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Appendix 5 Defining Reference Conditions for Chalk Stream and Fenland Natural Channels
Appendix 5 Defining reference conditions for chalk stream and Fenland natural channels Chalk stream geomorphology is poorly understood, and under-researched. What studies exist appear to confirm that the majority of UK and European chalk streams have been modified in form and hydraulics by a long history of river management (Sear and others 1999, WRc 2000). The overriding control these modifications exert on the geomorphology and processes operating within the channel, make it difficult to establish what features and physical habitat diversity a natural, unmodified chalk stream should display. In the absence of semi-natural chalk stream habitats from which reference conditions can be determined, the Water Framework Directive specifies the use of palaeoecological information (Logan and Furze 2002). However much of this research is focussed on interpretations of human activity or climatic reconstruction rather than on the specific determination of river form and associated habitats (Davies and Griffiths 2005; French and Lewis 2002). Despite this, it is possible to reconstruct some information of relevance to characterising the floodplain habitats associated with relatively undisturbed chalk streams and rivers. French and others 2005 report a complex suite of landscape changes in the Dry valley and upper reaches of a chalk stream in Dorset. Their results suggest the presence of a relatively wide shallow low sinuosity meandering channel throughout the Holocene into the early historic period, between 30 - 50m in width and 1.5 – 3m in depth with a width:depth ratio of between 10 and 33. The authors stress that the development of each chalk valley is best considered individually rather than to expect a common history of landscape evolution hence the precise form of the channel system and floodplain habitats is also likely to be valley specific. -
Protecting Wildlife for the Future
CINDERELLA SCORES A HAT-TRICK! 3 years, 3 projects, 3km of winterbourne chalkstream restored Introduction The Dorset Wild Rivers project and the Monitoring & Results Environment Agency have created three successful winterbourne restoration projects In order to measure the impacts of that have delivered a number of outcomes our work, pre and post work including Biodiversity Action Plan (BAP) macroinvertebrate and fish targets, working towards Good Ecological monitoring is being carried out as Status (GES under the Water Framework part of the project. Directive (WFD) and building resilience to climate change. A more diverse habitat supporting diverse wildlife has been created. Winterbournes are rare chalk streams which The bankside vegetation has been are groundwater fed and only flow at certain manipulated to provide a mixture of times of the year as groundwater levels in the both shaded and more open sections aquifer fluctuate. They support a range of of channel and a more species rich specialist wildlife adapted to this unusual margin. flow regime, including a number of rare or scarce invertebrates. Our macro invertebrate sampling indicates that the work has been a So called “Cinderella” chalkstreams because great success: the rare mayfly larva they are so often overlooked. Their Paraleptophlebia werneri (Red Data ecological value is often degraded as a result Book 3), and the notable blackfly of pressures from agricultural practices, land larva Metacnephia amphora, were drainage, urban and infrastructure found in the stream only 6 months development, abstraction and flood after the work was completed. defences. The Conservation value of the new Over centuries, the spring-fed South channel was reassessed using the Winterbourne in Dorset has been degraded. -
Introduction to Common Native & Invasive Freshwater Plants in Alaska
Introduction to Common Native & Potential Invasive Freshwater Plants in Alaska Cover photographs by (top to bottom, left to right): Tara Chestnut/Hannah E. Anderson, Jamie Fenneman, Vanessa Morgan, Dana Visalli, Jamie Fenneman, Lynda K. Moore and Denny Lassuy. Introduction to Common Native & Potential Invasive Freshwater Plants in Alaska This document is based on An Aquatic Plant Identification Manual for Washington’s Freshwater Plants, which was modified with permission from the Washington State Department of Ecology, by the Center for Lakes and Reservoirs at Portland State University for Alaska Department of Fish and Game US Fish & Wildlife Service - Coastal Program US Fish & Wildlife Service - Aquatic Invasive Species Program December 2009 TABLE OF CONTENTS TABLE OF CONTENTS Acknowledgments ............................................................................ x Introduction Overview ............................................................................. xvi How to Use This Manual .................................................... xvi Categories of Special Interest Imperiled, Rare and Uncommon Aquatic Species ..................... xx Indigenous Peoples Use of Aquatic Plants .............................. xxi Invasive Aquatic Plants Impacts ................................................................................. xxi Vectors ................................................................................. xxii Prevention Tips .................................................... xxii Early Detection and Reporting -
Flood Risk from Groundwater: Examples from a Chalk Catchment in 2 Southern England 3 4 A.G
1 Flood risk from groundwater: examples from a Chalk catchment in 2 southern England 3 4 A.G. Hughes1, T. Vounaki1, D.W. Peach1, A.M. Ireson2, C.R. Jackson1, A.P. Butler2, J.P. Bloomfield3, 5 J. Finch4 and H.S. Wheater2 6 1 British Geological Survey, Keyworth, Nottinghamshire, UK 7 2 Department of Civil and Environmental Engineering, Imperial College London, London, UK 8 3 British Geological Survey, Wallingford, Oxfordshire, UK 9 4 Centre for Ecology and Hydrology, Wallingford, Oxfordshire, UK 10 11 12 13 14 Correspondence Abstract A.G. Hughes, British Geological Survey, 15 Groundwater flooding has moved up the policy-makers’ agenda as a result of the 16 Keyworth, Nottinghamshire, UK Email: [email protected] United Kingdom experiencing extensive groundwater flooding in winter 2000/ 17 2001. However, there is a lack of appropriate methods and data to support 18 DOI:10.1111/j.1753-318X.2011.01095.x groundwater flood risk assessment. The implications for flood risk assessment of 19 groundwater flooding are outlined using a study of the Chalk aquifer underlying 20 Key words the Pang and Lambourn catchments in Berkshire, UK. Groundwater flooding in 21 Q2 ’; ’; ’. the Chalk results from the water table reaching the land surface and producing 22 long-duration surface flows (weeks to months), causing significant disruption to 23 transport infrastructure and households. By analyzing existing data with a farmers’ 24 survey, it was found that groundwater flooding consists of a combination of 25 intermittent stream discharge and anomalous springflow. This work shows that 26 there is a significant challenge involved in drawing together data and under- 27 standing of groundwater flooding, which includes vital local knowledge, reason- 28 able risk assessment procedures and deterministic modelling. -
Piddle Valley Conservation Area Review
Item 14 Council Meeting – 16 January 2018 Piddle Valley Conservation Area review 1. Purpose of report The purpose of this report is to seek the Council’s approval to adopt the draft appraisal and boundary proposal prepared for Piddle Valley Conservation Area. 2. Key issues 2.1 The Council designates and reviews conservation areas in fulfilment of statutory duties under Section 69 of the Planning (Listed Buildings and Conservation Areas) Act 1990. Purbeck District has twenty five Conservation Areas, twenty-two of which have been appraised and reviewed since their designation, twenty-one of these since 2008. 2.2 A conservation area is a historic built environment designation. The designation promotes the preservation and enhancement of groups of buildings and structures which hold special historic or architectural interest, together with associated spaces and trees. This is primarily achieved through the sensitive management of change within the planning process. 2.3 Paragraph 127 of the National Planning Policy Framework (NPPF) highlights the importance of ensuring that conservation area designations are justified. This is the key objective of the boundary review, and ensures fairness in the application of controls, and soundness in case of appeal against planning decisions. 2.4 The Council has a statutory duty to consider the impact of planning proposals upon conservation areas. This is reflected in paragraph 129 of the NPPF, which requires local planning authorities to assess the significance of heritage assets as part of the development management process. Assessment of significance is a key objective of conservation area character appraisals, and therefore provides the Council with an important part of the required evidence base in decision making. -
Rainfall Thresholds for Flow Generation in Desert Ephemeral
Water Resources Research RESEARCH ARTICLE Rainfall Thresholds for Flow Generation 10.1029/2018WR023714 in Desert Ephemeral Streams 1 1 2 1 Key Points: Stephanie K. Kampf G!), Joshua Faulconer , Jeremy R. Shaw G!), Michael Lefsky , Rainfall thresholds predict 3 2 streamflow responses with high Joseph W. Wagenbrenner G!), and David J. Cooper G!) accuracy in small hyperarid and 1 2 semiarid watersheds Department of Ecosystem Science and Sustainability, Colorado State University, Fort Collins, Colorado, USA, Department 3 Using insufficient rain data usually of Forest and Rangeland Stewardship, Colorado State University, FortCollins, Colorado, USA, USDA Forest Service, Pacific increases threshold values for larger Southwest Research Station, Arcata, California,USA watersheds, leading to apparent scale dependence in thresholds Declines in flow frequency and Rainfall thresholds for streamflow generation are commonly mentioned in the literature, but increases in thresholds with drainage Abstract area are steeper in hyperarid than in studies rarely include methods for quantifying and comparing thresholds. This paper quantifies thresholds semiarid watersheds in ephemeral streams and evaluates how they are affected by rainfall and watershed properties. The study sites are in southern Arizona, USA; one is hyperarid and the other is semiarid. At both sites rainfall and 3 2 2 Supporting Information: streamflow were monitored in watersheds ranging from 10- to 10 km . Streams flowed an average of 0-5 • Supporting Information 51 times per year in hyperarid watersheds and 3-11 times per year in semiarid watersheds. Although hyperarid sites had fewer flow events, their flow frequency (fraction of rain events causing flow) was higher than in Correspondence to: 2 semiarid sites for small ( < 1 km ) watersheds. -
Veronica Plants—Drifting from Farm to Traditional Healing, Food Application, and Phytopharmacology
molecules Review Veronica Plants—Drifting from Farm to Traditional Healing, Food Application, and Phytopharmacology Bahare Salehi 1 , Mangalpady Shivaprasad Shetty 2, Nanjangud V. Anil Kumar 3 , Jelena Živkovi´c 4, Daniela Calina 5 , Anca Oana Docea 6, Simin Emamzadeh-Yazdi 7, Ceyda Sibel Kılıç 8, Tamar Goloshvili 9, Silvana Nicola 10 , Giuseppe Pignata 10, Farukh Sharopov 11,* , María del Mar Contreras 12,* , William C. Cho 13,* , Natália Martins 14,15,* and Javad Sharifi-Rad 16,* 1 Student Research Committee, School of Medicine, Bam University of Medical Sciences, Bam 44340847, Iran 2 Department of Chemistry, NMAM Institute of Technology, Karkala 574110, India 3 Department of Chemistry, Manipal Institute of Technology, Manipal Academy of Higher Education, Manipal 576104, India 4 Institute for Medicinal Plants Research “Dr. Josif Panˇci´c”,Tadeuša Koš´cuška1, Belgrade 11000, Serbia 5 Department of Clinical Pharmacy, University of Medicine and Pharmacy of Craiova, Craiova 200349, Romania 6 Department of Toxicology, University of Medicine and Pharmacy of Craiova, Craiova 200349, Romania 7 Department of Plant and Soil Sciences, University of Pretoria, Gauteng 0002, South Africa 8 Department of Pharmaceutical Botany, Faculty of Pharmacy, Ankara University, Ankara 06100, Turkey 9 Department of Plant Physiology and Genetic Resources, Institute of Botany, Ilia State University, Tbilisi 0162, Georgia 10 Department of Agricultural, Forest and Food Sciences, University of Turin, I-10095 Grugliasco, Italy 11 Department of Pharmaceutical Technology, Avicenna Tajik State Medical University, Rudaki 139, Dushanbe 734003, Tajikistan 12 Department of Chemical, Environmental and Materials Engineering, University of Jaén, 23071 Jaén, Spain 13 Department of Clinical Oncology, Queen Elizabeth Hospital, Hong Kong SAR 999077, China 14 Faculty of Medicine, University of Porto, Alameda Prof. -
Veronica Odora
Veronica odora COMMON NAME Hebe SYNONYMS Hebe odora (Hook.f.) Cockayne, Leonohebe odora (Hook.f.) Heads, Veronica buxifolia Benth., Hebe buxifolia (Benth.) Cockayne et Allan, Veronica buxifolia var. patens Cheeseman, Veronica anomala J.F.Armstr., Hebe anomala (J.F.Armstr.) Cockayne, Veronica haustrata J.B.Armstr., Veronica buxifolia var. odora (Hook.f.) Kirk, Veronica elliptica var. odora (Hook.f.) Cheeseman, Hebe buxifolia var. odora (Hook.f.) Andersen, Hebe buxiflia (Benth.) Andersen var. buxifolia FAMILY Plantaginaceae AUTHORITY Veronica odora Hook.f. In cultivation. Prostrate form. Photographer: FLORA CATEGORY Jeremy Rolfe Vascular – Native ENDEMIC TAXON Yes ENDEMIC GENUS No ENDEMIC FAMILY No STRUCTURAL CLASS Mt Taranaki, January. Photographer: John Trees & Shrubs - Dicotyledons Smith-Dodsworth NVS CODE HEBODO CHROMOSOME NUMBER 2n = 42, 84 CURRENT CONSERVATION STATUS 2012 | Not Threatened PREVIOUS CONSERVATION STATUSES 2009 | Not Threatened 2004 | Not Threatened BRIEF DESCRIPTION Rounded shrub bearing pairs of small oval leaves with a low ridge on the underside inhabiting mountains south from central North Island and Auckland Islands. Leaves 4.5-11.5mm long by 2.3-5.4mm wide, with abrupt shoulder at base. Leaf bud with small gap at base. Several flower spikes at tip of twigs. DISTRIBUTION Widespread, south from the Huiarau Range, Lake Waikaremoana, on mountains of North Island, South Island, Stewart Island and the Auckland Islands. (see notes below) HABITAT It grows in montane to penalpine grassland, shrubland, bogs and flushes. FEATURES Spreading low or bushy shrub (varies from a rounded bush to very lax and open) to 0.9 (-1.7) m tall. Branches spreading or decumbent or ascending or erect, old stems brown or red-brown or grey or black (at least when dry); branchlets green, puberulent or pubescent, hairs bifarious; internodes (0.9-) 1.3-4.5 mm; leaf decurrencies evident and usually swollen; leaves abscising above nodes and lower part of petioles remaining attached to stem. -
The Natural Capital of Temporary Rivers: Characterising the Value of Dynamic Aquatic–Terrestrial Habitats
VNP12 The Natural Capital of Temporary Rivers: Characterising the value of dynamic aquatic–terrestrial habitats. Valuing Nature | Natural Capital Synthesis Report Lead author: Rachel Stubbington Contributing authors: Judy England, Mike Acreman, Paul J. Wood, Chris Westwood, Phil Boon, Chris Mainstone, Craig Macadam, Adam Bates, Andy House, Dídac Jorda-Capdevila http://valuing-nature.net/TemporaryRiverNC Suggested citation: Stubbington, R., England, J., Acreman, M., Wood, P.J., Westwood, C., Boon, P., The Natural Capital of Mainstone, C., Macadam, C., Bates, A., House, A, Didac, J. (2018) The Natural Capital of Temporary Temporary Rivers: Rivers: Characterising the value of dynamic aquatic- terrestrial habitats. Valuing Nature Natural Capital Characterising the value of dynamic Synthesis Report VNP12. The text is available under the Creative Commons aquatic–terrestrial habitats. Attribution-ShareAlike 4.0 International License (CC BY-SA 4.0) Valuing Nature | Natural Capital Synthesis Report Contents Introduction: Services provided by wet and the natural capital of temporary rivers.............. 4 dry-phase assets in temporary rivers................33 What are temporary rivers?...................................... 4 The evidence that temporary rivers deliver … services during dry phases...................34 Temporary rivers in the UK..................................... 4 Provisioning services...................................34 The natural capital approach Regulating services.......................................35 to ecosystem protection............................................ -
The Nelson Ranch Located Along the Shasta River Has Two Flow Gaging
Baseline Assessment of Salmonid Habitat and Aquatic Ecology of the Nelson Ranch, Shasta River, California Water Year 2007 Jeffrey Mount, Peter Moyle, and Michael Deas, Principal Investigators Report prepared by: Carson Jeffres (Project lead), Evan Buckland, Bruce Hammock, Joseph Kiernan, Aaron King, Nickilou Krigbaum, Andrew Nichols, Sarah Null Report prepared for: United States Bureau of Reclamation Klamath Area Office Center for Watershed Sciences University of California, Davis • One Shields Avenue • Davis, CA 95616-8527 Table of Contents 1. EXECUTIVE SUMMARY..................................................................................................................................2 2. INTRODUCTION...............................................................................................................................................6 3. ACKNOWLEDGEMENTS .................................................................................................................................6 4. SITE DESCRIPTION.........................................................................................................................................7 5. HYDROLOGY.....................................................................................................................................................8 5.1. STAGE-DISCHARGE RATING CURVES .......................................................................................................9 5.2. PRECIPITATION........................................................................................................................................11 -
Estuary Assessment
Appendix I Estuary Assessment Poole and Christchurch Bays SMP2 9T2052/R1301164/Exet Report V3 2010 Haskoning UK Ltd on behalf of Bournemouth Borough Council Poole & Christchurch Bays SMP2 Sub-Cell 5f: Estuary Processes Assessment Date: March 2009 Project Ref: R/3819/01 Report No: R.1502 Poole & Christchurch Bays SMP2 Sub-Cell 5f: Estuary Processes Assessment Poole & Christchurch Bays SMP2 Sub-Cell 5f: Estuary Processes Assessment Contents Page 1. Introduction....................................................................................................................1 1.1 Report Structure...........................................................................................................1 1.2 Literature Sources........................................................................................................1 1.3 Extent and Scope.........................................................................................................2 2. Christchurch Harbour ....................................................................................................2 2.1 Overview ......................................................................................................................2 2.2 Geology........................................................................................................................4 2.3 Holocene to Recent Evolution......................................................................................4 2.4 Present Geomorphology ..............................................................................................5 -
The Wareham Two Rivers Walks
THE WAREHAM Two Rivers Walks TWO RIVERS WALKS The Two Rivers Walks journey through beautiful ecologically-rich areas as they wind alongside the River Frome and the River Piddle. These two rivers flow through Wareham into Poole harbour, one of the largest natural Wareham to Swineham point harbours in the world, and support a wide variety of stunning flora and fauna. Along this walk experience: - Incredible Biodiversity The two rivers walks travel through designated Sites of Special Scientific Interest (SSSI). The combination of soil type, wet areas, tidal flooding and land management has supported the rich ecology and biodiversity for which the area is renowned. This area supports 40,000 birds in the winter, and a wonderful variety of birds can be seen throughout the year such as lapwings, redshanks and kingfishers. It is not uncommon to see otters along this route and hear River Piddle fisheries the ‘plop’ of a shy water vole dive into the water before being seen. The rivers also support a variety of fish such as Ragged Robin trout and salmon which spend much of their life at sea but return to healthy rivers to breed. - Archaeological History The stunning landscape that can be viewed along the walk has been shaped by human activity throughout the ages. Excavations have shown that the area has been used by humans for thousands of years, with relics being found that show there were once Bronze Age settlements here. River Frome reed bed The rich natural resources that were in this area, such as clay, stone and chalk were what would have once attracted settlers to Wareham.