Alginit essence of nature essence of future. Dr. Frank Gresens, Consultant of Alginit Kft., Budapest, Hungary

Similar documents
Soil Resources. Soil Horizons

Chapter 15 Soil Resources

Overview of Chapter 14

4/23/2018. Soil John Wiley & Sons, Inc. All rights reserved. Lecture 14

Loam: About 40% sand, 40% silt, 20% clay. Mixture of pore sizes to balance water retention and aeration. Considered the best soil for growing crops.

Unit 5: Soil - Stages of Soil formation

Unit 1 Lesson 5 Soil Formation. Copyright Houghton Mifflin Harcourt Publishing Company

CCA Exam Prep Intro to Soil & Water

Know Your Soil Getting the Dirt on Your Dirt FWAA. Dr. Steve Petrie Director of Agronomic Services

5.1 Introduction to Soil Systems IB ESS Mrs. Page

PASTURE AND HAY FIELDS: SOIL FUNDAMENTALS. Sanders County April 8, Clain Jones

Soils and plant nutrients

Great Soil-Great Gardens I Basic Soil Science Brad Park, Rutgers University Materials developed by: Karen A. Plumley, Ph.D.

Soils and Fertilizers. Leo Espinoza Soils Specialist

PROUDLY MADE IN AUSTRALIA

Introduction to Environmental Science. Soil Characteristics. Chapter 11 Soil

Soil 1/18/2012. Soils, Nutrients and Fertilizers Part I. Soil Profile

Soil is. Pieces of rock Minerals Decaying organic matter Water Air Living organisms All mixed together!

Understanding Your Virginia Soil Test Report

Soils. Nutrients needed by plants 10/21/2013. Consists of a series of layers called. Soils consists of: Topsoil (A horizon) upper most layer

THE FOREST NURSERY AND ITS SOILS

Components of Soil. Humus: (a carbon sink) Dark brown or black color indicates high nitrogen content.

Getting the Most out of Your Strawberry Soil Test Report. General Information

6 MAJOR SOIL FACTORS CONSIDERED IN LAND EVALUATION

MYCORRHIZA + MYCORRHIZA WITH WETTING AGENT WITH WETTING AGENT

Soil Fertility Note 14 Topsoil

Unit D: ph of Soil. Lesson : Identifying the ph Changes in Soil

NATURE OF SOILS OBJECTIVE:

Assessing and Amending Your Garden Soil Craig Cogger, Soil Scientist Emeritus Washington State University Puyallup

Understanding the Balance

Sunlight. Chlorophyll

Unlock your soil s potential with K-humate

Site Selection. The #1 Most Important Step in Planting Anything Soils a major component. Physical Characteristics. Chemical Composition

SOIL TESTS. Circular of Information 587 Revised September 1963 Agricultural Experiment Station, Oregon State University, Corvallis

Title: Lecture 16 Soil Water and Nutrients Speaker: Teresa Koenig Created by: Teresa Koenig, Kim Kidwell. online.wsu.edu

Unit 2: The Earth. Book: Chapter Barron: Chapter 1 Test: October 17/18

2016 Iowa FFA Soils Evaluation CDE Exam

Terms and Definitions. Characteristics and Qualities. Environmental Issues

SOIL BASICS & CONSERVATION

CLAY, SANDY AND PEAT SOILS, AND SOIL ORGANIC MATTER

Chapter 37. Plant Nutrition. AP Biology

Soils of Palau. Diversity and Fertility. Palau Livestock Management Workshop March 23-25, Jonathan Deenik, PhD University of Hawaii

POTTING SOIL VERMICULITE PEAT MOSS & SUBSTRATES PERLITE. Product Catalogue Horticultural

Master Composting Program. Sam Angima OSU Extension Lincoln County, Oregon

EDULABZ. Ans. (b) 7. The soft, porous layer with a good water-retaining capacity forms the

SOILS. Sam Angima. OSU Extension Agent Lincoln County, Oregon

SYM BIO INDUSTRIES SDN BHD INTRODUCTION OF SYM BIOGREEN NATURAL PLANT BIO ENHANCER

Urbanscape Landscaping Solutions

2018 Iowa FFA Soil Judging CDE Exam 1. Landscape positions characterizes the location of the soil on the landscape and identifies potential risks.

Chapter 2.2. Basic Soil-Plant Interactions. learning objectives

Site Selection. The #1 Most Important Step in Planting Anything Soils a major component. Physical Characteristics. Chemical Composition

CHECKLIST BMPs for FIELD NURSERIES REGULATIONS, SITE SELECTION, WATER MANAGEMENT

Soil Chemistry. Key Terms.

Soils and the Environment. A Summary of RI Envirothon Study Materials Compiled by Sally Paul

Saline and Sodic Field Demonstration project

27/01/2017. This event is being run by SAC Consulting. What is Soil?

Eco new farmers. Module 2 Soil and Nutrient Cycling. Section 1 Soils and soil fertility

Iowa FFA Soil Career Development Event 2008

Growing Better Houseplants. Potting Soil

STOCKOSORB for Water and Soil Management in Agriculture and Horticulture

A Plant & Soil Ecosystem

Special Assignment for Wednesday: Watch video on soil texture analysis

MIKSKAAR PROFESSIONAL POTTING SOIL

Inherent Factors Affecting Soil ph. Soil ph Management

Absorber products have the property of absorbing up to 500 times their weight in distilled water and they become gels.

Soil sampling & liming: Key steps in maintaining soil health

Global Soils. The Nature of Soil The Soil Water Balance Soil Development The Global Scope of Soils Global Climate Change and Agriculture

Plant Nutrition AP Biology

Management of Sodic Soils in Alberta

Soil & Fertilizer. Pam Brown, Extension Agent Emeritus, Gardening Coach

Managing Soils in Rangelands. Jerry Daigle

Slide 1: Welcome to today s From the Dirt Up presentation, where I ll be talking to you about the importance of soil testing and maintaining healthy

Inherent Factors Affecting Soil ph. Soil ph Management

NUTRIENT MANAGEMENT. PHOSPHORUS (P) is an essential element

This page intentionally left blank

Sandy Soils. Sand. Silt. Sandy soils. Silty soils. Wind blown and alluvial parent materials. Low water holding capacity

The Nature of Soil Soil Conservation Sustainable Ag.

EARTH SCIENCE CONCEPTS -Geologic time scale

Your Gardens Don t Have to be Thirsty!

Why is. Vermont Organics. soil the best choice you can make?

Potash Development Association ASSESSING SOIL FERTILITY; THE IMPORTANCE OF SOIL ANALYSIS AND ITS INTERPRETATION

Ecological Landscaping Association's 2013 Conference & Eco-Marketplace February 27, Geoff Kuter, Ph.D. Agresource Inc.

Class 3: Soil Sampling and Testing. Chris Thoreau

Learning Objectives. C. Owen Plank

Establish plants outdoors

Farmers need to develop an understanding

Plain Talk About Soil Chemistry. Plant nutrients must be dissolved in water. Dissolve-ability impacts availability.

Soils of Oahu. Outline. Soils and Plant Nutrient Supply 2/20/2014

3 From Bedrock to Soil

Soil Formation. 6.E.2.3 Explain how the formation of soil is related to the parent rock type and the environment in which it develops.

If your soil has a high salinity content, the plants

Soils 101: A practical approach. Kevin Marini UCCE Placer/Nevada Counties

DELHI PUBLIC SCHOOL TAPI

Soil testing Page 1. Contrary to what is widely believed, the colour of the soil reveals very little about its fertility.

STUDIES ON RETENTION CAPABILITY OF TREATED SOILS

GALLATIN GARDENER CLUB APRIL 6, Clain Jones

BIOSOL FORTE GENERAL DESCRIPTION MANUFACTURE: COMPOSITION: PROPERTIES:

NDSU. Soil Organic Matter and its Benefits

Learning Objectives Part 1. Chapter 4 Soil Physical Properties. Soil Physical Properties. Color. Physical properties part 1

DIRT! APES Laboratory Activity

Transcription:

Alginit essence of nature essence of future Dr. Frank Gresens, Consultant of Alginit Kft., Budapest, Hungary

Agenda Introduction What is Alginit Properties of Alginit Alginit - Research results Alginit - Application fields

Introduction Sweet water scarcity a worldwide problem Sweet water is rare, shortage is a main problem in arid and semiarid regions sweet water is one of the most important economic factors in developing countries the bulk of withdrawal of water accounts for agriculture (e.g. africa: 88%, asia:85%)

Introduction Soil fertility inadequate soil fertility is a problem (loose sandy soils and/or depleted soils with low water holding capacity, cation exchange capacity, organic matter content and micrcobial activity) these soils are leading to inefficient use and high loss rates of rare and expensive resources (e.g. sweet water, fertilisers)

Introduction What is needed? 1. sustainable ways for using the rare sweet water resources 2. solutions for better soil fertility A very good possibility for soil amelioration in a natural way is the addition of Alginit from Gérce to these kind of soils

What is Alginit Alginit is a naturally occuring mineral out of the family of oil shale It contains no inorganic additives or chemicals Sediment oil shale It developed from the mixture of fossil algae-biomass and eroded tuff 4-5 million years ago in the Pannonian lake system

What is Alginit Alginit from Gérce is composed by nature and contains: fossil" organic matter content: up to 19 % (fossil green alga Botryococcus braunii) mineral content: at least 81 % Clay content: up to 54 % Smectit: 50 % Illitt: 40 % Chlorit/Vermiculite: 10 % Silt content: 40 % Sand content: 6 % within the fractions of clay, silt and sand a CaCO 3 - content of up to 22 % is existing It contains macro- and microelements necessary for achieving optimum, balanced soil conditions

Properties of Alginit Water saving by reduction of evaporation and seepage 1 t of Alginit is able to store at least 630 l water of which 410 l are in any case plant available Reduction of water demand

Properties of Alginit Long-term storage capacity of nutrients CEC of 35 cmol kg -1 Decreases leaching out of nutrients Decreases fertiliser demand

Properties of Alginit Outstanding improvement in soil quality (soil amelioration) Addition of nutrients Stimulation of root growth Formation of clay-humus complexes Stabilization of soil structure Minimization of erosion potential

Root number (n) and root mass (g F.M./pot) Alginit research 90 80 70 Result: 60 30 20 results Greenhouse pot experiment (University of Bonn and experimental station Kamperhof, H+K Kalke, Germany) Different Alginit dosages on a sandy soil Culture: spinach, two water levels (70% and 30% FC) Root number Root fresh matter More root mass (+ 60%) 50 More root numbers (+ 307%) 40 Finer roots 10 0 Alginit 0 % Alginit 10 % Alginit 15 % Alginit 20 % 1 2 3 1 2 3 1 2 3 1 2 3 Liming level

Exchangeabel Cations (mmolc/100 g) Alginit research results Greenhouse pot experiment (University of Bonn and experimental station Kamperhof, H+K Kalke, Germany) 50,0 45,0 Ca effective CEC 40,0 Result: 35,0 30,0 effective CEC growht by a factor of 19 25,0 the main exchangeable element is 20,0 Calcium 15,0 10,0 Alginit 0% Alginit 10% Alginit 15% Alginit 20% 5,0 0,0 1 2 3 1 2 3 1 2 3 1 2 3 Liming level

Alginit research results Greenhouse pot experiment (University of Bonn and experimental station Kamperhof, H+K Kalke, Germany) Spinach fresh matter Spinach dry matter watering level Additional yield % 10 % Alginit 15 % Alginit 20 % Alginit 70 % FC + 4 + 8 + 8 30 % FC + 16 + 9 + 13 70 % FC + 15 + 22 + 25 30 % FC + 29 + 26 + 33 Result: more yield by application of Alginit especially under water stress

Alginit research results Field experiment, Cairo, Egypt (University of Cairo) Treatments control I 10 I 20 II 10 II 20 III 10 III 20 Different Alginit dosages on a sandy soil Culture: grass for landscaping F.C (Vol. % at 0.1 atm.) 8.2 8.9 8.7 11.0 10.6 13.3 12.6 max. retained water (m 3 / ha) 245.5 266.0 261.0 330.0 318.1 399.0 377.1 Increasing quantity (m 3 / ha) 20.5 15.5 84.5 72.6 153.5 131.6 10.0 I, II and III are the application rates of 4, 8 and 16 kg/m 2 of Alginit; 10, 20 are the depths of mixing into soil, F.C. = field capacity 0.0 Plant available water Vol. % Result: more water retention (+ 62.5%) more plant available water (+ 82%) 5.5 6.2 5.8 8.2 7.3 9.5

Root dry matter (g/m 2 ) Alginit research results Field experiment, Cairo, Egypt (University of Cairo) Influence of different Alginit application rates on root dry matter of Grass 1200 1100 1000 900 800 700 600 500 400 Control I II III Application rate of Alginit F 10 C 10 F 20 C 20 I, II and III are the application rates of 4, 8 and 16 kg/m 2 of Alginit; F=fine= Result: <2 mm Alginit particle size, C= coarse= 3-4 mm Alginit particle size; 10= 10 cm soil mixture depth, 20= 20 cm soil mixture More root DM (+ 81% in average) dept More root surface area and finer roots

Total dry matter (g/m 2 ) Alginit research results Field experiment, Cairo, Egypt (University of Cairo) Influence of different Alginit application rates on total dry matter (DM) production of Grass 1400 1300 1200 1100 1000 900 800 700 600 500 Control I II III Application rate of Alginit F 10 C 10 F 20 C 20 I, II and III are the application rates of 4, 8 and 16 kg/m 2 of Alginit; F=fine= Result: <2 mm Alginit particle size, C= coarse= 3-4 mm Alginit particle size; 10= 10 cm soil mixture depth, 20= 20 cm soil mixture More total dry matter dept + 93% (16 kg/m 2 ), + 64% (8kg/m 2 )

Alginit research results Field experiment, Gérce, Hungary (Farmer Szélessy) Experimental conditions: Alginit dosage of 2 to/ha on an acid sandy soil culture 1: corn, 5 ha, control area 8.85 ha culture 2: oat, 4 ha, control area 8 ha control areas fertilized with 200 kg/ha NKP (3*15) Alginit areas no NPK fertilisation all other treatments equal in May-June: 27 days drought periode Results: more harvest corn: + 10%, oat: + 23% areas treated with Alginit did not suffer from drougth

% 180 160 140 120 100 80 60 40 20 0 Alginit research results Greenhouse pot experiment (Bonn, Germany) Different Alginit dosages on a sandy soil Culture: cress Greenhouse pot trial with cress plants 135 165 100 100 Total dry matter (TDM) 68,5 61,1 Water consumption per g TDM 0% Alginit 10% Alginit 20% Alginit Results: more total dry matter (up to + 65%) much better water use efficiency

Alginit application fields Alginit s natural optimally balanced composition makes it suitable for use in the following areas: Agriculture and forestry Tree and shrub nurseries Gardening and landscaping Combat desertification Establishment of soil substrate

Alginit application fields Furthermore Alginit can be used in the following areas: land reclamation (binding of heavy metals and sodium) soil ph regulation (for acid soils) manure management (ammonia fixation) filter material by beverage production hormone filtering of drinking water

Thank you for your attention Alginit Kft. 1075 Budapest, Károly krt. 11. Tel.: 0036 (1) 269 7826 Fax: 0036 (1) 269 7827 E-mail: alginit.info@gmail.com www.alginit.hu www.alginit.com