<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "https://jats.nlm.nih.gov/nlm-dtd/publishing/3.0/journalpublishing3.dtd">
<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article" dtd-version="3.0" xml:lang="en">
<front>
<journal-meta>
<journal-id journal-id-type="publisher">HESS</journal-id>
<journal-title-group>
<journal-title>Hydrology and Earth System Sciences</journal-title>
<abbrev-journal-title abbrev-type="publisher">HESS</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Hydrol. Earth Syst. Sci.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1607-7938</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/hess-1-197-1997</article-id>
<title-group>
<article-title>Acidification in Three Lake District Tarns: Historical Iong term trends and modelled future behaviour under changing sulphate and nitrate deposition</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Whitchead</surname>
<given-names>P. G.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Barlow</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Haworth</surname>
<given-names>E. Y.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Adamson</surname>
<given-names>J. K.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Aquatic Environments Research Centre, Dept. of Geography, University of Reading, Whiteknights, Reading, RG6 2 AB.</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Dept. Civil Engineering, Imperial College, University of London, Exhibition Road, London W1.</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Institute of Freshwater Ecology, Ferry House, Ambleside, Cumbria, LA22 OLP</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Institute of Terrestrial Ecology, Merlewood Research Station, Grange over Sands, Cumbria, LA11 6JU</addr-line>
</aff>
<pub-date pub-type="epub">
<day>31</day>
<month>03</month>
<year>1997</year>
</pub-date>
<volume>1</volume>
<issue>1</issue>
<fpage>197</fpage>
<lpage>204</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 1997 P. G. Whitchead et al.</copyright-statement>
<copyright-year>1997</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 Generic License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by-nc-sa/2.5/">https://creativecommons.org/licenses/by-nc-sa/2.5/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://hess.copernicus.org/articles/1/197/1997/hess-1-197-1997.html">This article is available from https://hess.copernicus.org/articles/1/197/1997/hess-1-197-1997.html</self-uri>
<self-uri xlink:href="https://hess.copernicus.org/articles/1/197/1997/hess-1-197-1997.pdf">The full text article is available as a PDF file from https://hess.copernicus.org/articles/1/197/1997/hess-1-197-1997.pdf</self-uri>
<abstract>
<p>Three upland Lake District Tarns, Scoat, Greendale
and Burnmoor, have been evaluated using MAGIC (Model of Acidification
of Groundwater In Catchments) to reconstruct past, present and future chemical behaviour.
The modelled historical changes in acidity are compared with
palaeoecological estimation of pH to demonstrate model validity. Chemistry
as simulated for all anions and cations and two of the three lakes are
shown to have undergone significant acidification. The effects of changing
atmospheric pollution levels on lake chemistry is evaluated and 80-90% sulphur
reduction levels are required to achieve zero alkalinity. The impacts of
increased nitrogen deposition are assessed and are shown to further delay
reversibility.</p>
</abstract>
<counts><page-count count="8"/></counts>
</article-meta>
</front>
<body/>
<back>
</back>
</article>