人工富营养化提供了一种方法。利用勃兰登堡84个湖泊和河流遗址的沿海硅藻组合有效传递函数以及总磷(TP)和总无机氮(TN)推测了近4000年来哈维尔河和施普雷河的营养变化。在Platkow附近的施普雷河(River Spree),硅藻化石表明,在1300 ~ 1850 AD (TP: 36 μg dm, TN: 1000 μg dm)期间,ttn和TN浓度处于中等富营养化水平。在此期间,人类对施普雷河营养状况的影响或多或少是间接的,因为森林砍伐导致汇水径流量增加。在第2条低地河流哈维尔河下游,硅藻推断的tp浓度在亚北纬晚期(公元前2000 ~ 500年)为80 μg dm。这意味着这条河的天然硅藻群是富营养化的;即使在没有集约土地利用的时代,也没有出现中营养状况。此外,化石硅藻区系在夏季显示出潜在的氮限制(直到公元1400年:TN 1600 ~ 1700 μg dm)。自大约800年前以来,人类活动对哈维尔河的富营养化影响就可以检测到。硅藻推断的氮磷关系突出了研究区内富营养化历史的不同趋势。在没有人类活动的情况下,这两种营养成分的比例相对恒定。在过去的1000年里,汇水区的人为变化导致了TN/TP比率的下降,藻类群落的变化,例如在过去的几十年里,令人讨厌的蓝藻华的增加。
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How did the nutrient concentrations change in northeastern German lowland rivers during the last four millennia? - a paleolimnological study of floodplain sediments
This study focuses on the feasibility of floodplain sediments and fluvial sediments in paleomeanders and ox-bows of two lowland rivers (River Havel, River Spree, Brandenburg State, Germany) as archives for quantitative paleolimnological reconstructions and potential basis of future river management strategies. The results presented provide a mean to differentiate between the natural and cultural eutrophication of rivers. Available transfer functions of littoral diatom assemblages in 84 Brandenburg lakes and river sites, and total phosphorus (TP) and total inorganic nitrogen (TN) were used to infer nutrient changes in the Rivers Havel and Spree since the last 4,000 years. In the River Spree near Platkow, fossil diatoms indicated moderate eutrophic TPand TN-concentrations between 1300 and 1850 AD (TP: 36 μg dm, TN: 1,000 μg dm). During this time period, the human impact on the nutrient status of the River Spree was more or less indirect via increases of runoff from the catchment as a result of deforestation. In the second lowland river, the lower River Havel, diatom inferred TP-concentrations were 80 μg dm in the late Subboreal (2,000 to 500 BC). That means that the natural diatom flora of this river was eutrophic; mesotrophic conditions even in times without intensive land use did not occur. Furthermore, the fossil diatom flora revealed a potential nitrogen limitation during summer times (till 1400 AD: TN 1,600 to 1,700 μg dm). Anthropogenic eutrophication impact on the River Havel can be detected since approximately 800 year ago. The diatom-inferred nitrogen/phosphorus-relation highlighted different trends in eutrophication history within the study area. Without human activities the ratio of both nutrient components was relatively constant. Anthropogenic changes in the catchment area led to a declining TN/TP ratio in the last 1,000 years with changes in algal communities, such as increases of nuisance cyanobacteria blooms in the last decades.
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来源期刊
Studia Quaternaria
Studia Quaternaria GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
1.40
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期刊介绍: Studia Quaternaria is designed to publish scientific works concerning the Quaternary, on local, regional and global scale. Studia Quaternaria is interested in all fields of research dealing with stratigraphy and reconstruction of the past environments, including palaeogeography, palaeoecology, palaeoclimatology, palaeohydrology etc. The journal is also open to studies of natural environmental processes, and to recognition of mechanisms involved in the dynamics of our environment. The clue is that the Quaternary is still ongoing and vivid, and understanding of its past and present development support each other.
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