Characteristics of soil pockets resulting from AerWay rolling tines Song Ai, Ying Chen * Department of Biosystems Engineering, University of Manitoba,

Slides:



Advertisements
Similar presentations
Hydrologic (water) Cycle
Advertisements

If water can pass through a surface, the surface is permeable.
What on Earth is Soil?.
Infiltration Through Compacted Urban Soils and Effects on Biofiltration Robert Pitt Department of Civil and Environmental Engineering University of Alabama.
Rural, Onsite & Small Community Wastewater & Waste Engineering Designing Soil Based Systems.
Components and Physical Properties of Soil Unit: Soil Science Lesson 3.
Forms of Hydraulic Fractures at Shallow Depths in Piedmont Soils.
Introduction to Soil Mechanics
Determining Soil Texture by Feel
Erosion Control Short Course Monday, April 23, 2012 San Luis Obispo City/County Library Ron Harben, Project Director California Association of Resource.
Nitrogen use efficiency (NUE) is estimated to be 33% throughout the world, and can be lower in single, pre-plant applications compared with split nitrogen.
Soils. 3 characteristics of soil affect its value for farming and growing vegetation: 1.Organic Content 2.Mineral Content 3.Soil Texture.
Soil Texture Size or combination of sizes of the soil particles Influences how much water soaks into the soil versus how much runs off the surface and.
Chapter 4: Soil Architecture and Physical Properties
SOIL PHYSICAL COMPONENTS “Getting to the root of the problem” sand silt clay air water Cation exchange tillage roots.
Soil-climate impacts on water cycling at the patch level.
Infiltration Introduction Green Ampt method Ponding time
Percent Silt Percent Clay Percent Sand Clay Sandy Clay Clay Loam Silty Clay.
CTC-375 Construction Methods
Surveying Survey measurements can be represented graphically: diagrams; maps; profiles; and cross sections. And to determine: locations; directions; areas;
Factors that Influence Erosion
Introduction to Agriculture Soil Science Unit 2. » Physical properties or characteristics of the soil determine to a large degree how useable and productive.
Comparing soils Type of Soil Example of Test Jar
Introduction Agriculture is a large contributor of non-point source pollution to surface water. Field surface application of manure as a soil amendment.
Topic - Study of soil formation & physical properties of soil 1 | Vigyan Ashram | INDUSA PTI |
Inequalities in One Triangle
Timothy Reeves: Presenter Marisa Orr, Sherrill Biggers Evaluation of the Holistic Method to Size a 3-D Wheel/Soil Model.
Soil Quality Explain the effects of soil quality on the characteristics of an ecosystem.
Bell Work: Find the total surface area of this figure. Use 3.14 for π. 6 cm 10 cm.
RIVERS AN INTRODUCTION.
SOIL TEXTURE GEOGRAPHY 6A
5.5Use Inequalities in a Triangle Theorem 5.10: If one side of a triangle is longer than the other side, then the angle opposite the longest side is _______.
Surface Water Chapter 9. Surface water movement: Water Cycle Earths water supply is constantly recycled.
Lab 13 - Predicting Discharge and Soil Erosion Estimating Runoff Depth using the Curve Number method –Land use or cover type –Hydrologic condition –Soil.
LandJudging in Oklahoma
Soil Texture. Different Types of Soils ZSand ZSilt ZClay.
Soil and Environmental Implications of Land Rolling Corn Logan Ahlers and Paul Kivlin College of Agriculture, Food, and Environmental Science University.
Environmental Chemistry Chapter 5: Chemistry of the Solid Earth Copyright © 2009 by DBS.
SOIL OBSERVATORIES Austrian site by Winfried E.H. Blum Institute of Soil Research University of Natural Resources and Applied Life Sciences (BOKU), Vienna.
What is Erosion and Sedimentation ? Bill Laflamme CPESC, Office of the Commissioner MAINE DEPARTMENT OF ENVIRONMENTAL PROTECTION Protecting Maine’s Air,
Soils. Formation of Soils Physical Weathering Rain, wind, abrasion Chemical Composition is not altered Influenced by climate Chemical Weathering Acid.
4.7 Triangle Inequalities. Theorem 4.10 If one side of a triangle is longer than another side, then the angle opposite the longer side is larger than.
4.7 Triangle Inequalities. In any triangle…  The LARGEST SIDE lies opposite the LARGEST ANGLE.  The SMALLEST SIDE lies opposite the SMALLEST ANGLE.
Thursday, November 8, 2012 Agenda: TISK & No MM Lesson 5-5: Triangle Inequalities Homework: 5-5 Worksheet.
EROSION- The transport of weathered materials…. Major Erosive Agents: Running Water GLACIERS WIND OCEAN CURRENTS AND WAVES MASS WASTING (GRAVITY!)
Soil And Rock General Soil Characteristics Trafficability – ability of soil to support weight of vehicles under repeated traffic –Controls traffic on unimproved.
There are four main functions of the lens…. The first and most obvious is…
Irrigation Requirements Based upon the book Rain Bird Irrigation Design Manual From Chapter 3.
 Process of where soil particles are displaced  Wind Erosion.
Maximum Liquid Manure Spreading Rates on Sloping Land Ron Fleming and Malcolm MacAlpine University of Guelph Ridgetown Campus CSBE
SOIL MECHANICS AND CLASSIFICATION. FACTORS WHICH HOLD SOIL TOGETHER o Cohesion  Internal Friction.
SOIL DEGRADATION  When plants (trees & shrubs) are cleared from a site, soil is exposed to sunlight and the eroding effects of wind and water. Soil aeration.
Physical and Chemical Properties of soils from Pecan Orchards Sheny Leon Mentor: Dr. Manoj Shukla Plant and Environmental Sciences, NMSU NEW MEXICO AMP.
 Soil is the lose covering of rock particles and decaying organic matter(humus)  Results from both physical and chemical weathering.
Day 19 Objective You will learn about soil texture and composition in order to determine soil’s value as a resource and conservation measures. Warm-Up.
LO – To understand the changes in river process with distance from source - To understand Long and Cross Profiles of a river.
5.4 Inequalities in One Triangle
Soil & Land resources Objective: Evaluate soil properties that affect land use in agricultural and urban areas.
Soil Texture.
Cameras for dummies! (not that any of you are dummies…)
Soils.
مثلثهای کلاس بندی بافت خاک
Redahegn Sileshi1, Robert Pitt2, Shirley Clark3, and Chad Christian4
Soil.
Depth Of Field (DOF).
Soil
Use Inequalities in a Triangle
SCIENCE GRADE FOUR – SOILS
Unit 57 – Photography Depth of field
> < > < ≥ ≤ Shot at 90% Larger Smaller Larger
Presentation transcript:

Characteristics of soil pockets resulting from AerWay rolling tines Song Ai, Ying Chen * Department of Biosystems Engineering, University of Manitoba, Winnipeg, Manitoba, Canada R3T 5V6,

Introduction  AerWay rolling tines  Ontario-based Holland Equipment  Create pockets on the ground  Low soil disturbance  Reducing runoff and erosion

Objectives  Study pocket characteristics of AerWay rolling tines  Tillage depth  Offset angle  Type of tine

Site descriptions  Clay loam soil  57% sand, 22% silt, and 21% clay  located in Piney, Manitoba  Sandy soil  75% sand, 18% silt, and 7% clay  located in Menisino, Manitoba

Experimental design  Types of rolling tines  Shatter tines and Leaf tines  Offset angles  0 and 5 degree  Injection depths  125 and 150 mm  Number of treatments  8  Replication  4  Total number of test runs  64

Pocket opening Clay loam Sandy soil

Measurements - Pocket opening and volume

Results and discussion

Pocket opening  Clay loam  significant interaction effects  penetration depth and offset angle  for both tines, pocket length increased with a greater penetration depth  pocket width increased with a greater tine offset angle  the greatest length, width, and area mm depth and 5° offset angle, regardless of the type of tine used

Pocket opening  Sandy soil  not significant interaction effects  penetration depth and offset angle  pocket length was affected by penetration depth for shatter tines only  with the same penetration depth and offset angle  pocket opening created by Shatter tine was greater than that created by Leaf tine

Pocket volume in the clay loam soil for different combinations of penetration depth and offset angle

Pocket volume of AerWay rolling tines in the sandy soil

Conclusion  Characteristics of the soil pockets varied  type of soil, type of tine, penetration depth, and offset angle  Shatter tines created larger pocket openings than Leaf tines  Pockets openings  shorter and wider in the clay loam soil  longer and narrower in the sandy soil

Conclusion  The greater penetration depth resulted in a bigger pocket opening length  The larger offset angle increased pocket volume  Pocket volumes  sandy soil smaller than clay loam soil  Greater injection depth, large offset angle, heavier soil, and Shatter tines types favour large pocket volumes and opening

Question