Hydro G Final report - Kildare.ie
Hydro G Final report - Kildare.ie
Hydro G Final report - Kildare.ie
Create successful ePaper yourself
Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.
<strong>Hydro</strong>-G FINAL REPORT<br />
Mr. Simon Wallace<br />
Senior Executive Parks Superintendent<br />
<strong>Kildare</strong> County Council<br />
Dear Simon<br />
Re: Preliminary <strong>report</strong> on the hydrological investigation of Leixlip Spa, Co. <strong>Kildare</strong><br />
Our Ref: 07136_Leixlip Spa_D07<br />
17 th Dec 2007<br />
This <strong>report</strong> has been prepared by <strong>Hydro</strong>-G to inform <strong>Kildare</strong> County Council on a progress of the initial assessment of<br />
hydrological requirements of the Leixlip Spa SAC (code 001398). The <strong>report</strong> outlines site visits and f<strong>ie</strong>ld work<br />
investigations carr<strong>ie</strong>d out to date. An interpretation of results will be provided at a later date when the results of the<br />
sampling regime are processed and hydrochemical results returned from the laboratory.<br />
In November 2007 <strong>Hydro</strong>-G was approached by <strong>Kildare</strong> County Council to undertake an investigation on the<br />
hydrological regime of Leixlip Spa, Co. <strong>Kildare</strong>. The site is located in Leixlip village, along the western side of the Royal<br />
Canal and between a regional road R 148 and the Rye River. The western boundary of the site is adjacent to the Intel<br />
factory. The ecological features of the site comprise a wide range of protected spec<strong>ie</strong>s and habitats including<br />
petryfying tufa springs (SAC Site Synopsis 001398) and alkaline fen habitat. These habitats rely on a stable discharge<br />
of groundwater saturated with calcite carbonate. Although it is well understood that the rare habitats and spec<strong>ie</strong>s<br />
found at the Leixlip Spa are dependent on the hydrological regime of the site, the latter is not well understood and very<br />
limited data on the site hydrology exist at present. Neither quantitative nor qualitative data are available.<br />
The site is located on a steep limestone ridge which is a remnant of a quarry created in the late 18 th century. The most<br />
prominent hydrological feature of the site is a warm spring located at the entrance to the site, east of the public<br />
pathway leading into the site. The spring was discovered in late 18 th century and merits attention due to the relatively<br />
high temperature and iron content in the water that it discharges.<br />
To date, <strong>Hydro</strong>-G conducted two site visits the first on the 2 nd and latter on the 10 th of December 2007. The purpose of<br />
these visits was to meet with ecologists involved in works on the site, namely Mr Declan Doogue, Mr Brendan<br />
O’Hanrahan and Ms Evelyn Moorkens. These site meetings facilitated greater understanding of the site’s ecology and<br />
its hydrological needs for sustaining a healthy habitat. It was established during these visits that ecological features<br />
have changed throughout the past 20-30 years of ecological monitoring. Specifically, the following two issues had<br />
been raised:<br />
• Drying of the upper zone, west of the gravel pathway. Historically this area provided a suitable habitat for wet<br />
loving grasses and marsh orchids. However Mr Declan Doogue <strong>report</strong>ed this area had not been wet in<br />
winters within the past 20 years which led to loss of this habitat.<br />
Project No.: 07_136 -25-<br />
Leixlip Spa