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Port Silt Loam Oklahoma State Soil
PORT SILT LOAM Oklahoma State Soil SOIL SCIENCE SOCIETY OF AMERICA Introduction Many states have a designated state bird, flower, fish, tree, rock, etc. And, many states also have a state soil – one that has significance or is important to the state. The Port Silt Loam is the official state soil of Oklahoma. Let’s explore how the Port Silt Loam is important to Oklahoma. History Soils are often named after an early pioneer, town, county, community or stream in the vicinity where they are first found. The name “Port” comes from the small com- munity of Port located in Washita County, Oklahoma. The name “silt loam” is the texture of the topsoil. This texture consists mostly of silt size particles (.05 to .002 mm), and when the moist soil is rubbed between the thumb and forefinger, it is loamy to the feel, thus the term silt loam. In 1987, recognizing the importance of soil as a resource, the Governor and Oklahoma Legislature selected Port Silt Loam as the of- ficial State Soil of Oklahoma. What is Port Silt Loam Soil? Every soil can be separated into three separate size fractions called sand, silt, and clay, which makes up the soil texture. They are present in all soils in different propor- tions and say a lot about the character of the soil. Port Silt Loam has a silt loam tex- ture and is usually reddish in color, varying from dark brown to dark reddish brown. The color is derived from upland soil materials weathered from reddish sandstones, siltstones, and shales of the Permian Geologic Era. -
Silt Fence Note
9/3/2020 9:29:31 AM N:\CFL-DPIT\Drawings\FP-14\FP14_Details\C157-50.dgn _User: Angela.Johnson_ POST ANDGEOTEXTILEINSTALLATIONDETAIL See EndPostsDetail End posts ELEVATION 18" min. 30" min. See note5 Geotextile END POSTSDETAIL Fil l s lo pe 24" min. See Note3 END DETAIL PLAN 6" min. Backfilled andcompactedsoil F Fence supportmesh(optional) l Steel orwoodpost o See note5 Geotextile Staple ortie w Steel orwoodpost 6" min.trench PLAN Toe of slope See Note3 Posts Detail See End End posts (undisturbed) Existing ground Limits ofclearing SILT FENCEINSTALLATIONATTOEOFFILL for spacing See Note4 SILT FENCE ASPERIMETER CONTROL Existing ground A A Roadway Edge ofshoulder See TypicalSectionSheet Edge ofshoulder SECTION A-A Fill ELEVATION Varies Varies PLAN PLAN Flow Flow Toe ofslope Toe ofslope Silt fence S h Toe of slope e F e il t l s f l l o o p w e Silt fence Top ofpoststiedtogether. Posts driventightlytogether. Steel orwoodposts NO SCALE See note5 Section A Geotextile POSTS ATJOINTS REVISED: 08/2014 07/2020 5. 4. 3. 2. 1. NOTE: 713.16(a). Furnish geotextileconformingtosubsection 6 ft.(max.) Post spacing 10 ft.(max.) Post spacing running aroundtheends. fence uptheslopetopreventwaterfrom As theslopeisconstructed,curvesilt contours ascloselypossible. Install siltfencetofollowtheground manufacturer's recommendations. machine-sliced siltfenceaccordingtothe slicing asapprovedbytheCO.Install Silt fencemaybeinstalledusingmachine CENTRAL FEDERALLANDSHIGHWAYDIVISION PLAN DETAIL APPROVEDFORUSE U.S. DEPARTMENTOFTRANSPORTATION FEDERAL HIGHWAYADMINISTRATION U.S. CUSTOMARYDETAIL SILT FENCE without with STATE Fasten fabrictoposts. each postonefullturn. Fold geotextilearound fencesupportmesh= Staple ortie fencesupportmesh= See note5 Section B Geotextile PROJECT C157-50 DETAIL NUMBER SHEET NOTES TO THE DESIGNER Last Updated: July 2020 General Information 1. -
Strengthening Silt Fences
Article 56 Feature article from Watershed Protection Techniques. 2(3): 424-428 Strengthening Silt Fence ilt fences are one of the most widely used and reality, settling is actually the most important sedi- misused erosion and sediment control practices. ment removal function of silt fences (Kouwen, 1990), SRecent data suggest that they can perform well since runoff is detained behind the fence, giving sedi- under some circumstances. In addition, their cost- ment time to settle out. effectiveness continues to make them a popular ESC Three recent studies report sediment removal ef- technique. Unfortunately, silt fences are often used ficiencies ranging from 36 to 86% (Table 1). It is al- inappropriately or are improperly installed or maintained, most impossible to accurately predict the field perfor- resulting in poor performance. Simple improvements to mance of silt fences because relatively little research the standard silt fence, as well as some innovative has been done, and the results are so variable. This designs, can help to improve the current state of silt being said, some useful information emerges from fences. available data. First, these studies suggest that silt fences are more effective at removing coarser-grained How, and How Well, Do They Work? materials. Conversely, silt fences are ineffective at Silt fences trap sediment in construction runoff be- reducing turbidity, which is disproportionately influ- fore it washes into the street, a neighboring property or, enced by finer particles (Horner et al., 1990). A sec- in the worst case, a nearby stream or wetland. As sedi- ond finding is that silt fences are less effective on ment-laden runoff flows through the silt fence, the pores steeper slopes. -
Silt Fence Installation Guidelines
Silt Fence Installation Guidelines Sediment Control QUALITY - SUPPORT - EXPERTISE Silt Fence Installation Guidelines 2 00m m de ep 200mm STEP 1 STEP 2 Installation STEP 1 Excavate a trench a minimum of 200mm wide and 200mm deep on STEP 3 the uphill side of the proposed line of silt fence. STEP 2 Drive adequate length support posts to a depth (minimum 400mm) appropriate for the site conditions downhill of the trench. A. Post spacing is typically at 2m centres with wire attached along the top between posts to assist with support of the silt fence. B. Post spacing can be increased up to 4m centres if supported by 2.5mm diameter high tensile wire at mid height and along the top 600mm with hog rings, clips or pins every 150mm connecting the silt fence along the top wire. STEP 3 Roll out silt fence and position up against the support posts and fold over top wire. Hog rings, clips or pins are used to attach the silt fence to the top wire (at the required spacing). STEP 4 STEP 4 Bury bottom section along the base and up the side of the trench leaving a minimum exposed height of 600mm and backfill with soil. Compact to ensure good anchorage. Place safety caps on posts. NOTE Installation to follow your local Regional Council guidelines for erosion control and sediment control. Maintenance Regular inspection of silt fence is required especially after each rainfall event. Make any necessary repairs and remove excessive silt deposits to reduce pressure on the silt fence. NEW ZEALAND AUCKLAND HAMILTON NAPIER CHRISTCHURCH (64) 9 634 6495 (64) 21 732 178 (64) 21 916 736 (64) 3 349 5600 MELBOURNE SYDNEY NEWCASTLE COFFS HARBOUR PERTH ADELAIDE AUSTRALIA (03) 8586 9111 (02) 8785 8800 (02) 4951 2688 (02) 6653 5706 (08) 6305 0561 (08) 8162 5855 HOBART BRISBANE TOWNSVILLE BUNDABERG GOLD COAST DARWIN (03) 6273 0511 (07) 3279 1588 (07) 4774 8222 (07) 4155 9968 (07) 5594 8600 0407 523 669 0800 60 60 20 (Freephone NZ only) Follow GEOFABRICS.CO.NZ Geofabrics on GEOFABRICS.COM.AU The information contained in this brochure is general in nature. -
Silt Fences Allow Sediment to Settle from Runoff Before Water Leaves the Construction Site
Silt Fence SC-1 BMP Objectives ○ Soil Stabilization ● Sediment Control ○ Tracking Control ○ Wind Erosion Control ○ Non-Storm Water Management ○ Materials and Waste Management Definition and Purpose A silt fence is a temporary linear sediment barrier of permeable fabric designed to intercept and slow the flow of sediment-laden sheet flow runoff. Silt fences allow sediment to settle from runoff before water leaves the construction site. Appropriate Applications Silt fences are placed: n Below the toe of exposed and erodible slopes. n Down-slope of exposed soil areas. n Around temporary stockpiles. n Along streams and channels. Limitations n Not effective unless trenched and keyed in. n Not intended for use as mid-slope protection on slopes greater than 4:1. n Must be maintained to remain effective. n Not intended for use in streams, channels, or anywhere flow is concentrated. n Difficult to install and maintain in windy areas. n Must be removed and disposed of. 70 Design Guidelines and Considerations n Do not use below slopes subject to creep, slumping, or landslides. n Do not use in streams, channels, or anywhere flow is concentrated. n Do not use silt fences to divert flow. n The maximum length of slope upgradient of the silt fence should be 60 m (200 ft) or less to minimize flow volumes and velocities and increase the effectiveness of the silt fence. n Slope of areas draining to fence should be less than 1:1 but can be used below steeper slopes at the Engineers discretion. n Limit to locations suitable for temporary ponding or deposition of sediment. -
Straw Wattles
EROSION & SEDIMENT CONTROL PRODUCT OVERVIEW Straw Wattles Straw wattles are an effective and economical Straw wattles are available in two sizes: alternative to silt fence and straw bales for • 9 inch (22.86 cm) diameter sediment control and storm water runoff. • 12 inch (30.48 cm) diameter Cylinders of recycled, compressed, 100% agricultural straw, straw wattles are wrapped in Advantages of Straw Wattles tubular, UV-stabilized black synthetic netting. • Increased weight per linear foot for less Straw wattles can be placed and staked along resistance to movement from wind, water and the contour of newly constructed or disturbed sediment load. slopes. Fertile topsoil, organic matter, and native • Low-cost solution to sheet and rill erosion seeds are trapped behind straw wattles and problems. provide a stable medium for germination. Straw • Replaces silt fence or straw bales on steep wattles also retain moisture from rainfall, aiding slopes. the growth of tree seedlings planted to their up- • Lasts up to two years. slope side. • Stores moisture for vegetation planted immediately up-slope. • The straw incorporates into the soil over time, adding organic material to the soil and retaining moisture for vegetation. • Can be staked with fascines to stabilize low- velocity stream banks and establish wetland plants. Straw Wattles Applications for Straw Wattles The Nilex Advantage • Control stormwater runoff. Diverts flow and Nilex is committed to unearthing better directs stormwater to treatment areas. results. Whether it’s for a civil, resource or • Prevent off-site sedimentation at active environmental project, we offer the latest construction sites. Keeps soil on-site and engineered and technically superior materials prevents it from washing onto pavement and techniques to save our customers time and asphalt; an economical and effective and money, and minimize the need to move or perimeter control alternative to silt fence and remove earth, and reduce the need for granular straw bales. -
Types of Landslides.Indd
Landslide Types and Processes andslides in the United States occur in all 50 States. The primary regions of landslide occurrence and potential are the coastal and mountainous areas of California, Oregon, Land Washington, the States comprising the intermountain west, and the mountainous and hilly regions of the Eastern United States. Alaska and Hawaii also experience all types of landslides. Landslides in the United States cause approximately $3.5 billion (year 2001 dollars) in dam- age, and kill between 25 and 50 people annually. Casualties in the United States are primar- ily caused by rockfalls, rock slides, and debris flows. Worldwide, landslides occur and cause thousands of casualties and billions in monetary losses annually. The information in this publication provides an introductory primer on understanding basic scientific facts about landslides—the different types of landslides, how they are initiated, and some basic information about how they can begin to be managed as a hazard. TYPES OF LANDSLIDES porate additional variables, such as the rate of movement and the water, air, or ice content of The term “landslide” describes a wide variety the landslide material. of processes that result in the downward and outward movement of slope-forming materials Although landslides are primarily associ- including rock, soil, artificial fill, or a com- ated with mountainous regions, they can bination of these. The materials may move also occur in areas of generally low relief. In by falling, toppling, sliding, spreading, or low-relief areas, landslides occur as cut-and- La Conchita, coastal area of southern Califor- flowing. Figure 1 shows a graphic illustration fill failures (roadway and building excava- nia. -
Silt Fences: an Economical Technique for Measuring Hillslope Soil Erosion
United States Department of Agriculture Silt Fences: An Economical Technique Forest Service for Measuring Hillslope Soil Erosion Rocky Mountain Research Station General Technical Peter R. Robichaud Report RMRS-GTR-94 Robert E. Brown August 2002 Robichaud, Peter R.; Brown, Robert E. 2002. Silt fences: an economical technique for measuring hillslope soil erosion. Gen. Tech. Rep. RMRS-GTR-94. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 24 p. Abstract—Measuring hillslope erosion has historically been a costly, time-consuming practice. An easy to install low-cost technique using silt fences (geotextile fabric) and tipping bucket rain gauges to measure onsite hillslope erosion was developed and tested. Equipment requirements, installation procedures, statis- tical design, and analysis methods for measuring hillslope erosion are discussed. The use of silt fences is versatile; various plot sizes can be used to measure hillslope erosion in different settings and to determine effectiveness of various treatments or practices. Silt fences are installed by making a sediment trap facing upslope such that runoff cannot go around the ends of the silt fence. The silt fence is folded to form a pocket for the sediment to settle on and reduce the possibility of sediment undermining the silt fence. Cleaning out and weighing the accumulated sediment in the field can be accomplished with a portable hanging or plat- form scale at various time intervals depending on the necessary degree of detail in the measurement of erosion (that is, after every storm, quarterly, or seasonally). Silt fences combined with a tipping bucket rain gauge provide an easy, low-cost method to quantify precipitation/hillslope erosion relationships. -
Summarization and Comparison of Engineering Properties of Loess in the United States
Summarization and Comparison of Engineering Properties of Loess in the United States J. B. SHEELER, Associate Professor of Civil Engineering, Iowa State University •LARGE deposits of loess are found in many parts of the United States, but published values of the engineering properties of loess are relatively scarce. The data in this paper were gathered to indicate similarities and compare the properties of loess from one area with another. Loess is composed primarily of rather loosely arranged angular grains of sand, silt, and clay. Silt is usually the dominant size. Calcite is also generally present in amounts ranging from zero to more than 10 percent of the total soil.. The aeolian hypothesis of loess deposition is compatible with the physical charac teristics of undisturbed loess masses. This hypothesis states that fine-grained ma terial was transported, sorted, and redeposited by wind action and thus became loess. During deposition, moisture and clay minerals are believed responsible for cementing the coarser grains together to form a loose structure. The loess is therefore subject to loss of shear strength due to water softening the clay bonds and to severe consolida tion caused by a combination of loading and moisture. Loess is usually thought of as an aeolian material that was deposited thousands of years ago and has remained in place since the time of deposition. Loess that has been eroded and redeposited is often referred to as redeposited loess, reworked loess or more simply as a silt deposit. This implies that the word loess indicates an aeolian soil, undisturbed since deposition. Certain engineering properties of loess, such as shear strength, are quite drastically changed by erosion and redeposition. -
SDD 8E9 Silt Fence
SDD 08E09 Silt Fence GENERAL NOTES DETAILS OF CONSTRUCTION NOT SHOWN ON THIS DRAWING SHALL CONFORM ROADWAY ROADWAY ROADWAY TO THE PERTINENT REQUIREMENTS OF THE STANDARD SPECIFICATIONS AND APPLICABLE SPECIAL PROVISIONS. SHOULDER SHOULDER SHOULDER 1 HORIZONTAL BRACE REQUIRED WITH 2" X 4" WOODEN FRAME OR EQUIVALENT A DITCH DIKE AT TOP OF POSTS. INSLOPE FLOW INSLOPE FLOW INSLOPE FLOW FLOW 4 1 2 FOR MANUAL INSTALLATIONS THE TRENCH SHALL BE A MINIMUM OF 4" WIDE AND 1 6" DEEP TO BURY AND ANCHOR THE GEOTEXTILE FABRIC. FOLD MATERIAL TO FIT TRENCH AND BACKFILL AND COMPACT TRENCH WITH EXCAVATED SOIL. 1 1 3 WOOD POSTS SHALL BE A MINIMUM SIZE OF 1 8" X 1 8" OF OAK OR HICKORY. INSLOPE INSLOPE 4 SILT FENCE TO EXTEND ACROSS THE TOP OF THE PIPE. A FLOW FLOW FLOW 5 CONSTRUCT SILT FENCE FROM A CONTINUOUS ROLL IF POSSIBLE BY CUTTING SHOULDER SHOULDER LENGTHS TO AVOID JOINTS. IF A JOINT IS NECESSARY USE ONE OF THE FOLLOWING TWO METHODS; A) OVERLAP THE END POSTS AND TWIST, OR ROTATE, AT LEAST 180 DEGREES, B) HOOK THE END OF EACH SILT FENCE ROADWAY ROADWAY LENGTH. INSLOPE 10'- 0" POST MIN. ** **GEOTEXTILE FABRIC FLOW FLOW GROUND 2 LINE GEOTEXTILE FABRIC SITUATION 1 SITUATION 2 SECTION A - A (TYPICAL) FLOW PLAN VIEW DIRECTION 2 PLAN VIEW SILT FENCE AT MEDIAN SURFACE DRAINS TYPICAL APPLICATION OF SILT FENCE EXCESS FABRIC FLOW DIRECTION TRENCH DETAIL NOTE: ADDITIONAL POST DEPTH OR GEOTEXTILE TIE BACKS MAY BE REQUIRED FOLD 6 3" MAX. FABRIC 6 IN UNSTABLE SOIL. SUPPORT CORD OR TENSION TAPE 3 WOOD POSTS 4' - 0" MIN. -
The Fairfax County Erosion and Sediment Control Checklist
DEPARTMENT OF PUBLIC WORKS AND ENVIRONMENTAL SERVICES, COUNTY OF FAIRFAX OFFICE OF SITE DEVELOPMENT SERVICES ENVIRONMENTAL AND FACILITIES REVIEW DIVISION EROSION AND SEDIMENT CONTROL CHECKLIST Project Name: Project #: Tax Map #: District: Design Engineer: Plan Reviewer: Date: Abbreviations PFM: Fairfax County Public Facilities Manual VESCH: Virginia Erosion and Sediment Control Handbook CC: Fairfax County Code MS: Minimum State Standard LTI: Fairfax County Letter to Industry Shown on Item # Code Section Requirement OK NO N/A Plan Sheet # 1 NARRATIVE All plans must have Erosion and Sediment Control Narrative. The narrative should be site specific and include the PFM 11 -0405.8.B following items: 1.1 VESCH 7A-2 Project Description- Briefly describe the purpose and nature of land disturbing activity, and the area to be disturbed. 1.2 VESCH 7A-2 Existing Site Condition - Description of existing topography, vegetation and drainage Adjacent Areas - a Brief description of neighboring areas such as streams, lakes, ponds, floodplain, Resources 1.3 VESCH 7A-2 Protection Area (RPA), Environmental Quality Corridor (EQC) or residential areas which might be affected by this project. 1.4 VESCH 7A-2 Off-site areas - Describe any off-site land-disturbing activities that will occur including borrow sites, waste or surplus areas. Critical Areas - A description of areas on the site which have potential serious erosion problem (e.g., steep slopes, 1.5 VESCH 7A-2 channels, wet weather/underground springs) Soils - A description of areas on the site giving such information as soil name, mapping unit, erodibility, permeability, 1.6 VESCH 7A-2 depth, texture and soil structure. -
Step 2-Soil Mechanics
Step 2 – Soil Mechanics Introduction Webster defines the term mechanics as a branch of physical science that deals with energy and forces and their effect on bodies. Soil mechanics is the branch of mechanics that deals with the action of forces on soil masses. The soil that occurs at or near the surface of the earth is one of the most widely encountered materials in civil, structural and architectural engineering. Soil ranks high in degree of importance when compared to the numerous other materials (i.e. steel, concrete, masonry, etc.) used in engineering. Soil is a construction material used in many structures, such as retaining walls, dams, and levees. Soil is also a foundation material upon which structures rest. All structures, regardless of the material from which they are constructed, ultimately rest upon soil or rock. Hence, the load capacity and settlement behavior of foundations depend on the character of the underlying soils, and on their action under the stress imposed by the foundation. Based on this, it is appropriate to consider soil as a structural material, but it differs from other structural materials in several important aspects. Steel is a manufactured material whose physical and chemical properties can be very accurately controlled during the manufacturing process. Soil is a natural material, which occurs in infinite variety and whose engineering properties can vary widely from place to place – even within the confines of a single construction project. Geotechnical engineering practice is devoted to the location of various soils encountered on a project, the determination of their engineering properties, correlating those properties to the project requirements, and the selection of the best available soils for use with the various structural elements of the project.