Site and Soil Investigations Terry L. BoveeSteve Lawler Professional Soil Scientists Henderson, MN 56044Rochester, MN 55906 507-248-9626507-282-4090

Slides:



Advertisements
Similar presentations
WATER QUALITY ANALYSIS for ANTIDEGRADATION
Advertisements

STP Land Application Site Suitability and Selection Considerations in Montana What do I look for besides a willing landowner?
Ground Water Mounding & P Evaluations
Horticulture Science Explaining a Soil Profile
Groundwater Mounding and Minnesota ISTS Rules MPCA 2/21/06.
Genesis and function of pore structures formed in saprolite by Mike Vepraskas, NCSU, Soil Science.
Selected Soil Related Topics
Bliss Area Sewage System Groundwater Monitoring Pete Ganzel Washington County Department of Public Health & Environment.
MA Envirothon Soils Glenn Stanisewski, Soil Resource Specialist, USDA-NRCS West Wareham, MA.
Soil Physical Properties – Colour, Texture, Structure
Redoximorphic Features and Hydric Soils NC STATE UNIVERSITY DEPARTMENT of SOIL SCIENCE NC STATE UNIVERSITY DEPARTMENT of SOIL SCIENCE NC STATE UNIVERSITY.
Formation and Characteristics of Hawaii’s Soils
Soil Mapping and Erosion
Important/significant foundation soil physical properties Color Texture Structure Consistence Coarse fragments Reaction.
Hydrologic storage in seasonal, mineral flat wetlands across native prairie, farmed, and restored prairie land cover: structural controls and hydrologic.
1 Septic Tank Drainfield Site Suitability and Evaluation Workshop Montana State University Extension Service, Department of Land Resources an Environmental.
Rule Change Update MPCA 1/13/ Mid-Sized ISTS (MSTS)
Natural Resources Conservation Service Helping People Help the Land SOIL – The Fundamental Concepts.
Chapter 4: Soil Architecture and Physical Properties
Welcome! The Topic For Today Is… Soil. SOIL TextureStructureBMPsSoil SurveySoil Forming Factors FINAL JEOPARDY.
Soil Physical Properties
1 Important/significant foundation soil physical properties Color Redoximorphic features Texture Structure Consistence Coarse fragments Reaction.
Its NOT DIRT!!! Soils Somewhat Simplified. SOILS FORM IN MINERAL AND ORGANIC DEPOSITS OVER THOUSANDS TO MILLIONS OF YEARS NEW ENGLAND SOILS ARE YOUNGLESS.
Soils Investigation Soil Investigation
 Soil grains come from weathering of bedrock ◦ Physical weathering – granular soils ◦ Chemical weather – creates clay  Soil is either residual or transport.
Growing Plants : The Soil Profile. What is Soil Made up of?
NextEnd. INTRODUCTION Grapes can be grown on a variety of soil types. However, the highest vine vigor and yield and the most efficient production are.
Growing Plants Hydroponically vs. In Soil:
Fruit & Vegetable Production Unit for Plant Science Core Curriculum Lesson 3: Site Evaluation Fruit & Vegetable Production Unit for Plant Science Core.
Section 3: Soil Preview Key Ideas Soil Soil Characteristics
Problem Hydric Soils. Saturated, but not Reduced Low organic matter –e.g., sands No iron –e.g., E horizons of Spodosols, sands Oxygenated water –slopes,
How To Describe or Identify Water Levels Using Soil Morphology Prepared by Mr. Brian Oram, Professional Geologist, Soil Scientist Wilkes University Environmental.
Site Investigation and Storage Structure Sizing CNMP Core Curriculum Section 4 – Manure Wastewater Storage and Handling.
Envirothon Soil. Topics Soil Soil Formation Soil Texture Soil Color Organic Matter pH Salinity Soil Air Compaction/Shrink-Swell Drainage Erosion Soil.
WHAT’S IN THE SOIL? And why is it important?. Sand  Drains well but can not hold onto nutrients. Sand is a large particle.  Form lightweight, free-draining.
Presented by: 1. A measure of how easily a fluid (e.g., water) can pass through a porous medium (e.g., soils) 2 Loose soil - easy to flow - high permeability.
STRATIFICATION PLOT PLACEMENT CONTROLS Strategy for Monitoring Post-fire Rehabilitation Treatments Troy Wirth and David Pyke USGS – Biological Resources.
“Soil Wetness Modeling Rules for Sewage Treatment and Disposal Systems in North Carolina” by Barrett L. Kays, Ph.D., NCCHS Steven Berkowitz, P.E., NCDENR.
Environmental Factors Soils Earth’s Surface 770 % Water 330 % Land OOnly 10 % of land is arable (suitable for cultivation) OOf this arable land,
Soil Quality Explain the effects of soil quality on the characteristics of an ecosystem.
SOIL - Fundamental Concepts Prepared by Earl D. Lockridge National Soil Survey Center Lincoln, NE.
BASIC INSTALLERS COURSE. SHARED RESPONSIBILITY  SOIL TESTER SITE EVALUATION ○ PERCOLATION ○ OTHER  PUBLIC HEALTH ENVIRONMENTALIST PLAN REVIEW INSPECTION.
Landscapes and Landscape Development Topic 14 in Review Book.
Massachusetts Public Health Inspector Training Wastewater Certificate Program (MA PHIT WW) Session 3: Site Evaluation and Selection 1 MA PHIT- Wastewater.
Water Movement Below Surface
Soils & Soil Horizons APES – Ch. 8. Weathering of Minerals.
Timeline Impaired for turbidity on Minnesota’s list of impaired waters (2004) MPCA must complete a study to determine the total maximum daily load (TMDL)
12.2 Soil Key Ideas: Soil is made of weathered rock and organic material. Climate and other factors affect the composition of the soil.
Groundwater & Wetlands
 This is a questionnaire about the family  How many and what ages?  Hobbies?  Pets?  Do they like to garden?  Do they prefer patios or decks? 
Estimating Groundwater Recharge in Porous Media Aquifers in Texas Bridget Scanlon Kelley Keese Robert Reedy Bureau of Economic Geology Jackson School of.
Analyzing the Landscape Site. Preparation for the Design Process The one key to successful landscaping is to consider the features of the site and the.
Understanding Soil.
 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.
Introduction to Land Evaluation Basic Soil Science AFNR-BAS-6: Describe soil formation and management and assess its relevance to plant/animal production.
6. Drainage basins and runoff mechanisms Drainage basins Drainage basins The vegetation factor The vegetation factor Sources of runoff Sources of runoff.
The Site Landscaping Chapter 4. Objectives*  Define the word site and explain its significance in the development of a landscape  List the typical features.
Soils and Growing Media
Introduction to | Soil Science Presented by: Mr. Brian Oram, PG, PASEO Wilkes University GeoEnvironmental Sciences and Environmental Engineering Department.
Physical Properties of Soil. Soil Texture What is Soil Texture? It is the proportion of three sizes of soil particles. Which are: Sand (Large) Silt (Medium)
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.
GROUNDWATER HYDRAULICS ECV 5406 NAME : SHARINA BINTI SULAIMAN MATRIK. NO : GS69364.
Soil Properties Unit 5.02.
Factors of Soil Development
Soils 5.02: Discuss the soil profile and soil sampling for surface and subsurface layers.
Analyzing the Landscape Site (Analisis Tapak)
Soil 7.EC.5A.2 Construct explanations of how soil quality (including composition, texture, particle size, permeability, and pH) affects the characteristics.
Soil Quality
7.EC.5A.2 Construct explanations of how soil quality (including composition, texture, particle size, permeability, and pH) affects the characteristics.
Properties of Soil.
Presentation transcript:

Site and Soil Investigations Terry L. BoveeSteve Lawler Professional Soil Scientists Henderson, MN 56044Rochester, MN Minnesota Onsite Wastewater Convention March 13-15, 2006

Site & Soil Evaluation for Medium and Large Sized Sewage Treatment Systems (MSTS and LSTS)

From this…

To this…

You Need A Lot of Information!

What is the Purpose of a Site Evaluation??

Site Evaluation PURPOSE To provide a large MSTS/LSTS system designer with specific information about the landscape and soils of a site to determine suitability for the proposed use.

Site Evaluation REASONS Required by Minnesota Rules - small & medium sized systems LSTS Guidance considerations

Site Evaluation Getting the BIG Picture… The Designer is RESPONSIBLE for accurate & complete site/soil observations, evaluation, interpretations and conclusions. BOTTOM LINE: WILL THE TREATED WATER STAY BELOW THE SOIL SURFACE??

Site Evaluation Two Stages of Evaluating a Site: 1 st – Preliminary Data Collection 2 nd – Field Data Collection

Preliminary Data Cultural features; ownership, parcel boundaries, buildings, easements, setbacks, field roads, wells, property lines, current & historic land use & vegetation Sources: P & Z, SWCD, aerial photos

Preliminary Data Natural features; floodplains, wetlands, surface waters, direction of surface water runoff, groundwater flow direction, topography Sources: P & Z, SWCD = surface water data; USGS/MGS/MDH = ground water flow direction

Preliminary Data

Preliminary Data SOILS: Online Soil Survey

Preliminary Data Design parameters; daily flows, size of proposed treatment area, size of area being considered Regulatory input; meet w/permitting authority, LGUs, technical consultants, developer Is everyone… on the same page?

Preliminary Data Before going into the field: Cultural and Natural Features should be recorded on a sketch map. OK…time to get into the field!

Field Data What Is It? Geomorphic Features - large scale units Soil Features - small scale units

Field Data Why is it Important? DESIGN, DESIGN, DESIGN! Accurate Soils Descriptions : Critical! Interpretation of Soils Data : Critical!

Field Data Geomorphic Features - P arent Material: till, residuum, loess? - Landform: till plain, bedrock, outwash? - Landscape Position: side slope or toe slope? - Slope Characteristics: shape, position, length, gradient, aspect

Field Data Slope Shapes

Soil…what is it? Natural body that occurs on the land surface, occupies space and is characterized by one or both of the following: -Horizons or layers, and/or -Ability to support rooted plants in a natural environment

Field Data Soil Features…what are they? - Horizons, Textures, Structure - Colors, Redoximorphic Features, Mottles - Consistance, Roots, Pores - Depth to Bedrock, Coarse Fragments, Lithologic Discontinuities - Water Status

The Soils are REALLY Important!

Recording Soil Descriptions

Horizons Influenced by: Time, Landscape, Parent Material, Vegetation, Climate

Texture Numerical proportion of sand, silt, clay (% by weight) Usually done in field by hand (qualitative) Important factor in influencing soil water movement

Structure Naturally occurring arrangement of soil particles…Peds Grade, size, type, consistance Important factor in soil water movement Best described by excavations

Color Matrix: predominant color Redoximorphic Features: chemistry, secondary color Mottles: usually geologic, secondary color Best described by natural light – avoid dawn/dusk

Interpreting Soil Color Color is an INDICATOR of … soil wetness Critical Part of Evaluation…. and must be done correctly!

Redoximorphic Features… What Are They?

Redoximorphic Features (RMF) Anaerobic conditions: - soil is saturated Prolonged absence of O 2 alters chemical process Reduction of Fe and Mn oxides – results in distinct characteristics

RMF and Minnesota MSTS & LSTS Guidance RMF are used to determine: - Depth to Seasonally Saturated Soil (a restricting layer) - Operating Separation Distance (needed distance to meet treatment and hydraulic performance requirements)

RMF Interpretation Problems Not all wet soils develop RMF - Low amounts of soluble organic carbon (sands) - High pH - Cold temperatures - Low amounts of Fe (sands or parent material) - Aerated ground water (floodplains?) - Masking of RMF (overthickened topsoils)

Soil Drainage Classes

Soil Drainage as Related to Landscape

Soil Water Movement… What Is It? It Is: - Rate of flow OVER the soil (runoff) - Rate of flow INTO the soil (infiltration) - Rate of flow WITHIN the soil (hydraulic conductivity)

Soil Permeability NRCS Description - Qualitative analysis - Measured in units of length/time - Estimations derived from percolation tests, soil texture and structure - Concept has changed over time: Emphasis is now on quantitative data vs. qualitative data

Soil Permeability

Hydraulic Conductivity… A Better Way? Quantifies soil’s ability to transmit water under standard conditions and units (pressure, length, cross-sectional area) Saturated conditions are easiest to assess Highly variable (pores, etc), therefore multiple reps recommended per area of interest Field methods (natural conditions) generally more reliable than lab methods

Hydraulic Conductivity… A Better Way? Provides “measured” data in soil horizons: The horizon with the lowest Ksat value should be used for design purposes. Field tools available: permeameters, infiltrometers, etc

Hydraulic Conductivity… A Better Way?

Soil Interpretation Are the soil properties described favorable to downward movement of water? Will the soils on the proposed site support the density of the intended use? Do you have sufficient soils information to justify moving forward on this site?

REVIEW

Review Preliminary Map - topography - conceptual MSTS/LSTS layout - Any existing soils data - Wells, roads, etc.

Review Mark-up Preliminary map - Soils data - Surface water - Soil water monitoring - Problem areas - Field notes

Review Discussion w/ Designer - Soil Descriptions - Soil Water - Soil Sizing Factors - Additional data needed - Revise layout? - Other issues?

Review Additional Soils Data?? - More soil borings per regulatory request? - Additional soil pits? - Piezometer data? - Hydraulic Conductivity data?

CONCLUSION Large-scale MSTS/LSTS projects can benefit from professionals in the area of soil science and geology that can: 1) accurately describe soil properties, 2) model ground water characteristics, and 3) provide the designer with interpretation of water movement through the soils and substratums of the landscape.

Resources Soil Surveys: Soil Scientists: Minnesota Assoc. of Professional Soil Scientists Geologists & Groundwater: