Stream Inventory Handbook

Total Page:16

File Type:pdf, Size:1020Kb

Stream Inventory Handbook STREAM INVENTORY HANDBOOK LEVEL I & II APPENDIX REFERENCE IN TEXT Ohanapecosh River - Gifford Pinchot NF PACIFIC NORTHWEST REGION REGION 6 2010 ~ Version 2.10 Stream Inventory Handbook: Level 1 and Level II CONTENTS CHAPTER 1 Introduction/Overview ......................................................................... 4 Background ............................................................................................................................ 4 Inventory Attributes ............................................................................................................... 5 Establishing Forest Priorities ................................................................................................. 6 Stream Inventory Program Management ............................................................................... 6 Program Administration And Quality Control ...................................................................... 7 A Standard Protocol ............................................................................................................... 8 Presentation of Information ................................................................................................... 9 Handbook Content ............................................................................................................... 10 CHAPTER 2 Office Procedures Level I Inventory - Identification Level ..............12 Objectives ............................................................................................................................ 12 Standards .............................................................................................................................. 12 Equipment/information Needed ........................................................................................... 12 Procedure ............................................................................................................................. 13 Products................................................................................................................................ 13 Survey Form .............................................................................................................. 14 Preliminary Reach Form ............................................................................................ 18 CHAPTER 3 Field Procedures: Level II Inventory-Aquatic Ecosystem Inventory 24 Objectives ............................................................................................................................ 24 Safety ................................................................................................................................... 24 Standards .............................................................................................................................. 25 Equipment/information Needed ........................................................................................... 26 Procedures ............................................................................................................................ 27 Products................................................................................................................................ 27 FINAL REACH FORM ............................................................................................. 28 Channel Unit Form .................................................................................................... 34 Special Cases Form (Culverts, Dams, Falls, Chutes, and Marshlands) ..................... 54 COMMENTS FORM ................................................................................................ 58 Aquatic Biota Form ................................................................................................... 61 SAFETY .................................................................................................................... 61 CHAPTER - 4 Specialized Field Procedures: Discharge and Wolman .................67 Stream Habitat Data Discharge Form ........................................................................ 67 Wolman Form ............................................................................................................ 73 APPENDIX A Watershed Codes .............................................................................79 APPENDIX B Stream Orders ..................................................................................80 APPENDIX C Forest Options .................................................................................81 VALLEY FORM CODES ......................................................................................... 81 VALLEY CROSS-SECTION ................................................................................... 81 APPENDIX D Successional Class Codes ...............................................................92 Version 2.10 2 Stream Inventory Handbook: Level 1 and Level II APPENDIX E Stream Inventory Glossary ..............................................................93 GLOSSARY OF STREAM INVENTORY ACRONYMS AND ABBREVIATIONS ...............................................................................................104 APPENDIX F - Table of Life Stage Values ..........................................................109 APPENDIX G - Table of Life History Values ......................................................110 APPENDIX H Stream Inventory JHA ...................................................................111 INDEX ...................................................................................................................114 Version 2.10 3 Stream Inventory Handbook: Level 1 and Level II CHAPTER 1 Introduction/Overview BACKGROUND Periodic, recurring inventories are an integral part of the fish habitat and watershed management programs and form the foundation for effective program management. Inventories should produce comparable information, both between administrative units, as well as across time. They will generate the baseline information that will be used to support a variety of management activities, including, but not limited to; watershed analysis, timber sales, range allotments, special use permitting, and fish habitat and watershed restoration programs. They will also serve as the basis for stream monitoring and evaluation programs. Specifically, inventories will identify existing aquatic and riparian conditions, identify factors limiting the productive capabilities of habitats, measure attainment of meeting stream habitat objectives, and help to assess cumulative watershed effects. The inventories can be used to monitor and refine Land Management Plan Standards and Guidelines. The Pacific Northwest Region (Region 6) stream inventory is designed on a hierarchical scale to provide the user the opportunity to choose an inventory protocol which meets the data needs for the questions asked. Level I is the basic in-office procedure which identifies standard attributes of the watershed/stream to be analyzed. Its primary objective is to document and consolidate sources of general knowledge of the stream system. Level II is an extensive stream channel, riparian vegetation, aquatic habitat condition and biotic inventory on a watershed-wide scale. This level is to be used to determine the "pulse" or condition of a system during low flow conditions. Level III is an intensive field inventory designed specifically to answer a particular question (i.e., monitoring, project level planning and project design, etc.). This handbook provides standards for both the level I (office inventory) and level II (field inventory). A level II inventory requires the completion of a level I as a prerequisite. The protocol identifies core attributes that are necessary to evaluate the condition of the stream (mandatory for collection), and non-core, Forest optional attributes. Forests have the flexibility to add attributes to the protocol to meet their needs; however, unit costs and target allocations/accomplishments will be based on the Regional protocol. Region 6 has produced a recommended protocol for level III inventories, but the methods are not included in this handbook. By contrast, it is recognized that a standardized approach to level IV is inappropriate due of the large variation in data needs that exist. Therefore, procedures for level IV are open to development at the District, Forest, or research unit level. The purpose of both the level I and level II inventories is to identify existing stream channel, riparian and aquatic ecosystem conditions on a watershed scale. As inventories are completed and repeated over time, the information generated by them can be useful in measuring changes in Version 2.10 4 Stream Inventory Handbook: Level 1 and Level II stream channel conditions and determining attainment of habitat management objectives, provided stringent quality control administration occurs. In this context, the inventory can be applied as a basic "monitoring" tool. INVENTORY ATTRIBUTES Key attributes of the Region 6 level I and II stream inventories were developed considering the following concepts: Driven by questions that are to be addressed. Identification of management questions formed the basis for the content of the inventory. The ability to address questions consistently and comparably across units has been demanded of the United States Department of Agriculture, Forest Service (FS) by both users and managers of the resources. Inventory and analysis procedures were developed
Recommended publications
  • Geomorphic Classification of Rivers
    9.36 Geomorphic Classification of Rivers JM Buffington, U.S. Forest Service, Boise, ID, USA DR Montgomery, University of Washington, Seattle, WA, USA Published by Elsevier Inc. 9.36.1 Introduction 730 9.36.2 Purpose of Classification 730 9.36.3 Types of Channel Classification 731 9.36.3.1 Stream Order 731 9.36.3.2 Process Domains 732 9.36.3.3 Channel Pattern 732 9.36.3.4 Channel–Floodplain Interactions 735 9.36.3.5 Bed Material and Mobility 737 9.36.3.6 Channel Units 739 9.36.3.7 Hierarchical Classifications 739 9.36.3.8 Statistical Classifications 745 9.36.4 Use and Compatibility of Channel Classifications 745 9.36.5 The Rise and Fall of Classifications: Why Are Some Channel Classifications More Used Than Others? 747 9.36.6 Future Needs and Directions 753 9.36.6.1 Standardization and Sample Size 753 9.36.6.2 Remote Sensing 754 9.36.7 Conclusion 755 Acknowledgements 756 References 756 Appendix 762 9.36.1 Introduction 9.36.2 Purpose of Classification Over the last several decades, environmental legislation and a A basic tenet in geomorphology is that ‘form implies process.’As growing awareness of historical human disturbance to rivers such, numerous geomorphic classifications have been de- worldwide (Schumm, 1977; Collins et al., 2003; Surian and veloped for landscapes (Davis, 1899), hillslopes (Varnes, 1958), Rinaldi, 2003; Nilsson et al., 2005; Chin, 2006; Walter and and rivers (Section 9.36.3). The form–process paradigm is a Merritts, 2008) have fostered unprecedented collaboration potentially powerful tool for conducting quantitative geo- among scientists, land managers, and stakeholders to better morphic investigations.
    [Show full text]
  • Stream Restoration, a Natural Channel Design
    Stream Restoration Prep8AICI by the North Carolina Stream Restonltlon Institute and North Carolina Sea Grant INC STATE UNIVERSITY I North Carolina State University and North Carolina A&T State University commit themselves to positive action to secure equal opportunity regardless of race, color, creed, national origin, religion, sex, age or disability. In addition, the two Universities welcome all persons without regard to sexual orientation. Contents Introduction to Fluvial Processes 1 Stream Assessment and Survey Procedures 2 Rosgen Stream-Classification Systems/ Channel Assessment and Validation Procedures 3 Bankfull Verification and Gage Station Analyses 4 Priority Options for Restoring Incised Streams 5 Reference Reach Survey 6 Design Procedures 7 Structures 8 Vegetation Stabilization and Riparian-Buffer Re-establishment 9 Erosion and Sediment-Control Plan 10 Flood Studies 11 Restoration Evaluation and Monitoring 12 References and Resources 13 Appendices Preface Streams and rivers serve many purposes, including water supply, The authors would like to thank the following people for reviewing wildlife habitat, energy generation, transportation and recreation. the document: A stream is a dynamic, complex system that includes not only Micky Clemmons the active channel but also the floodplain and the vegetation Rockie English, Ph.D. along its edges. A natural stream system remains stable while Chris Estes transporting a wide range of flows and sediment produced in its Angela Jessup, P.E. watershed, maintaining a state of "dynamic equilibrium." When Joseph Mickey changes to the channel, floodplain, vegetation, flow or sediment David Penrose supply significantly affect this equilibrium, the stream may Todd St. John become unstable and start adjusting toward a new equilibrium state.
    [Show full text]
  • Riparian Buffer
    Riparian Buffer A Technical Primer on Assessing Potential Water Quality Improvements for the Quantifying Benefits of Miyun Reservoir in Beijing, China Watershed Interventions September 2016 Prepared by: “Andrew” Feng Fang, Ph.D. Work supported by: Mark S. Kieser 536 E. Michigan Ave, Suite 300 Kalamazoo, MI 49007 USA The China Mega-City Water Fund (CMWF) was launched in August of 2015 in cooperation with the Beijing Forestry Society (BFS), China Biodiversity Conservation and Green Development Foundation (CBCGDF), International Union for Conservation of Nature (IUCN), and Forest Trends. Once fully operating, the CMWF will identify, fund, and help implement watershed improvement projects (“interventions”) to benefit water quality and water quantity in the Miyun Reservoir. The City of Beijing relies in part on this reservoir as a critical drinking water supply. A notable challenge facing the CMWF, and other water funds throughout the world, is the ability to reasonably estimate water quality and/or water quantity benefits associated with specific interventions. Recent 2016 efforts have established an operating framework for the CMWF that will evaluate various watershed interventions in the context of relatively simple, established performance metrics for water quality and water quantity benefits. Coupled with projected costs for such interventions, the CMWF will be able to assess, compare and optimize benefits associated with its investments in watershed improvements with this framework. This Technical Primer1 represents an initial examination of quantification methods that the CMWF and others may use to reliably estimate water resource benefits derived from particular land management interventions in the watershed of the Miyun Reservoir. This approach relies upon existing studies from both the Miyun Reservoir watershed and other basins in China.
    [Show full text]
  • Quantitative Geomorphology of Drainage Basins Related to Fish
    INFORMATIONAL LEAFLET NO. 162 QUANTITATIVE GEOMORPHOLOGY OF DRA INAGE BAS INS RELATED TO F ISH PRODUCT ION BY G. L. Ziemer STATE OF ALASKA William A. Egan - Governor DEPARTMENT OF F l SH AND GAME James W. Brooks, Commissioner Subport Building, Juneau 99801 July 1973 TABLE OF CONTENTS Page ABSTRACT .............................. 1 INTRODUCTION .......................... 1 GEOMORPHIC ELEMENTS ...................... 2 OBJECTIVES ............................ 4 METHODOLOGY .......................... 4 SUMMARY ............................. 11 CONCLUSIONS ........................... 14 REFERENCES ............................ 18 APPENDIX A . GEOMORPHIC ELEMENTS .............. 19 APPENDIX B . MEASURE OF FISH PRODUCTION .......... 25 QUANTITATIVE GEOMORPHOLOCX OF DRAINAGE BASINS RELATED TO FISH PRODUCTION G.L. Ziemer, P.E. Chief Engineer Alaska Department of Fish and Game Juneau, Alaska ABSTRACT This report covers the results of a study investigating the possibility of developing a classification index system for watersheds which would quan- tify their total composite salmon production potential. The premise was tested that, within a geologically and climatologically homogenous region, the water flow regimen of streams, and the channels that flow builds, is universally related to certain identifiable characteristics of their basins and drainages and that these control or indicate the level of fisheries production. This study shows that a correlation between drainage system geometry and freshwater production factors for anadromous fishes can be shown, and an index expressing that relationship, in the case of pink salmon in Prince William Sound, has been developed. INTRODUCTION As anadromous fisheries management proceeds from the basic position of husbandry of the existing stocks to the addition of programs designed to increase the quantity and to enhance the quality of the freshwater environment for fish production, it becomes desirable to provide to the manager better tools to equate one site against another so his projects return the maximum dividends.
    [Show full text]
  • National Stream Internet Protocol and User Guide
    National Stream Internet Protocol and User Guide David Nagel1, Erin Peterson2, Daniel Isaak1, Jay Ver Hoef3, and Dona Horan1 U.S. Forest Service, Rocky Mountain Research Station Air, Water, and Aquatic Environments Program 322 E. Front St., Boise, ID 1 Author affiliations: 1 US Forest Service, Rocky Mountain Research Station, AWAE Program, 322 E. Front St., Suite 401, Boise, ID 83702. 2 Queensland University of Technology, Brisbane, Queensland, Australia. 3 National Oceanic and Atmospheric Administration, Fairbanks, AK. Version 3-22-2017 Abstract The rate at which new information about stream resources is being created has accelerated with the recent development of spatial stream-network models (SSNMs), the growing availability of stream databases, and ongoing advances in geospatial science and computational efficiency. To further enhance information development, the National Stream Internet (NSI) project was developed as a means of providing a consistent, flexible analytical infrastructure that can be applied with many types of stream data anywhere in the country. A key part of that infrastructure is the NSI network, a digital GIS layer which has a specific topological structure that was designed to work effectively with SSNMs. The NSI network was derived from the National Hydrography Dataset Plus, Version 2 (NHDPlusV2) following technical procedures that ensure compatibility with SSNMs. This report describes those procedures and additional steps that are required to prepare datasets for use with SSNMs. 2 1.0 Introduction 1.1 Overview The USGS National Hydrography Dataset Plus, Version 2 (NHDPlusV2) (McKay et al., 2012) is an attribute rich, GIS stream network developed at 1:100,000 scale by the Environmental Protection Agency (EPA) and U.S.
    [Show full text]
  • James City County Perennial Stream Protocol Guidance Manual
    James City County Perennial Stream Protocol Guidance Manual Purpose This protocol defines the procedure for making field determinations of the presence and the origin of a perennial stream. The procedure was developed to meet the requirement of James City County’s Chesapeake Bay Preservation Ordinance, Section 23-8, to perform site-specific field evaluations to determine the boundaries of Resource Protection Areas (RPA) and Section 23-10(2) to identify water bodies with perennial flow. Development of the protocol was finalized using funds from the Chesapeake Bay Implementation Grant #BAY-2007-14-PT awarded to the County by the Department of Conservation and Recreation (DCR). Introduction This protocol describes the process of determining whether a stream in James City County has perennial flow, and if necessary, determining the origin of the perennial stream. The origin of the perennial reach may occur as a transition from an ephemeral or intermittent reach or may occur at a spring with no upslope stream channel. The field identification of a perennial stream is based on the combination of hydrological, physical and biological characteristics of a stream. In the protocol, the field indicators of these characteristics are classified as primary or secondary and ranked using a weighted, four-tiered scoring system similar to the current system developed by the North Carolina Division of Water Quality (NCDWQ 2005) as modified to address conditions in James City County. A stream reach is classified as perennial based on the overall score but with consideration of other supporting information such as long term monitoring or historic information in certain situations.
    [Show full text]
  • Spatial Patterns in CO 2 Evasion from the Global River Network Ronny Lauerwald, Goulven Laruelle, Jens Hartmann, Philippe Ciais, Pierre A.G
    Spatial patterns in CO 2 evasion from the global river network Ronny Lauerwald, Goulven Laruelle, Jens Hartmann, Philippe Ciais, Pierre A.G. Regnier To cite this version: Ronny Lauerwald, Goulven Laruelle, Jens Hartmann, Philippe Ciais, Pierre A.G. Regnier. Spatial patterns in CO 2 evasion from the global river network. Global Biogeochemical Cycles, American Geophysical Union, 2015, 29 (5), pp.534 - 554. 10.1002/2014GB004941. hal-01806195 HAL Id: hal-01806195 https://hal.archives-ouvertes.fr/hal-01806195 Submitted on 28 Oct 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. PUBLICATIONS Global Biogeochemical Cycles RESEARCH ARTICLE Spatial patterns in CO2 evasion from the global 10.1002/2014GB004941 river network Key Points: Ronny Lauerwald1,2,3, Goulven G. Laruelle1,4, Jens Hartmann3, Philippe Ciais5, and Pierre A. G. Regnier1 • First global maps of river CO2 partial pressures and evasion at 0.5° 1Department of Earth and Environmental Sciences, Université Libre de Bruxelles, Brussels, Belgium, 2Institut Pierre-Simon resolution Laplace, Paris, France, 3Institute for Geology, University of Hamburg, Hamburg, Germany, 4Department of Earth Sciences- • Global river CO2 evasion estimated at À 5 650 (483–846) Tg C yr 1 Geochemistry, Utrecht University, Utrecht, Netherlands, LSCE IPSL, Gif Sur Yvette, France • Latitudes between 10°N and 10°S contribute half of the global CO2 evasion Abstract CO2 evasion from rivers (FCO2) is an important component of the global carbon budget.
    [Show full text]
  • Fluvial Geomorphology
    East Branch Delaware River Stream Corridor Management Plan Volume 2 Fluvial Geomorphology: the Hydrology: the science study of riverine landforms and dealing with the properties, the processes that create them distribution, and circulation of water on and below the earth’s surface and in the atmosphere (Merriam-Webster Online 09/12/07) An understanding of both hydrology and fluvial geomorphology is essential when approaching stream management at any level. This section is intended to serve as an overview of both aspects of stream science, as well as their relation to management practices past and present. Applied fluvial geomorphology utilizes the relationships and principles developed through the study of rivers and streams and how they function within their landscape to preserve and restore stream systems. In landscapes unchanged by human activities, streams reflect the regional climate, biology and geology. Bedrock and glacial deposits influence the stream system within its drainage basin. The “dendritic” (formed like the branches of a tree, Figure 3.1) stream pattern of the East Branch Delaware River watershed developed because horizontally bedded, sedimentary Figure 3.1 Stream Ordering (NRCS) and the bedrock had a gently sloping regional Depiction of a Dendritic Stream System dip at the time the initial drainage channels began forming16. The bedrock’s jointing pattern (the pattern of deep, vertical fractures) also influence stream pattern formation. The region’s geologic history has favored the development of non-symmetric drainage basins in the East Branch basin. As rivers flow across the landscape, they generally increase in size, merging with other rivers. This increase in size brings about a concept known as stream order.
    [Show full text]
  • Stream Order
    About Tutorial Glossary Documents Images Maps Google Earth Please provide feedback! Click for details The River Basin You are here: Home>The River Basin >Hydrology>Principles of Hydrology >Surface Water >Stream Order Introduction Geography Climate and Weather Hydrology Stream Order Principles of Hydrology Water Cycle Surface Water Most rivers are considered as reaches with different geomorphological characteristics. Stream Order The most simple divison generally made is to divide the river into Upper and Lower Lakes and Reservoirs River reaches Flooding Groundwater Upper River SW/ GW Interactions Water Balance Explore the sub- basins of the Hydrology of Southern The uppermost portion of a river system includes the river headwaters and low- order Kunene River Africa streams at higher elevation. The upper river basin is usually characterised by steep Hydrology of the Kunene gradients and by erosion that carries sediment downstream. Streams in this upper Basin region are usually steep and torrential, and often include rapids and waterfalls. These Water Quality streams generally have little floodplain, although part of the bank and surrounding Ecology & Biodiversity land may be wetted during periods of high flow. Watersheds References Lower River The lower section of a river system (extending to the mouth), usually exhibits a larger river channel and lower slope – the landscape is usually flat. In the middle portion of the river there is a balance between erosion and deposition of sediment. Further Video Interviews about the downstream, the lower river sees mainly deposition, though localised erosion and integrated and transboundary reworking of sediments may also occur. The main channel of the river often forms a management of the Kunene sinuous (meandering) path across the landscape unless artificially channelled.
    [Show full text]
  • Creek, Stream, Or Branch
    Creek, Stream, or Branch What is the difference between a creek, stream or a branch, and when does a spring become one of them? Let me introduce you to the world of stream classification. To begin at the beginning, streams have their origin high up in their watershed. A watershed is that area in which precipitation falls and collects into water bodies. On a large scale, Mitchell, Yancey, and Avery Counties drain into the French Broad River Basin. Within these river basins are many sub-basins or smaller watersheds that drain into tributaries or creeks. When rainfall hits the earth it either infiltrates and recharges groundwater or it runs off and goes into a stream. Most infiltrating rainfall enters shallow groundwater which feeds year-round streams, which is why year-round, or perennial streams and rivers run with water even in dry weather. Old hand dug or bored (shallow) wells tap into shallow ground water, which is why shallow wells can dry- up during prolonged droughts. Of the approximately 40-55 inches of annual rainfall that Mitchell, Yancey, and Avery Counties receive in an average year, only one inch penetrates into the deep groundwater on which most drilled wells depend. If a stream runs wet only during rainfall events, it is called an ephemeral stream. Ephemeral steams depend upon stormwater runoff for water. These streams are perched above the shallow water table, so when rain stops falling, they dry up. The second level of stream is called an intermittent stream. Intermittent streams run with water only during part of the year, typically during winter and spring when shallow water tables are highest.
    [Show full text]
  • A Mass Balance of Nitrogen in a Large Lowland River (Elbe, Germany)
    water Article A Mass Balance of Nitrogen in a Large Lowland River (Elbe, Germany) , Stephanie Ritz * y and Helmut Fischer Federal Institute of Hydrology—BfG, Am Mainzer Tor 1, 56068 Koblenz, Germany; [email protected] * Correspondence: [email protected] Current address: Federal Agency of Nature Conservation—BfN, Konstantinstrasse 110, 53179 Bonn, Germany. y Received: 23 September 2019; Accepted: 13 November 2019; Published: 14 November 2019 Abstract: Nitrogen (N) delivered by rivers causes severe eutrophication in many coastal waters, and its turnover and retention are therefore of major interest. We set up a mass balance along a 582 km river section of a large, N-rich lowland river to quantify N retention along this river segment and to identify the underlying processes. Our assessments are based on four Lagrangian sampling campaigns performed between 2011 and 2013. Water quality data served as a basis for calculations of N retention, while chlorophyll-a and zooplankton counts were used to quantify the respective primary and secondary transformations of dissolved inorganic N into biomass. The mass balance 2 1 revealed an average N retention of 17 mg N m− h− for both nitrate N (NO3–N) and total N (TN). Stoichiometric estimates of the assimilative N uptake revealed that, although NO3–N retention was associated with high phytoplankton assimilation, only a maximum of 53% of NO3–N retention could be attributed to net algal assimilation. The high TN retention rates in turn were most probably caused by a combination of seston deposition and denitrification. The studied river segment acts as a TN sink by retaining almost 30% of the TN inputs, which shows that large rivers can contribute considerably to N retention during downstream transport.
    [Show full text]
  • A Hydrological Framework for Persistent River Pools in Semi- Arid Environments
    https://doi.org/10.5194/hess-2020-133 Preprint. Discussion started: 1 April 2020 c Author(s) 2020. CC BY 4.0 License. A hydrological framework for persistent river pools in semi- arid environments 1 Sarah A. Bourke , Margaret Shanafield2, Paul Hedley3, Shawan Dogramaci3 5 1School of Earth Sciences, University of Western Australia, Crawley WA 6009 Australia 2College of Science and Engineering, Flinders University, Bedford Park, SA 5042, Australia 3Rio Tinto Iron Ore, Perth, WA 6000 Australia Correspondence to: Sarah A. Bourke ([email protected]) Abstract 10 Persistent surface water pools along non-perennial rivers represent an important water resource for the plants, animals, and humans that inhabit semi-arid regions. While ecological studies of these features are not uncommon, these are rarely accompanied by a rigorous examination of the hydrological and hydrogeological characteristics that create or support the pools. Here we present an overarching framework for understanding the hydrology of persistent pools based on data from 22 pools in the Hamersley Basin in Western Australia. Three dominant 15 mechanisms that control the occurrence of persistent pools have been identified; perched pools, through flow pools and groundwater discharge pools. Groundwater discharge pools are further categorized into those that are present because of a geological contact or barrier, and those that are controlled by topography. A suite of diagnostic tools (including geological mapping, hydraulic data and hydrochemical surveys) is generally required to identify the mechanism supporting persistent pools. Perched pools are sensitive to climate variability but their 20 persistence is largely independent of groundwater withdrawals. Water fluxes to pools from alluvial and bedrock aquifers can vary seasonally and resolving these inputs is generally non-trivial.
    [Show full text]