OR/15/038 Monitoring
Gareth Farr (with contributions from Luz Ramos Cabrera). 2015. Nedern Brook Wetland SSSI Phase 1 hydrological monitoring. British Geological Survey Internal Report, OR/15/038. |
Monthly monitoring visits were undertaken between October 2014 and May 2015. Observations on the brook and the wetlands were made from the ‘Cwm’ in the north to its mouth in the Bristol Channel (Figure 2). Information on the location of key groundwater discharge areas was also collected. Detailed survey elevations were collected from repeatable locations near all water level data loggers in both the dipwells and the stilling wells in the brook (see Appendix 2 - Elevation survey data).
Surface water
Spot flow gauging was undertaken by Paul Griffiths, John Evans, Ross Adamson and Kris Tomsett staff from Natural Resources Wales’ Hydrometry & Telemetry Team, South East Wales. Spot flow gauging was undertaken at three sites on the Nedern Brook (Table 1, Figure 2, Figure 3) during low, medium and high flow conditions using a Sontek M9 ADCP (Figure 1). The sites represent inflow to the top of the SSSI (‘Nedern Brook at Tyne Cottages’) and outflow (Nedern DS and Nedern Castle Car Park).
Stilling wells were installed at the start of the project at two locations called Nedern Brook US and DS (Figure 2). Later on, in January 2015, an additional stilling well was installed further up the Nedern Brook underneath the bridge near Tyne Cottages to complement the spot gauging and to allow for stage-discharge relationships to be calculated in the future. Due to this stilling well being installed part way through the project the data from this site only covers part of the study period.
Surface water gauging was also attempted within the SSSI boundary at the small tributary (ST 48654 89452) and at the ‘Nedern US’ monitoring point (ST 48427 89489). However both were ruled out for further monitoring due to access. Both sites can be entirely flooded and conversely experience extremely low flow velocities during dry periods.
Visual observations of surface water flow were undertaken during the monthly monitoring visits, starting upstream on the Castrogi Brook ‘Cwm’ where the surface water is known to sink and has been traced to the Great Spring (Drew et al 1970, Clarke & Aldous, 1987[1] and Lawrence et al, 2013[2]). The Nedern Brook was observed throughout the SSSI section and then south through the industrial estate to the outflow.
Groundwater
Groundwater levels in the bedrock Carboniferous Limestone aquifer are monitored at boreholes installed by Natural Resources Wales at Caldicot Castle Car Park, Tyne Cottages, Five Lanes and Dewstone Road (Figure 2, Table 1, Appendix 4 - Borehole logs). Each borehole is instrumented with a vented pressure transducer recording changes in groundwater levels every 30 minutes with the data corrected to maOD. To complement the groundwater level data within the Carboniferous Limestone aquifer a non-vented Solinst Level logger™ with a 10 m range was installed in Piezometer P3 monitoring the shallow clays and peats within the wetland (Figure 2, Figure 3). It was not possible to dip P3 during the majority of the study as it was fully submerged by flood waters.
Precipitation
Precipitation data on a 15 minute basis was provided by Natural Resources Wales from weather stations at Collister Pill and Llanvaches, the data was then converted to daily total (mm).
Elevation survey and flood map
Dipwells, piezometers and stilling wells were surveyed to maOD using a Leica Smart Rover CS10/CS15 & GS 14 Sensors, capable of surveying elevation to an accuracy of <5 cm. Flood levels of the Nedern Brook were also surveyed on a monthly basis to allow for corrections of the water level data loggers installed within the flooded area (Nedern US, Nedern P3 and to a lesser extent Nedern DS). The survey data is included in Appendix 2 - Elevation survey data. The water level data and survey data were combined, and the maximum and mean flood values were input into ArcView, with the 1 m LIDAR data for the area. The LIDAR was ‘flooded’ in order to create two flood maps.
Water chemistry
Water chemistry sampling was undertaken in Dec 2015, with samples collected from the Nedern Brook and flood waters. The samples were analysed at the Environment Agency National Labs. Due to the flood levels it was not possible to sample groundwater directly from the Piezometers, or from discharge from the Whirly Holes, both of which were under water. Field observations of temperature, pH and electrical conductivity were collected during site visits on the 18th December 2014 and 16th January 2015 using a Hannah HI98312 hand held temperature and electrical conductivity meter with an accuracy of ± 2% for electrical conductivity and ± .5°C for temperature. Results for the field parameters are presented in Appendix 3 - Field water chemistry, and the ion analysis in Table 3.
General observations
During each site visit a sketch map was made of the extent of flooding (Appendix 5 - Field maps with sketches of flood extent). Observations on the flow of water in the Nedern Brook were made from the Castrogi Brook ‘Cwm’ monitoring point upstream to the outflow into the Bristol Channel.
Monitoring Point | Source | Type | Method | Depth (mbgl) | Response Zone (mbgl) | Frequency | Easting | Northing |
Dipwell DW2 | Groundwater | Dipwell | Manual Dip | 0.86 | 0–0.86 | 60 minutes | 348674 | 189360 |
Piezo P3 | Groundwater | Piezometer | Data logger | 1.78 | 1.815–2.115 | Monthly | 348675 | 189361 |
Dipwell D1 | Groundwater | Dipwell | Manual Dip | 0.76 | 0–0.76 | Monthly | 348638 | 189368 |
Piezo P1a | Groundwater | Piezometer | Manual Dip | 2.265 | 1.965–2.265 | Monthly | 348638 | 189368 |
Piezo P1 | Groundwater | Piezometer | Manual Dip | 3.07 | 2.77–3.07 | Monthly | 348638 | 189369 |
Barologger | Atmospheric Pressure | Barologger | Data logger | n/a | n/a | 30 Minutes | 348685 | 189307 |
Nedern US | Surface water | Surface water | Data logger | n/a | n/a | 30 Minutes | 348430 | 189486 |
Lower Hole Whirly | Groundwater | Spring/rising | Visual | n/a | n/a | Monthly | 348163 | 189925 |
Upper Hole Whirly | Groundwater | Spring/rising | Visual | n/a | n/a | Monthly | 347354 | 189943 |
Caldicot Country Park BH | Groundwater | NRW Observation Borehole | Data logger | 70 | 56–70 | 30 Minutes | 348900 | 188200 |
Five Lanes BH | Groundwater | NRW Observation Borehole | Data logger | 55 | 22–55 | 30 Minutes | 344800 | 190900 |
Tyne Cottage BH | Groundwater | NRW Observation Borehole | Data logger | 65 | 17–65 | 30 Minutes | 347200 | 189900 |
Dewston Road BH | Groundwater | NRW Observation Borehole | Data logger | 60 | 5.1–60 | 30 Minutes | 347100 | 188500 |
Great Spring | Groundwater | Abstraction Monitored by Network Rail | Abstraction Monitored by Network Rail | n/a | Daily | 350721 | 187374 | |
Nedern at Tyne Cottages | Surface water | Nedern Brook | NRW Spot Gauging and Data logger | n/a | n/a | 30 Minutes | 347195 | 189997 |
Nedern DS | Surface water | Nedern Brook | NRW Spot Gauging and Data logger | n/a | n/a | 30 Minutes | 348674 | 188591 |
Nedern Castle Car Park | Surface water | Nedern Brook | NRW Spot Gauging and Data logger | n/a | n/a | 30 Minutes | 348771 | 188369 |
Nedern Outflow | Surface water | Nedern Brook | Visual | n/a | n/a | Monthly | 348985 | 187258 |
Castrogi Brook Sink at the ‘Cwm’ | Surface water | Castrogi Brook | Visual | n/a | n/a | Monthly | 345879 | 192739 |
References
- ↑ CLARKE, L, and ALDOUS, P J. 1987. Hydrogeological investigations in the Chepstow Block, Gwent: Summary report. WRc Environment for the Welsh Office: restricted report CO1469-M/EV 8390.
- ↑ LAWRENCE, D J D, FARR, G J, WHITBREAD, K, and KENDALL, R. 2013. The geology, hydrogeology and vulnerability of the Great Spring Source Protection Zone. Commissioned Report CF/12/024 for Environment Agency Wales. Confidential Report.