What is GeoPEARL? GeoPEARL is a spatially-distributed model of pesticide leaching to the groundwater and surface waters in the Netherlands. Calculations.

Slides:



Advertisements
Similar presentations
The Australian Soil Resource Information System David Jacquier, Neil McKenzie, Garry Swan, Linda Gregory CSIRO Land & Water.
Advertisements

1 Water discharge rate is monitored continually. 2 Sampling of stream and drainage water is made automatically or by grab sampling weekly while groundwater.
The Drainage Basin System
Short introduction to the use of PEARL General properties First tier assessments Higher tier assessments Before looking at first and higher tier assessments,
WHAT IS ELINK? Thermoflow, Inc.
Pollution in Rivers Design by H Graham BSc PGCE. AIR Land flowing water River Bed.
Factors influencing Soil Formation
NWS Calibration Workshop, LMRFC March, 2009 Slide 1 Sacramento Model Derivation of Initial Parameters.
Formation and Characteristics of Hawaii’s Soils
Distribution of Nitrate in Ground Water Under Three Unsewered Subdivisions Erin P. Eid Mike Trojan Jim Stockinger Jennifer Maloney Minnesota Pollution.
A spatially-distributed model of pesticide leaching Aaldrik Tiktak
Hydrological Modelling of Small Scale Processes in a Wetland Habitat O. M. JOHANSEN, J.B. JENSEN & M.L. PEDERSEN Aalborg University, Department of Civil.
The Graphical User Interface.
Non-point pollution modelling by Dr. Anders Refsgaard DHI, Water and Environment Denmark.
NATURAL RESOURCES II: WATER RESOURCES. ANNUAL MOVEMENT OF WATER ON THE GLOBE.
Introduction to Agriculture Soil Science Unit 2. » Physical properties or characteristics of the soil determine to a large degree how useable and productive.
Models to predict metal leaching to ground- and surface water: from soil data to scenario studies Bert-Jan Groenenberg, Luc Bonten, Paul Römkens.
Solutions and Suspensions
Advancements in Simulating Land Hydrologic Processes for Land Surface Modeling (LSM) Hua Su Presentation for Physical Climatology.
Jaco van der Gaast The Winand Staring Centre, P.O. Box 125, 6700 AC Wageningen, The Netherlands 1 Water Management Tools Jaco van der Gaast The Winand.
Basin-scale assessment of transport of water and agricultural chemicals through the unsaturated zone Rick Webb, Randy Bayless, Tracy Hancock, Chuck Fisher,
Water Quality Data, Maps, and Graphs Over the Web · Chemical concentrations in water, sediment, and aquatic organism tissues.
Human Activity. TEK 7.8C I can model the effects of human activity on ground water and surface water in a watershed.
Lecture Notes Applied Hydrogeology
Water Movement Below Surface
1 Soils Soil is made up of a number of different layers.
Integrated Ecological Assessment February 28, 2006 Long-Term Plan Annual Update Carl Fitz Recovery Model Development and.
 Basin irrigation is still used today. It consists of a field enclosed by a raised bank called a dike. The water is allowed to flood the field and the.
Trends in Shallow Ground-Water Quality of the Delmarva Peninsula Results from regional and local studies Linda M. Debrewer Judith M. Denver U.S. Department.
355.T1 Model Agricultural Core Curriculum: Supplement University of California, Davis Irrigation Practices Sources of Irrigation Water The majority of.
How are GeoPEARL assessments carried out? GeoPEARL is run for plots, depending on spatial detail wanted; The model.
Land and Water Resource Information Systems By David R. Maidment Center for Research in Water Resources University of Texas at Austin Presented at UN.
Fresh water lenses on saline groundwater Dispersive Behavior of the Mixing Zone between a Shallow Freshwater Lens and Upward Seeping Saline Groundwater.
Water and ph Done by: Rashid Khalid Alneaimi Class:
DIAS INFORMATION DAY GLOBAL WATER RESOURCES AND ENVIRONMENTAL CHANGE Date: 09/07/2004 Research ideas by The Danish Institute of Agricultural Sciences (DIAS)
Properties of Water. Learning Objectives  Discuss the unique properties of water.  Differentiate between solutions and suspensions.  Explain what acidic.
RACC High School Training June 26, 2012 Jody Stryker University of Vermont Introduction to Watershed Hydrology.
351.T1 Model Agricultural Core Curriculum: Supplement University of California, Davis Irrigation Systems Water Requirements are Effected by: The crop being.
7-4.4 SOIL QUALITY. Soil is one of the most valuable abiotic factors in an ecosystem because everything that lives on land depends directly or indirectly.
Revision presentation. The drainage basin 1.the edge of highland surrounding a river. 2.An area from which all precipitation flows to a single stream.
Redistribution. the continued movement of soil water after infiltration ends rate decreases over time influences plant available water influences solute.
9GH Environmental Chemistry and Using Chemistry
Soil and Permafrost Ooooh! Exciting .
FREEWAT Project FREEWAT (FREE and open source tools for WATer resource management) is a HORIZON 2020 project financed by the EU Commission under the call WATER.
Basic soil properties in GeoPEARL
Basic Hydrology & Hydraulics: DES 601
Soil Science Objectives: Identify the major soil areas of Alabama. Identify the layers in a soil profile. Determine the texture of different soil samples.
Loge or not Loge? Some Questions with Answers about Soil Properties
Space-Time in Hydrology How to define the GIS of the Future?
8.3 Properties of Acids and Bases
Aquifers and Groundwater flow
Soil Formation Soil horizons - layers of soil renewal
Human Activity.
Welcome to GIS in Water Resources 2017
Properties of Water Notes
Soil 7.EC.5A.2 Construct explanations of how soil quality (including composition, texture, particle size, permeability, and pH) affects the characteristics.
Soil Quality
Soil Textures Brown earth - 40% sand, 40% silt, and 20% clay
7.EC.5A.2 Construct explanations of how soil quality (including composition, texture, particle size, permeability, and pH) affects the characteristics.
Landscape Regions.
KEY CONCEPT Water’s unique properties allow life to exist on Earth.
Soil texture Coarse (sandy) soils conduct more heat, but have less heat capacity Fine-grained (clay) soils “hold onto” water.
Welcome to GIS in Water Resources 2013
Texas Aquatic Ecosystems
Chapter 4 Boundaries.
Newbury slope: (a) slope cross-section and soil water retention and hydraulic conductivity function properties for the modelled London Clay; (b) history.
Properties of Water Polarity Cohesion Adhesion Solubility
Chemical Reactions.
Distribute and combine like terms
The Water or Hydrological Cycle
Presentation transcript:

What is GeoPEARL? GeoPEARL is a spatially-distributed model of pesticide leaching to the groundwater and surface waters in the Netherlands. Calculations are performed for 1D-columns During the parameterisation of the model, information from a regional groundwater flow model was used so that it is possible to distinguish between fluxes into the groundwater and fluxes into surface waters (next slide).

Position of PEARL column in landscape field- ditches water courses < 3m water courses > 3 m PEARL 1D column Leaching into the regional groundwater Groundwater table Drainage into local surface waters

The plot approach PEARL is run in a GIS context for a large number of unique combinations (plots) of soil, climate, land-use and hydrogeological units.

Derivation of the unique combinations: GeoPEARL is a spatially-distributed model of pesticide leaching to the groundwater and surface waters in the Netherlands The core of the model consists of a 1D-model, i.e. FOCUS PEARL 2.2.2. PEARL is run in a GIS context for a large number of unique combinations (plots) of soil, climate, land-use and hydrogeological units. A Graphical User Interface facilitates model use.

Plots are represented by a single vertical column: A plot

Basic soil properties in GeoPEARL Clay soils with near neutral pH-values (‘lower part’) Acidic peat soils Slightly acidic sandy soils (‘higher part’)