By Eric Swaisgood Spring 2010. CELINA SERIES: SOIL 1 CRIDER SERIES: SOIL 2

Slides:



Advertisements
Similar presentations
One of Our Natural Resources!
Advertisements

MA Envirothon Soils Glenn Stanisewski, Soil Resource Specialist, USDA-NRCS West Wareham, MA.
The four components of soil:
 Mollisols  Alfisols  Inceptisols  Entisols Example of an Udipsamment, which is an Entisol – A young poorly developed soil in a sandy glacial outwash.
 Found in middle latitudes and prairie regions  Areas with moderate temps and precipitation  Organic decomposition is responsible for thick dark topsoil.
OM  humus 1º minerals  clays OM, clay, ions Transformations: runoff leaching Rain, OM capillary rise Four processes: Additions Losses Translocations.
DO Now: You find a sedimentary rock that has one graded bed. Describe how you know which layer of the graded bed is formed last?
SOILS Most important result of weathering and Erosion is soil Soils - soil science = PEDOLOGY Residual soil - soil made from local bedrock (weathered material)
Unit 2 Topic 2 soil. What is soil and why do we care about it?  complex mixture:  weathered mineral materials from rocks  partially decomposed organic.
The Ground Beneath Our Feet. What Makes Up Healthy Soil? Mineral fragments, humus, air, water, and living things – Plant roots, Insects, Worms Humus –
Environmental Pedology Field Assignment Spring 2010 Kamaljit Banger GCREC Wimauma GCREC Wimauma, Florida.
Karen Balentine SWS 5716 Spring 2011 Soil samples were taken from field sites located on the Harney River, in Everglades National Pak, Fl. The two sites.
Topic 5 Part 1 soil.
Copyright © 2006 Pearson Education, Inc., publishing as Benjamin Cummings World soil conditions Soils are becoming degraded in many regions.
Comparison of Candler Sand and Adamsville Fine Sand Shengsen Wang Presentation for Environmental Pedology, Spring
Soil Classification Comparison Hall County, Georgia University of Florida Soil Pedology, Spring 2010 Prof: Willie Harris By: Sam Vacca 4/22/10.
Weathering has led to valuable mineral deposits and has provided materials for sedimentary rocks. Most important, weathering has helped form a priceless.
Soils. Soil Weathering and erosion transports materials across Earth’s surface Weathering and erosion transports materials across Earth’s surface The.
U.S. Department of the Interior U.S. Geological Survey Norman B. Bliss, ASRC Federal InuTeq Contractor to the USGS 6/4/2015 A continental view of soil.
Selected Soils of Leon County, Florida Matt Wilson: Pedology Spring 2010.
Soil Project: Two Southeast Michigan Soils Ray Powe SWS 5716C.
Tim Hull Environmental Pedology
Ch 5 - Soils Important effect of weathering for people!
Soils and Microclimate
NORTH County MELBOURNE DISCUSSED LAKE Washington SOUTH County DISCUSSED JOe Ramos 01 University of Florida SWS 5716 – Pedology Prof. Willie Harris Site.
Daniel L. Irick Environmental Pedology Spring 2008
Lisa Shaw SOS 5716C -Pedology Spring Coastal Plain Lakes, Creeks, Springs Mean Air Temperature : 67.5 F Avg. Yearly Precipitation: 67.2” North Site-
Descriptions of two shallow soils overlying limestone bedrock (oolite) in SW Miami-Dade County Wayne Worthley SWS 5716c Dr. Harris Krome ‘R’ Biscayne.
Getting Dirty with SOILS. Older than dirt????!!!!
Soil. Mechanical and chemical weathering of rocks form soil. Soil covers much of the land on Earth. It is made up of minerals, air, water, and organic.
 The top few inches of the earth’s surface that supports plant growth.  Formed from parent material (rocks and minerals) by a process known as weathering.
Soil Basics AP Environmental Science. SOIL ≠ DIRT.
Understanding Soil Formation. Five different factors that affect soil formation 2. Topography -the slope characteristics of the soil 1.Parent material.
Soil Interpretations Field Project of Soils Patancheru, Andhra Pradesh, India Environmental Pedology DE Spring 2010 K.S. Winans.
Description and Interpretations of two soils at Long and Scott Farms, Inc. Jacqueline Depaz.
Comparison of Two Soils in Warren County, MS Michelle Bourne March 2010 SWS5716C-Pedology.
A tale of two soils in Warren County, MS James Lindsay SWS5716C-Pedology Spring 2012.
SOIL HORIZON ANALYSIS ACROSS A DRAINAGE GRADIENT IN NORTHEASTERN CONNECTICUT Deborah Spalding SWS 5716C April 21, 2011.
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.
Will Weiss Spring #7: Candler sand, 0-5% slope #8: Candler sand, 5-12% slope Mean rain fall: 48 in Mean temperature: 74 degrees F Elevation: 80ft.
Cedar Key & Pine Acres Drained vs. Not So..! Stew Whitney 03/25/10 Environmental Pedology.
SOIL A mixture of rock particles, minerals, decayed organic matter, air, and water. Soil composition depends on the size of the individual particles (gravel,
Final Presentation of GIS in Water Resources
Soil.
SOIL FORMATION.
The Nature of Soil Essential Question:
October 11, 2011.
Soil Origin and Development
The Nature of Soil Essential Question:
Wangari Gardens: Soil Survey
Soils.
Getting Dirty with SOILS
Soil and Its Uses.
The Ground Beneath Our Feet
The Nature of Soil Essential Question:
What is a soil profile? Cross section of soil layers revealing all soil horizons O Horizon = organic material (humus) A Horizon = topsoil B Horizon =
Warmup List three things you might find in soil.
Soil Regolith – layer of rock and mineral fragments produced by weathering Soil – part of regolith that supports plant growth.
Soil How much soil is there?.
Soil Origin and Development
The Ground Beneath Our Feet
What is happening in numbers 1, 2, 3 and 4
Properties of Soil.
One of Our Natural Resources!
Warmup List three things you might find in soil.
The Ground Beneath Our Feet
Composition Formation Erosion Profile
Warmup List three things you might find in soil- don’t have to write this down.
Warmup List three things you might find in soil.
Week 3: Lesson 2 and 3 Soils and Relationships
Presentation transcript:

By Eric Swaisgood Spring 2010

CELINA SERIES: SOIL 1 CRIDER SERIES: SOIL 2

FAYETTE COUNTY JEFFERSONVILLE, OHIO MONROE COUNTY BLOOMINGTON, INDIANA

CeB (Celina Silt Loam)

Sample Location

Overview of entire profile with a max depth of 16-ft. Shallow (left) to Deep (right)

ApBt12Bt2

2Bt2 close-up of Fe accumulation at about 58 cm.

2Bt3 2Bct 2Cd2 2Cd

CtC (Crider-Urban land complex)

Sample Location

Ap Bt1 Bt2 2Bt3 2C R

ApBt1 Bt2 2Bt3 2C R

Depletions Chert Rock

CelinaCrider Parent Material Glacial Till (Central Lowlands) Climate Average Rain = 48-in. Average Temp = 57 ° F Average Rain = 38-in. Average Temp = 53 ° F Topography 6-12% Slopes; shallow bedrock 2-6% Slopes; deep bedrock Organisms Worms Time Young (shallow)Older (deep)

CelinaCrider Infiltration RateModerate (Silt Loam) Available WaterHighLow Hydraulic Conductivity Low Seasonal High Water Table 50 to 100 cm<25 cm BasementsSevere (3) Absorption fieldsSevere (3) Local Roads & Streets Severe (3)

CelinaCrider EpipedonOchric Subsurface Horizon Argillic OrderAlfisol or Ultisol (based on location probably Alfisol)

Feedback: Privacy Policy Feedback
Do Not Sell My Personal Information
About project: SlidePlayer Terms of Service

© 2025 SlidePlayer.com. Inc. All rights reserved.