LIFE Project code: LIFE+10 ENV/IT/ Action 8b Parco Delta - Deliverable

Size: px
Start display at page:

Download "LIFE Project code: LIFE+10 ENV/IT/ Action 8b Parco Delta - Deliverable"

Transcription

1 WATER POLLUTION REDUCTION AND WATER SAVING USING A NATURAL ZEOLITITE CYCLE LIFE Project Code: LIFE+10/ENV/IT/ Notice Boards Deliverable product of the Ente regionale per i Parchi e la Biodiversità Delta del Po ER Code of the associated Action: 8b Deadline: 30/01/2013 Lucilla Previati Maria Cristina Veratelli

2 ANNEX 7.22 NOTICE BOARDS, ROLL-UPS, FLAGS AND PLATES 1. NOTICE BOARDS Two equal generic notice boards appear respectively by the experimental field and by the prototype. Two different specific notice boards appear respectively by the experimental field and by the prototype. So it has been produced three different types of notice boards. 1 The generic notice board installed in a pre-fixed geo-referentiated point, given by the Coordinating Beneficiary, located near the experimental field, with (first image) and without (second image) project s flag. 2

3 The generic notice board installed in a pre-fixed geo-referentiated point, given by the Coordinating Beneficiary, located near the prototype. 3

4 Overview of the project s experimental field located in the farm Amadori in territory of the Municipality of Codigoro. 4

5 The specific notice board for the experimental field, installed in a pre-fixed geo-referentiated point, given by the Coordinating Beneficiary. The specific notice board for the prototype, installed in a pre-fixed geo-referentiated point, given by the Coordinating Beneficiary 5

6 The graphic image of the generic notice-board. Each panel measures 300 cm x 200 cm, plus two support puncheons of height 100 cm. 6

7 The text included in the generic notice board is the following: The project Zeolife was designed to test an innovative integrated cycle of the zeolitites, with the purpose of decreasing the contribution of nitrogen fertilizers and water irrigation in agriculture, resulting in reduction of nitrate pollution and use of water resources. The zeolitite is a rock of volcanic origin, then a natural material, rich of zeolite minerals with high cation exchange capacity when immersed in a solution. The used zeolitites, coming from a quarry in central Italy (Sorano, GR), are naturally rich in potassium and water, and are "loaded" with NH4 + (ammonium ion, which, oxidized to nitrate form, becomes a source of nitrogen for plants) thanks to contact with pig slurry. After the treatment also such sewage also are poorer in ammonium and therefore more easily disposable. Sparse in right quantity in agricultural fields, the zeolitites loaded with NH4 + act as a slow release fertilizer: they are not washed away by rains, but give the nutrients only in contact with the roots of plants, improving productive yields and avoiding the dispersion of nitrogen in the surface and deep water system. The correction of farmland with zeolitite can also represent a defense against desertification caused by climate change and overexploitation of the soil. Zeolites in fact contain water in the crystal grid and the chemical changes that trigger with humic acids allow the solubilization of phosphates, primarily responsible for the formation of hard crusts that prevent infiltration of water. 7

8 The graphic image of the experimental field specific notice-board. 8

9 The text included in the experimental field specific notice board is the following: The zeolitites are natural volcanic rocks containing more than 50% of zeolite, a type of mineral with unique physical and chemical properties (high and selective cation exchange capacity: Cation Exchange Capacity or CEC; molecular absorption; reversible dehydration). The zeolites are able to capture NH4 + (ammonium ion) from the solutions and subsequently release it to the roots of the plants in a gradual manner. The characteristics of zeolitites and their ability to adjust the water content in soils allow a reduction in both the quantity of fertilizer and the quantity of water normally used for irrigation. The project proposes the experiment in open field, by Codigoro in the province of Ferrara, of the integrated cycle of zeolitites, for two years of cultivation (sorghum-corn). The experimental field was divided into six plots: two of these are cultivated in a traditional way; in two other zeolitite is added in the natural state and fertirrigation will be reduced by 20 and 40% in proportion to the quantities of zeolitite used. The zeolitite loaded with ammonium in the prototype is added in a further area, where it will release the nutrient only for cation exchange, induced by humic acids of plant roots and in proportion to the real needs of the crops. Here fertirrigation will be reduced by over 50%. The last plot is left uncultivated in the first year, and will be used in the second year of cultivation. Direct consequence of the use of zeolitite in agriculture is the reduction of nitrate load that is placed in the water system and watersaving irrigation. The reduction in the amount of nitrogen in the hydrogeological system is verified creating a hydro-geochemical budget that takes into account the quantity and quality of water in and out of the camp, with monitoring of the chemical composition of the soil, pore waters, ground waters and surface waters (drains and collector channels), for the entire duration of the trial.

10 The graphic image of the prototype specific notice-board. LIFE Project code: LIFE+10 ENV/IT/ Action 8b Parco Delta - Deliverable

11 The text included in the prototype specific notice board is the following: CATION-EXCHANGE OF ZEOLITE In the structure of the zeolites, the compensator cations (Na, K, Ca, etc.) present in channels and cavities are linked to the tetrahedral scaffold by forces not big enough to prevent their escape if the zeolite is in contact with a solution containing cations able to replace them, therefore involving the same number of positive charges. If, for example, a zeolite containing Na is put in contact with a solution containing NH4 (eg. a zootecnical slurry), the zeolite Na goes into solution being replaced within the structure by NH4 until equilibration between the composition of the zeolite and the one of the solution. The project ZeoLIFE experiences an integrated cycle of zeolitites in order to reduce the use of water and fertilizers in agriculture. The selected zeolitites are volcanic rocks containing more than 60% of zeolites of the type chabasite, a mineral naturally rich in potassium and water, and having particular physicchemical properties, such as doffing and selective ability to exchange cations (Cation Exchange Capacity or CEC) and reversible dehydration. Immersed in a liquid rich in ammonium ion (NH4 +) as the pig slurry, this mineral is able to capture it within its crystal lattice. In this way the ammonium content of the slurry will became lower and the zeolitite will be enriched with nitrogen, which can subsequently be released to the roots of the plants in a gradual manner. In this project the zeolitite is used in the form of fine sand (<3 mm), recovered from the processing waste of a brick quarry of Central Italy (Sorano, GR). Laboratory tests allowed us to identify a method of loading and determine the optimal parameters (ratio zeolitite/slurry, particle size of the material, stirring and rest time) so that the zeolitite capture the greatest possible amount of NH4. These parameters are used in the prototype built to produce loaded zeolitite on a large scale. The prototype consists of a cylindrical tank in which the zeolitite is introduced together with the slurry pumped from the second storage tank of the breeding wastewater. Inside the tank a mechanical vertical agitator stirs the material bringing the zeolitite in suspension which is then allowed to settle to achieve the balance of the exchange reaction. At the end of the process the slurry is re-entered back into the first storage tank, while the zeolitite enriched in ammonium is unloaded at the base of the tank on a vibrating screen which allows the separation of the residual liquid from the solid, which is then accumulated in a special container. The zeolitite is then ready to be spread in the experimental field and buried by plowing. A daily cycle can produce an average of 300 kg of zeolitite loaded with ammonium.

12 LIFE Project code: LIFE+10 ENV/IT/ Action 8b Parco Delta - Deliverable 2. ROLL-UPS The indoor roll-up distributed to each project s partner, which measures cm 100 x cm

13 Here is the text included in the indoor roll-up: The project ZeoLIFE was designed to test an innovative integrated cycle of zeolitites, whose purpose is to reduce the content of NH4 in the sewage produced by livestock and correct agricultural soils, with a consequent increase of the harvest and saving of water for irrigation and fertilizers, leading to a reduction of pollution of freshwater and groundwater and of over-exploitation of water resources. The project s propose is the testing in open field (periphery of Codigoro, FE) of the integrated cycle of zeolites, for two years of cultivation. It is planned the realization of a prototype for the treatment of pig slurry: the zeolitite, once reached the cation balance with the sewage, will be removed and added to an experimental parcel of farmland, where it will release the nutrient NH4 only when the roots of plants require it, without suffering the effects of washout. The zeolitites are natural rocks that contain more than 50% of zeolite, a type of mineral with unique physical and chemical properties, such as high and selective cation exchange capacity, molecular absorption and reversible dehydration. The zeolitites are able to take NH4 from the solutions and of releasing it gradually to the roots of plants. 13

14 Photos of the indoor roll-up exposed by the annual international fair Slow Fish held in Genova, Ancient Port, from 9 to 12 may

15 2. FLAGS The graphic image of the Zeolife project s flag, realized in outdoor canvas, with dimensions 160 cm x 110 cm. An image of the project s flag. 15

16 2. PLATES The graphic image of the Zeolife project s plate, which measures 40 cm x 30 cm. 16

17 The Zeolife project s plate handed to every partner - exposed by the entrance of the seat of the partner Ente di Gestione per i Parchi e la Biodiversità-Delta del Po. 17

Soils. Source: Schroeder and Blum, 1992

Soils. Source: Schroeder and Blum, 1992 Soils Source: Schroeder and Blum, 1992 Literature cited: Schroeder, D. and Blum, W.E.H. 1992. Bodenkunde in Stichworten. Gebrüder Borntraeger, D-1000 Berlin. Geology and Life Conceptual model Source: Knight,

More information

Only healthy soil can grow a nutrient dense food. You are what you eat!

Only healthy soil can grow a nutrient dense food. You are what you eat! Understanding How Cation Nutrients & Soil Structure are Related By Michael Martin Meléndrez Only healthy soil can grow a nutrient dense food. You are what you eat! Soil Must be able to hold onto water,

More information

Agricultural Fertilizer Applicator Soil Test Results What the heck do they mean?

Agricultural Fertilizer Applicator Soil Test Results What the heck do they mean? Agricultural Fertilizer Applicator Soil Test Results What the heck do they mean? Northeast Ohio Pesticide Safety Education Program Lee Beers, OSU Extension Trumbull County beers.66@osu.edu 330-638-6783

More information

List of Equipment, Tools, Supplies, and Facilities:

List of Equipment, Tools, Supplies, and Facilities: Unit D: ph of Soil Lesson 2: Identifying ph Connection With Plant Growth Student Learning Objectives: Instruction in this lesson should result in the students achieving the following objectives: 1. Explain

More information

Adsorption of ions Ion exchange CEC& AEC Factors influencing ion

Adsorption of ions Ion exchange CEC& AEC Factors influencing ion Adsorption of ions Ion exchange CEC& AEC Factors influencing ion exchange- Significance. Adsorption of ions Ion adsorption and subsequent exchange are important processes that take place between soil colloidal

More information

Lecture 14: Cation Exchange and Surface Charging

Lecture 14: Cation Exchange and Surface Charging Lecture 14: Cation Exchange and Surface Charging Cation Exchange Cation Exchange Reactions Swapping of cations between hydrated clay interlayers and the soil solution Also occurs on organic matter functional

More information

CLASS EXERCISE 5.1 List processes occurring in soils that cause changes in the levels of ions.

CLASS EXERCISE 5.1 List processes occurring in soils that cause changes in the levels of ions. 5 SIL CHEMISTRY 5.1 Introduction A knowledge of the chemical composition of a soil is less useful than a knowledge of its component minerals and organic materials. These dictate the reactions that occur

More information

Shirley E. Clark, Ph.D., P.E., D. WRE Robert E. Pitt, Ph.D., P.E., BCEE, D. WRE

Shirley E. Clark, Ph.D., P.E., D. WRE Robert E. Pitt, Ph.D., P.E., BCEE, D. WRE Shirley E. Clark, Ph.D., P.E., D. WRE Robert E. Pitt, Ph.D., P.E., BCEE, D. WRE Current PA Guidance Many guidance documents apply expected pollutant removals based on literature. However, typically presented

More information

TREATMENT OF LANDFILL LEACHATE USING ZEOLITE

TREATMENT OF LANDFILL LEACHATE USING ZEOLITE TREATMENT OF LANDFILL LEACHATE USING ZEOLITE Grant Redvers and Renate Timm (City Design Ltd), Garry Peters (Auckland City Council) and Craig Mowatt (NZ Natural Zeolite Ltd) Introduction City Design Ltd,

More information

FOR Soil Quality Report 2017

FOR Soil Quality Report 2017 Student Name: Partner Name: Laboratory Date: FOR 2505 - Soil Quality Report 2017 Objectives of this report: 10 Marks Lab Objectives Section Principles behind methods used to determine soil base cation

More information

Plant Nutrition and Transport. Chapter 29

Plant Nutrition and Transport. Chapter 29 Plant Nutrition and Transport Chapter 29 Overview: Underground Plants The success of plants depends on their ability to gather and conserve resources from their environment. The transport of materials

More information

SST3005 Fundamentals of Soil Science LAB 5 LABORATORY DETERMINATION OF SOIL TEXTURE: MECHANICAL ANALYSIS

SST3005 Fundamentals of Soil Science LAB 5 LABORATORY DETERMINATION OF SOIL TEXTURE: MECHANICAL ANALYSIS LAB 5 LABORATORY DETERMINATION OF SOIL TEXTURE: MECHANICAL ANALYSIS Learning outcomes The student is able to: 1. Separate soil particles : sand, silt and clay 2. determine the soil texture class using

More information

Cation Exchange Capacity, CEC

Cation Exchange Capacity, CEC Cation Exchange Capacity, CEC The basic building blocks of clay minerals are: silicon atoms surrounded by four oxygen atoms (tetrahedra), and aluminium atoms surrounded by six hydroxide groups (dioctahedra),

More information

Pepper cultivation on a substrate consisting of soil, natural zeolite and olive mill waste sludge-changes in soil properties

Pepper cultivation on a substrate consisting of soil, natural zeolite and olive mill waste sludge-changes in soil properties Pepper cultivation on a substrate consisting of soil, natural zeolite and olive mill waste sludge-changes in soil properties S. Kosmidis 1, M. K. Doula 2, A. Assimakopoulou 1, Ch. Kolovos 2, Y. Troyanos

More information

Effect of Heat Treatment on Phosphate Sorption by Soils from Different Ecologies

Effect of Heat Treatment on Phosphate Sorption by Soils from Different Ecologies Effect of Heat Treatment on Phosphate Sorption by Soils from Different Ecologies 1* Aghedo, J.E., 2 Ukpebor, E. and 3 Oviasogie, P.O., 4 Omorogbe, S.O. 1Department of Chemistry, College of Education, Ekiadolor,

More information

Section 1: Weathering and Soil Formation. We will study some of the processes that contribute to soil formation

Section 1: Weathering and Soil Formation. We will study some of the processes that contribute to soil formation Section 1: Weathering and Soil Formation We will study some of the processes that contribute to soil formation ***Minerals form rocks. The decomposition of rocks and minerals will form soil. Minerals are

More information

Carbon Cycling Internal

Carbon Cycling Internal Carbon Cycling Internal The 4 subcycles Atmosphere The Earth s Atmosphere The Earth has a radius of some 6400 km. Ninety-nine percent of the earth's atmosphere is contained within a layer approximately

More information

Water & Wastewater Mixing (WWM)

Water & Wastewater Mixing (WWM) Water & Wastewater Mixing (WWM) Steve Bungay October 2011 BHR Group offer Research Consultancy Product development in the field of Water, Environment and Power (WEP) With a multi-disciplinary team covering

More information

Storm Sewer Design [2]

Storm Sewer Design [2] Class 5 [1] Storm Sewer Design 9. Check Q < Qf and Vmax > vf > Vmin. Vmin is normally specified to avoid sedimentation. This will normally be 1.0 m/s at pipe full condition. (BS EN 752 suggests that for

More information

Application of Nitrogen and Oxygen Isotopes to Identify Sources of Nitrate

Application of Nitrogen and Oxygen Isotopes to Identify Sources of Nitrate Application of Nitrogen and Oxygen Isotopes to Identify Sources of Nitrate Illinois Groundwater Consortium Conference April 9, 2001 George S. Roadcap, Illinois State Water Survey Keith C. Hackley, Illinois

More information

Earth: An Introduction to Physical Geology Weathering and Soil

Earth: An Introduction to Physical Geology Weathering and Soil Chapter 6 Lecture Earth: An Introduction to Physical Geology Eleventh Edition Weathering and Soil Tarbuck and Lutgens Weathering Weathering involves the physical breakdown and chemical alteration of rock

More information

Sun. Photosynthesis (performed by plants, algae, and some bacteria) Respiration (performed by all organisms) 6 O 2 6 CO 2.

Sun. Photosynthesis (performed by plants, algae, and some bacteria) Respiration (performed by all organisms) 6 O 2 6 CO 2. Photosynthesis (performed by plants, algae, and some bacteria) Sun 6 O 6 CO 6 H O C 6 H O 6 (glucose) Solar energy + 6 H O + 6 CO C 6 H O 6 + 6 O Energy Respiration (performed by all organisms) 6 O 6 CO

More information

Soil Fertility. Fundamentals of Nutrient Management June 1, Patricia Steinhilber

Soil Fertility. Fundamentals of Nutrient Management June 1, Patricia Steinhilber Soil Fertility Fundamentals of Nutrient Management June 1, 2010 Patricia Steinhilber Ag Nutrient Management Program University of Maryland College Park Main Topics plant nutrition functional soil model

More information

STUDY GUIDE FOR CONTENT MASTERY. Surface Water Movement

STUDY GUIDE FOR CONTENT MASTERY. Surface Water Movement Surface Water SECTION 9.1 Surface Water Movement In your textbook, read about surface water and the way in which it moves sediment. Complete each statement. 1. An excessive amount of water flowing downslope

More information

Mechanical Weathering

Mechanical Weathering Weathering is the disintegration and decomposition of material at or near the surface. Erosion is the incorporation and transportation of material by a mobile agent, usually water, wind, or ice. Geologists

More information

Chapter 6. Weathering, Erosion, and Soil

Chapter 6. Weathering, Erosion, and Soil Chapter 6 Weathering, Erosion, and Soil Introduction Rocks and minerals disintegrate and decompose by the processes of physical and chemical weathering. This breakdown occurs because the parent material

More information

Clinoptilolite in Drinking Water Treatment for Ammonia Removal H. M. Abd El-Hady, A. Grünwald, K. Vlčková, J. Zeithammerová

Clinoptilolite in Drinking Water Treatment for Ammonia Removal H. M. Abd El-Hady, A. Grünwald, K. Vlčková, J. Zeithammerová Acta Polytechnica Vol. 41 No.1/21 Clinoptilolite in Drinking Water Treatment for Ammonia Removal H. M. Abd El-Hady, A. Grünwald, K. Vlčková, J. Zeithammerová In most countries today the removal of ammonium

More information

Precision Ag Services

Precision Ag Services Precision Ag Services PRECISION AGRICULTURE SERVICES AVAILABLE Yield Mapping, Data Analysis, Data Storage, Data Processing The key to precision agriculture is the data. Many systems and software packages

More information

Removal of suspended and dissolved organic solids

Removal of suspended and dissolved organic solids Removal of suspended and dissolved organic solids Types of dissolved solids The dissolved solids are of both organic and inorganic types. A number of methods have been investigated for the removal of inorganic

More information

NEW DIAGRAM USEFUL FOR CLASSIFICATION OF GROUNDWATER QUALITY

NEW DIAGRAM USEFUL FOR CLASSIFICATION OF GROUNDWATER QUALITY NEW DIAGRAM USEFUL FOR CLASSIFICATION OF GROUNDWATER QUALITY Elhag A.B Department of Civil Engineering, College of Engineering, King Khalid University, Saudi ABSTRACT: Due to human and human activities

More information

NITROGEN AND ITS COMPOUNDS Q30 (i) Explain how the following would affect the yield of ammonia. An increase in (i). Pressure.

NITROGEN AND ITS COMPOUNDS Q30 (i) Explain how the following would affect the yield of ammonia. An increase in (i). Pressure. NAME SCHOOL INDEX NUMBER DATE NITROGEN AND ITS COMPOUNDS 1. 1990 Q30 (i) Explain how the following would affect the yield of ammonia. An increase in (i). Pressure. (2 marks) marks)... (ii) Temperature

More information

Weathering and Soil Formation. Chapter 10

Weathering and Soil Formation. Chapter 10 Weathering and Soil Formation Chapter 10 Old and New Mountains The Appalachian Mountains appear very different from the Sierra Mountains. The Appalachians are smaller, rounded, gently sloping, and covered

More information

Helen M. Lang West Virginia University

Helen M. Lang West Virginia University Zeolites and their Applications Helen M. Lang West Virginia University Zeolite Mineralogy Zeolites are framework silicates, with a completely linked framework of tetrahedra, each consisting of 4 O 2- surrounding

More information

About me (why am I giving this talk) Dr. Bruce A. Snyder

About me (why am I giving this talk) Dr. Bruce A. Snyder Ecology About me (why am I giving this talk) Dr. Bruce A. Snyder basnyder@ksu.edu PhD: Ecology (University of Georgia) MS: Environmental Science & Policy BS: Biology; Environmental Science (University

More information

Igneous rocks + acid volatiles = sedimentary rocks + salty oceans

Igneous rocks + acid volatiles = sedimentary rocks + salty oceans The Lithosphere Weathering physical processes chemical processes biological processes weathering rates Soil development soil formation processes types of soils and vegetation soil properties physical chemical

More information

Chapter 8 Earth Systems and Resources

Chapter 8 Earth Systems and Resources Chapter 8 Earth Systems and Resources Earth s resources were determined when the planet formed. The Earth s Crust Layers Core: innermost zone of the planet, largely nickel and iron. Mantle: above the core,

More information

Chapter 11. Rivers: Shaping our landscape

Chapter 11. Rivers: Shaping our landscape Chapter 11 Rivers: Shaping our landscape Learning outcomes In this presentation you will learn: Common terms associated with rivers About the three stages of a river About the processes of river erosion

More information

15. GRIT CHAMBER 15.1 Horizontal Velocity in Flow Though Grit Chamber

15. GRIT CHAMBER 15.1 Horizontal Velocity in Flow Though Grit Chamber 15. GRIT CHAMBER Grit chamber is the second unit operation used in primary treatment of wastewater and it is intended to remove suspended inorganic particles such as sandy and gritty matter from the wastewater.

More information

APPLICATION OF METAKAOLIN GEOPOLYMER FOR AMMONIUM REMOVAL IN SMALL-SCALE WASTEWATER TREATMENT SYSTEMS

APPLICATION OF METAKAOLIN GEOPOLYMER FOR AMMONIUM REMOVAL IN SMALL-SCALE WASTEWATER TREATMENT SYSTEMS APPLICATION OF METAKAOLIN GEOPOLYMER FOR AMMONIUM REMOVAL IN SMALL-SCALE WASTEWATER TREATMENT SYSTEMS Tero Luukkonen, Kateřina VĕžnÍková, Emma-Tuulia Tolonen, Hanna Runtti, Juho Yliniemi, Tao Hu, Kimmo

More information

Biogeochemical cycles

Biogeochemical cycles Lecture -2: Biogeochemical cycles ENV 107: Introduction to Environmental Science Dr. A.K.M. Saiful Islam Case Study: Lake Washington The city of Seattle, USA lies between two major bodies of water- saltwater

More information

Gain a better understanding of soil ph and how it is measured. Understand how lime requirement is determined.

Gain a better understanding of soil ph and how it is measured. Understand how lime requirement is determined. LABORATORY 7 SOIL REACTION (ph) AND LIME REQUIREMENT I Objectives Gain a better understanding of soil ph and how it is measured. Understand how lime requirement is determined. II Introduction A Soil Reaction

More information

6. What instrument does a geologist use to record the motions produced by an earthquake?

6. What instrument does a geologist use to record the motions produced by an earthquake? Name: Date: 1. Which human activity does NOT help control water runoff? A. contour plowing B. planting crops C. building flood control dams D. paving with asphalt 2. Which is NOT an effect of sewage put

More information

Shirley E. Clark, Ph.D., P.E., D. WRE Penn State Harrisburg. Robert Pitt, Ph.D., P.E., BCEE, D. WRE University of Alabama

Shirley E. Clark, Ph.D., P.E., D. WRE Penn State Harrisburg. Robert Pitt, Ph.D., P.E., BCEE, D. WRE University of Alabama Shirley E. Clark, Ph.D., P.E., D. WRE Penn State Harrisburg Robert Pitt, Ph.D., P.E., BCEE, D. WRE University of Alabama Site Stormwater Characteristics and Permit Limits Analytes on Permit 90 th percentile

More information

Lecture 15: Adsorption; Soil Acidity

Lecture 15: Adsorption; Soil Acidity Lecture 15: Adsorption; Soil Acidity Surface Complexation (Your textbook calls this adsorption ) Surface Complexation Both cations and anions can bind to sites on the external surfaces of soil minerals

More information

ENVIRONMENTAL SCIENCE

ENVIRONMENTAL SCIENCE Advanced Placement ENVIRONMENTAL SCIENCE Geologic Processes & Soil Student 2014 Geologic Processes and Soil Geologic Processes The age of Earth is best measured by the geologic time scale. The idea that

More information

Permeable Treatment Wall Project

Permeable Treatment Wall Project West Valley Demonstration Project West Valley Environmental Services Permeable Treatment Wall Project 20614_1 John Chamberlain May 26, 2010 West Valley Citizen Task Force Meeting West Valley Demonstration

More information

Advanced TRS - ZEOLITE IN A COLLOIDAL SUSPENSION

Advanced TRS - ZEOLITE IN A COLLOIDAL SUSPENSION Advanced TRS - ZEOLITE IN A COLLOIDAL SUSPENSION The need for this product is summarized in the following graphic Since this data was collected the numbers of deaths have gone up yearly. 25 MARCH 2014

More information

Sustainable Energy Science and Engineering Center GEOTHERMAL ENERGY. Sustainable Energy Sources. Source:

Sustainable Energy Science and Engineering Center GEOTHERMAL ENERGY. Sustainable Energy Sources. Source: Sustainable Energy Sources GEOTHERMAL ENERGY Earth s Temperature Profile GEOTHERMAL ENERGY Plate Tectonics Earth's crust is broken into huge plates that move apart or push together at about the rate our

More information

Template for Sediment and Erosion Control Plan General Instructions. Section Instructions

Template for Sediment and Erosion Control Plan General Instructions. Section Instructions Template for Sediment and Erosion Control Plan General Instructions Introduction: Soil erosion and sediment deposition from farmlands can contribute to degraded surface water quality. Sediment delivery

More information

Lidia Sas Paszt The Rhizosphere Laboratory, Research Institute of Horticulture, Skierniewice, Poland,

Lidia Sas Paszt The Rhizosphere Laboratory, Research Institute of Horticulture, Skierniewice, Poland, Lidia Sas Paszt lidia.sas@inhort.pl The Rhizosphere Laboratory, Research Institute of Horticulture, Skierniewice, Poland, www.inhort.pl - Research on the role of roots & rhizosphere in growth & yelding

More information

ANALYSIS OF THE ZEOLITE VOLCANIC TUFFS FROM CLUJ COUNTY, ROMANIA

ANALYSIS OF THE ZEOLITE VOLCANIC TUFFS FROM CLUJ COUNTY, ROMANIA Proceedings of the 13 th International Conference of Environmental Science and Technology Athens, Greece, 5-7 September 2013 ANALYSIS OF THE ZEOLITE VOLCANIC TUFFS FROM CLUJ COUNTY, ROMANIA C.A. DOBOCAN

More information

Radionuclide Migration: Prediction Experience

Radionuclide Migration: Prediction Experience Radionuclide Migration: Prediction Experience V.V. Martianov, M.Yu. Sheglov, A.V. Guskov State Unitary Enterprise MosSIA Radon 2/14, 7th Rostovsky pereulok, Moscow 119121 Russia ABSTRACT Many different

More information

Crows Landing Naval Base Easement

Crows Landing Naval Base Easement 1 of 15 West Stanislaus Resource Conservation District Crows Landing Naval Base Easement Annual Reserve Monitoring Report Jamie McFarlin 11/112012 2 of 15 West Stanislaus Resource Conservation District

More information

Volume Composition of a Desirable Surface Soil

Volume Composition of a Desirable Surface Soil Soil Chemistry Volume Composition of a Desirable Surface Soil 50% pore space 25% air 45 to 48% mineral matter 50% solid material 25% water 2 to 5% organic matter Soil Organic Matter Soil organic matter:

More information

Questions. 1. What kind of radiation dominates the first phase of radiation emission from a nuclear fireball?

Questions. 1. What kind of radiation dominates the first phase of radiation emission from a nuclear fireball? Questions 1. What kind of radiation dominates the first phase of radiation emission from a nuclear fireball? 2. What is the ignition temperature of wood? 3. What fuels a firestorm? Natural Radioactivity

More information

Circle the best answer for each question. There are a total of 50 questions.

Circle the best answer for each question. There are a total of 50 questions. Winter Packet 2013 Name Period ircle the best answer for each question. There are a total of 50 questions. 1. What occurs when ions from the Sun hit air molecules and cause them to emit vivid colors of

More information

Portland Water Bureau. Preparing Portland s Water Supply for The Big One. July 11, Tim Collins, P.E., G.E.

Portland Water Bureau. Preparing Portland s Water Supply for The Big One. July 11, Tim Collins, P.E., G.E. Portland Water Bureau Preparing Portland s Water Supply for The Big One July 11, 2018 Tim Collins, P.E., G.E. Presentation Outline Portland water system overview Pacific Northwest seismic hazards Building

More information

Nutrient Cycling in Land Vegetation and Soils

Nutrient Cycling in Land Vegetation and Soils Nutrient Cycling in Land Vegetation and Soils OCN 401 - Biogeochemical Systems 15 September 2016 Reading: Schlesinger & Bernhardt, Chapter 6 2016 Frank Sansone Outline 1. The annual Intrasystem Nutrient

More information

2010 Crop Year Fertilizer Report

2010 Crop Year Fertilizer Report 2010 Crop Year Fertilizer Report This report is based on the tonnage of fertilizer reported from licensed dealers that has been either distributed OR sold in Minnesota 1. Each registrant under section

More information

Study of Particle Granularity Impact on Nutrient Concentration

Study of Particle Granularity Impact on Nutrient Concentration A publication of 2161 CHEMICAL ENGINEERING TRANSACTIONS VOL. 32, 2013 Chief Editors: Sauro Pierucci, Jiří J. Klemeš Copyright 2013, AIDIC Servizi S.r.l., ISBN 978-88-95608-23-5; ISSN 1974-9791 The Italian

More information

Lithosphere. Solid shell of the Earth, consists of crust and upper mantle The lithosphere includes things like:

Lithosphere. Solid shell of the Earth, consists of crust and upper mantle The lithosphere includes things like: Lithosphere Lithosphere Solid shell of the Earth, consists of crust and upper mantle The lithosphere includes things like: Rocks, minerals, soil Mountains Plains Volcanoes Essential to Life The lithosphere

More information

Name Date Class. Directions: Use the diagram below to answer question Florida Progress Monitoring and Benchmark Assessments

Name Date Class. Directions: Use the diagram below to answer question Florida Progress Monitoring and Benchmark Assessments b e n c h m a r k t e s t : e a r t h a n d s p a c e s c i e n c e Multiple Choice 1. Geologists obtain indirect evidence about Earth s interior by A measuring pressure differences at Earth s surface.

More information

Soil - the battery of your business

Soil - the battery of your business Soil - the battery of your business By DAVID HANLON The basis of our farm business is the soil and increasingly all growers are focusing their attention on this vital resource. Just what state it is in

More information

Development and Test of Potassium Management Algorithms for Corn. Ron Potok (Solum), Kyle Freeman (Mosaic), and Scott Murrell (IPNI) Project Summary:

Development and Test of Potassium Management Algorithms for Corn. Ron Potok (Solum), Kyle Freeman (Mosaic), and Scott Murrell (IPNI) Project Summary: Development and Test of Potassium Management Algorithms for Corn Ron Potok (Solum), Kyle Freeman (Mosaic), and Scott Murrell (IPNI) Project Summary: In our 1 year project spanning April 2013 Feb 2014,

More information

Soils and Soil Minerals. Remember, most things can be too little or too much.

Soils and Soil Minerals. Remember, most things can be too little or too much. Soils and Soil Minerals Remember, most things can be too little or too much. 1 2 3 Source of essential elements CO 2, O 2 from atmosphere H 2 0, O 2, minerals from soil NH 4, SO 4 can volatilize and be

More information

AP ENVIRONMENTAL SCIENCE 2013 SCORING GUIDELINES [14 pt space] Question 1

AP ENVIRONMENTAL SCIENCE 2013 SCORING GUIDELINES [14 pt space] Question 1 AP ENVIRONMENTAL SCIENCE 2013 SCORING GUIDELINES [14 pt space] Question 1 (a) Identify TWO human activities that alter the natural flow of sediments into Gulf Coast ecosystems. Explain how each of the

More information

Catastrophic Events Impact on Ecosystems

Catastrophic Events Impact on Ecosystems Catastrophic Events Impact on Ecosystems Hurricanes Hurricanes An intense, rotating oceanic weather system with sustained winds of at least 74 mph and a welldefined eye Conditions for formation: Warm water

More information

Mehlich and Modified Mehlich Buffer for Lime Requirement

Mehlich and Modified Mehlich Buffer for Lime Requirement Mehlich and Modified Mehlich Buffer for Lime Requirement David H. Hardy Application and Principle The development of the Mehlich buffer was to estimate acidity actually affecting plant growth in North

More information

Soil gas and gas flux baselines

Soil gas and gas flux baselines Soil gas and gas flux baselines Regional and site-scale baseline surveys of near- surface gas geochemistry parameters Understanding natural variability as a framework for monitoring programs and public

More information

Rocks and Weathering

Rocks and Weathering Rocks and Weathering The Effects of Weathering The process of mountain building thrusts rock up to Earth s surface. Weathering is the process that breaks down rock and other substances at Earth s surface.

More information

Erosion and Deposition

Erosion and Deposition CHAPTER 3 LESSON 2 Erosion and Deposition Landforms Shaped by Water and Wind Key Concepts What are the stages of stream development? How do water erosion and deposition change Earth s surface? How do wind

More information

Soil Colloidal Chemistry. Compiled and Edited by Dr. Syed Ismail, Marthwada Agril. University Parbhani,MS, India

Soil Colloidal Chemistry. Compiled and Edited by Dr. Syed Ismail, Marthwada Agril. University Parbhani,MS, India Soil Colloidal Chemistry Compiled and Edited by Dr. Syed Ismail, Marthwada Agril. University Parbhani,MS, India 1 The Colloidal Fraction Introduction What is a colloid? Why this is important in understanding

More information

Automating Wet Chemical Analysis

Automating Wet Chemical Analysis Automating Wet Chemical Analysis Who Should Automate? Anyone looking to improve laboratory efficiency Environmental Agricultural Food and beverage Pharmaceutical Mining Etc. Advantages of Automating Save

More information

Weathering, Soil, and Mass Movements

Weathering, Soil, and Mass Movements Tarbuck Lutgens Weathering, Soil, and Mass Movements 5.1 Weathering Mechanical Weathering Mechanical weathering occurs when physical forces break rock into smaller and smaller pieces without changing the

More information

Fertilisers. Topic 12 National 5 Chemistry Summary Notes

Fertilisers. Topic 12 National 5 Chemistry Summary Notes Fertilisers LI 1 Topic 12 National 5 Chemistry Summary Notes Chemistry is extremely important to the future of food production. As the population of the world increases, more and more efficient ways of

More information

The Role of Soil Organic Matter in Potassium Fixation Nathan Smith

The Role of Soil Organic Matter in Potassium Fixation Nathan Smith The Role of Soil Organic Matter in Potassium Fixation Nathan Smith Undergraduate Research Assistant in Agronomy Senior in Agronomy and Environmental Science Iowa State University Soil Potassium (K + )

More information

2012 Crop Year Fertilizer Report

2012 Crop Year Fertilizer Report 2012 Crop Year Fertilizer Report This report is based on the tonnage of fertilizer reported from licensed dealers that has been either distributed OR sold in Minnesota. Fertilizer can be reported as distributed

More information

6.E E Rock Cycle/Weathering/Soil

6.E E Rock Cycle/Weathering/Soil Name: Date: 1. A lake is surrounded by hills covered with trees and shrubs. Which statement correctly describes how a change to the plants in this area will affect this environment? A. Adding plants to

More information

Satellite remote sensing and GIS used to quantify water input for rice cultivation (Rhône delta, France)

Satellite remote sensing and GIS used to quantify water input for rice cultivation (Rhône delta, France) 446 Remote Sensing and Hydrology 2000 (Proceedings of a symposium held at Sanla Fe, New Mexico, USA, April 2000). IAHS Publ. no. 267, 2001. Satellite remote sensing and GIS used to quantify water input

More information

MODULE 5.2 Soil properties

MODULE 5.2 Soil properties MODULE 5.2 Soil properties Exchangeable cations and cation exchange capacity 3 Acid - Base Ion Exchange Reaction In Soils 3 Anion retention 5 Soil Profile And Its Importance 7 Water, air and particles

More information

In the space provided, write the letter of the description that best matches the term or phrase. a. any form of water that falls to Earth s

In the space provided, write the letter of the description that best matches the term or phrase. a. any form of water that falls to Earth s Skills Worksheet Concept Review In the space provided, write the letter of the description that best matches the term or phrase. 1. condensation 2. floodplain 3. watershed 4. tributary 5. evapotranspiration

More information

Module 15 : Grit Chamber. Lecture 19 : Grit Chamber

Module 15 : Grit Chamber. Lecture 19 : Grit Chamber 1 P age Module 15 : Grit Chamber Lecture 19 : Grit Chamber 2 P age Grit chamber is the second unit operation used in primary treatment of wastewater and it is intended to remove suspended inorganic particles

More information

Particles in aqueous environments

Particles in aqueous environments Lecture 11 Particle-Aqueous Solute Interactions Today 1. Particle types and sizes 2. Particle charges 3. Particle-solute Interactions Next time Please continue to read Manahan Chapter 4. 1. Fresh-salt

More information

Chapter 37: Plant Nutrition - A Nutritional Network

Chapter 37: Plant Nutrition - A Nutritional Network Chapter 37: Plant Nutrition - A Nutritional Network Every organism continually exchanges energy and materials with its environment For a typical plant, water and minerals come from the soil, while carbon

More information

Lecture 2: Soil Properties and Groundwater Flow

Lecture 2: Soil Properties and Groundwater Flow ENGI 7718 Environmental Geotechniques ENGI 9621 Soil Remediation Engineering Lecture 2: Soil Properties and Groundwater Flow Spring 2011 Faculty of Engineering & Applied Science 1 2.1 Soil properties 2.1.1

More information

Changes to the Earth Study Guide

Changes to the Earth Study Guide Changes to the Earth Study Guide Earth has a core, crust, and mantle. The core is made of a solid inner region and a liquid outer region. The mantle is the middle layer of earth made up of molten rock.

More information

Let the Earth help us to save the Earth. R.D.Schuiling

Let the Earth help us to save the Earth. R.D.Schuiling Let the Earth help us to save the Earth R.D.Schuiling What has saved the Earth and provided the conditions for life? Annual CO2 emission of volcanoes is around 300 million tons a year 300 million tons

More information

EARTH S CHANGING SURFACE

EARTH S CHANGING SURFACE EARTH S CHANGING SURFACE Weathering Together, weathering and erosion work continuously to wear down the material on Earth s surface. weathering process that breaks down rock and other substances of Earth

More information

Weathering, Erosion & Soils Quiz

Weathering, Erosion & Soils Quiz Weathering, Erosion & Soils Quiz Multiple Choice Identify the choice that best completes the statement or answers the question. 1. The diagram below shows a cross-section of a rock layer. Erosion is the

More information

COMPUTER METHODS AND MODELING IN GEOLOGY THE GLOBAL PHOSPHORUS CYCLE

COMPUTER METHODS AND MODELING IN GEOLOGY THE GLOBAL PHOSPHORUS CYCLE COMPUTER METHODS AND MODELING IN GEOLOGY THE GLOBAL PHOSPHORUS CYCLE Phosphorous (P) is an essential nutrient for life. It is found in the RNA and DNA of all organisms, as well as in the adenosine triphosphate

More information

Lecture 13 More Surface Reactions on Mineral Surfaces. & Intro to Soil Formation and Chemistry

Lecture 13 More Surface Reactions on Mineral Surfaces. & Intro to Soil Formation and Chemistry Lecture 13 More Surface Reactions on Mineral Surfaces & Intro to Soil Formation and Chemistry 3. charge transfer (e.g., ligand/donor sorption): Sorption involves a number of related processes that all

More information

Weathering & Soil. Chpt 6

Weathering & Soil. Chpt 6 Weathering & Soil Chpt 6 Some important processes that break-down and transport solid material at the Earth s surface Weathering the physical breakdown and chemical decomposition of rock Mass wasting the

More information

Learning Objectives: I can identify and interpret river flows and directions.

Learning Objectives: I can identify and interpret river flows and directions. Learning Objectives: I can identify and interpret river flows and directions. Bellringer Review: Check for Understanding Questions: 1 2 What Are The Key Parts Of A River s Anatomy? In your data notebooks

More information

CONTENTS. Foreword... Summary (English, French, Russian, Spanish) 1. Introduction by R. Schneider

CONTENTS. Foreword... Summary (English, French, Russian, Spanish) 1. Introduction by R. Schneider CONTENTS Page Foreword............ IX Summary (English, French, Russian, Spanish) XI 1. Introduction by R. Schneider.. 1 1.1 1.1.1 1.1.2 1.1.3 1.1.4 1.1.5 1.1.6 1.2 1.2.1 1.2.2 1.2.3 The present position

More information

Welcome to GEO 101 Introduction to Geology

Welcome to GEO 101 Introduction to Geology Welcome to GEO 101 Introduction to Geology so what is Geology? not just rocks! Geology is... study of Earth and planetary bodies processes responsible for formation processes that modify all areas of geology

More information

9 Week Review Biology. Magnolia High School 2015

9 Week Review Biology. Magnolia High School 2015 9 Week Review Biology Magnolia High School 2015 What is the cellular process shown below? Phagocytosis The BEST choice to complete this concept map! Animal Cell or Plant Cell? PLANT Cell What is the function

More information

Soil physical and chemical properties the analogy lecture. Beth Guertal Auburn University, AL

Soil physical and chemical properties the analogy lecture. Beth Guertal Auburn University, AL Soil physical and chemical properties the analogy lecture. Beth Guertal Auburn University, AL Soil Physical Properties Porosity Pore size and pore size distribution Water holding capacity Bulk density

More information

Weathering, Erosion, Deposition, and Landscape Development

Weathering, Erosion, Deposition, and Landscape Development Weathering, Erosion, Deposition, and Landscape Development I. Weathering - the breakdown of rocks into smaller particles, also called sediments, by natural processes. Weathering is further divided into

More information

Source Pollution to Groundwater

Source Pollution to Groundwater This file was created by scanning the printed publication. Errors identified by the software have been corrected; however, some errors may remain. Consideration of Spatial Variability in the Management

More information

Acid Soil. Soil Acidity and ph

Acid Soil. Soil Acidity and ph Acid Soil Soil Acidity and ph ph ph = - log (H + ) H 2 O H + + OH - (H + ) x (OH - )= K w = 10-14 measures H + activity with an electrode (in the lab), solutions (in the field) reflects the acid intensity,

More information