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HomeMy WebLinkAbout20142338.tiff AGPROfessionals ■ ■ DEVELOPERS OF AGRICULTURE Geology Report Weld County Change of Zone Application Prepared for Mile High Investments, LLC soTLOGIC February 24, 2014 AGPROfessionals, LLC 3050 67th Avenue, Suite 200 Greeley, Colorado 80634 Attn: Mr. Tim Naylor Re: Geology Report Mile High Investments, LLC (Approximate 74 Acre Parcel) Weld County, Colorado Soilogic Project # 14-1036 Mr. Naylor: Soilogic, Inc. (Soilogic) personnel have completed the geologic evaluation you requested for the above referenced project. Our evaluation was completed through review of mapped and published information concerning site soil and groundwater conditions. A list of the references reviewed is included with this report. The subject property includes a total of approximately 74 acres located in Section 2, Township 5 North, Range 65 West and Section 35, Township 6 North, Range 65 West of the 6th Principal Meridian in Weld County, Colorado. The property is located both north and south of County Road 47 and west of County Road 62 in Weld County, Colorado. The site is relatively flat with the maximum difference in ground surface elevation across the parcel estimated to be less than 5 feet. The included soil type delineation diagram outlines those soil groupings identified at the site by Weld County Soil Conservation Service (SCS) maps. SCS descriptions of those soil types are included with this report. In general, the near surface soils at this site consist of low to moderately plastic sandy clay loam from the Nunn and Otero series. The mapped soils consist of Pinedale and Bull Lake Age alluvium from upper Pleistocene geologic period. Mapped information indicates the property is not in an area identified as being flood prone and would be expected to have groundwater at depths ranging from approximately 10 to 20 below ground surface Soilogic, Inc. 3050 67th Avenue, Suite 200 • Greeley, CO 80634 • (970) 535-6144 P.O. Box 1121 • Hayden, CO 81639 • (970) 276-2087 Geology Report Mile High Investments, LLC (Approximate 74-Acre Parcel) Weld County, Colorado Soilogic # 14-1036 2 According to geologic maps of the area, the site overburden soils are underlain by the Laramie bedrock formation consisting of shale, claystone and sandstone from the upper cretaceous period. According to SCS data, the depth to bedrock would be expected to be greater than 5 feet across the site. Based on our review of the site as outlined above, we expect the near surface soils could be used for support of lightly to moderately loaded industrial structures. Deep foundation systems could be employed if heavy foundation loads are anticipated. During our review of available site data, we did not identify other potential geologic hazards as outlined in H.B. 1041 . In addition, we did not identify economically recoverable gravel resources at this site. We appreciate the opportunity to be of service to you on this project. If we can be of further service to you in any way or if you have any questions concerning the enclosed information, please do not hesitate to contact us. Very Truly Yours, Soilogic, Inc. 0 REGjs``�� ( a9 .• . • ' • • 3 . J . r ss/oNA Wolf von Cal owitz, P.E. Principal Engineer Geology Report Mile High Investments, LLC (Approximate 74-Acre Parcel) Weld County, Colorado Soilogic # 14-1036 3 REFERENCES 1 . Colton R.B. and Harold R. Fitch, 1974, Map Showing Potential Sources of Gravel and Crushed-Rock Aggregate, in the Boulder-Fort Collins-Greeley Area, Front Range Urban Corridor, Colorado: U.S. Geological Survey Miscellaneous Investigation Series Map I-855-D. 2. Colton R.B., 1978, Geologic Map of the Boulder-Fort Collins-Greeley Area, Colorado: U.S. Geological Survey Miscellaneous Investigation Series Map I-955-G. 3 . Hershey L.A. and Schneider, Jr. P.A., 1972, Geologic Map of the Lower Cache La Poudre River Basin, North-Central Colorado: U.S. Geological Survey Miscellaneous Investigation Series Map I-687. 4. Hillier D. and Schneider, Jr. P.A., 1979, Depth to the Water Table in the Boulder-Fort Collins-Greeley Area, Front Range Urban Corridor, Colorado: U.S. Geological Survey Miscellaneous Investigation Series Map I-855-I. 5. United States Department of Agriculture Soil Conservation Service and Forest Service in Cooperation with Colorado Agricultural Experiment Station, 1980, Soil Survey of Weld County Area, Colorado, Maps 239-812/3. 6. Schneider, Jr. P. A., 1983 Shallow Groundwater in the Boulder-Fort Collins-Greeley Area, Front Range Urban Corridor, Colorado 1975-77: U.S. Geological Survey Water Resources Investigations Report 83-4058. 7. Soil Survey Staff, Natural Resources Conservation Service, United States Department of Agriculture. Web Soil Survey. Available online at http://websoilsurvey.nrcs.usda.gov/ accessed (October 20, 2011). Soil Map—Weld County, Colorado, Southern Part I. (Mile High Investments, LLC (74 Acre Parcel)) in ° ° 531600 531700 531800 531900 532000 532100 532200 10° 26' 12"N A�`•_ - 40° 26' 12"N 1. 1 / 1 1 it a 0.10 n O NI w 4 N K 4 1 ' -, • I L fv 1 )s ..l �; —r----r. I 4 14 464 11 idsr +tfli i 1 11•..41��seii. t tr .-( {. ! ! I 4r. • 4 ` . . 11111 .- • 1! 1 + v 1 `-+`1-So. 4151 4` 1 ♦ 1I la . I N . , t. o r. i �. : 1 . 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U C i4 aTI m ■ to 3 C 0 in c._ i• ii Z 0� Soil Map—Weld County, Colorado, Southern Part Mile High Investments, LLC (74 Acre Parcel) Map Unit Legend Weld County, Colorado, Southern Part (CO618) Map Unit Symbol Map Unit Name Acres In AOI Percent of AOI 41 Nunn clay loam, 0 to 1 percent 48.3 66.9% slopes 51 Otero sandy loam, 1 to 3 23.9 33.1% percent slopes Totals for Area of Interest 72.3 100.0% t :) Natural Resources Web Soil Survey 2/24/2014 Conservation Service National Cooperative Soil Survey Page 3 of 3 Map Unit Description: Nunn clay foam, 0 to 1 percent slopes—Weld County, Colorado, Southern Mile High Investments, LLC (74 Acre Part Parcel) Weld County, Colorado, Southern Part 41 —Nunn clay loam, 0 to 1 percent slopes Map Unit Setting Elevation: 4,550 to 5,150 feet Mean annual precipitation: 12 to 18 inches Mean annual air temperature: 46 to 54 degrees F Frost-free period: 115 to 180 days Map Unit Composition Nunn and similar soils: 85 percent Minor components: 15 percent Description of Nunn Setting Landform: Terraces, plains Down-slope shape: Linear Across-slope shape: Linear Parent material: Mixed alluvium and/or eolian deposits Properties and qualities Slope: 0 to 1 percent Depth to restrictive feature: More than 80 inches Drainage class: Well drained Capacity of the most limiting layer to transmit water (Ksat): Moderately low to moderately high (0.06 to 0.20 in/hr) Depth to water table: More than 80 inches Frequency of flooding: None Frequency of ponding: None Calcium carbonate, maximum content: 15 percent Maximum salinity: Nonsaline (0.0 to 2.0 mmhos/cm) Available water capacity: High (about 9. 1 inches) Interpretive groups Farmland classification: Prime farmland if irrigated Land capability classification (irrigated): 2e Hydrologic Soil Group: C Ecological site: Clayey Plains (R067BY042CO) Typical profile 0 to 9 inches: Clay loam 9 to 29 inches: Clay loam 29 to 60 inches: Sandy loam Minor Components Heldt Percent of map unit: 7 percent Dacono Percent of map unit 4 percent USDA Natural Natural Resources Web Soil Survey 2/24/2014 Conservation Service National Cooperative Soil Survey Page 1 of 2 Map Unit Description: Nunn clay loam, 0 to 1 percent slopes—Weld County, Colorado, Southern Mile High Investments, LLC (74 Acre Part Parcel) Altvan Percent of map unit: 4 percent Data Source Information Soil Survey Area: Weld County, Colorado, Southern Part Survey Area Data: Version 12, Jan 3, 2014 iiivii Natural Resources Web Soil Survey 2/24/2014 Conservation Service National Cooperative Soil Survey Page 2 of 2 Map Unit Description: Otero sandy loam, 1 to 3 percent slopes--Weld County, Colorado, Mile High Investments, LLC (74 Acre Southern Part Parcel) Weld County, Colorado, Southern Part 51 —Otero sandy loam, 1 to 3 percent slopes Map Unit Setting Elevation: 4,700 to 5,250 feet Mean annual precipitation: 12 to 15 inches Mean annual air temperature: 48 to 52 degrees F Frost-free period: 130 to 180 days Map Unit Composition Otero and similar soils: 85 percent Minor components: 15 percent Description of Otero Setting Landform: Plains Down-slope shape: Linear Across-slope shape: Linear Parent material: Eolian deposits and/or mixed outwash Properties and qualities Slope: 1 to 3 percent Depth to restrictive feature: More than 80 inches Drainage class: Well drained Capacity of the most limiting layer to transmit water (Ksat): Moderately high to high (0.57 to 5.95 in/hr) Depth to water table: More than 80 inches Frequency of flooding: None Frequency of ponding: None Calcium carbonate, maximum content: 10 percent Maximum salinity: Nonsaline to very slightly saline (0.0 to 4.0 mmhos/ cm) Available water capacity: Moderate (about 7.7 inches) Interpretive groups Farmland classification: Prime farmland if irrigated and the product of I (soil erodibility) x C (climate factor) does not exceed 60 Land capability classification (irrigated): 3e Land capability (non irrigated): 4e Hydrologic Soil Group: B Ecological site: Sandy Plains (R067BY024CO) Typical profile 0 to 12 inches: Sandy loam 12 to 60 inches: Fine sandy loam Minor Components Kim Percent of map unit 10 percent USDA Natural Resources Web Soil Survey 2/24/2014 a Conservation Service National Cooperative Soil Survey Page 1 of 2 Map Unit Description: Otero sandy loam, 1 to 3 percent slopes--Weld County, Colorado, Mile High Investments, LLC (74 Acre Southern Part Parcel) Vona Percent of map unit: 5 percent Data Source Information Soil Survey Area: Weld County, Colorado, Southern Part Survey Area Data: Version 12, Jan 3, 2014 USDA Natural Resources Web Soil Survey 2/24/2014 Conservation Service National Cooperative Soil Survey Page 2 of 2 AGPROfessionals ■■ DEVELOPERS OF AGRICULTURE Soil Survey and Study Weld County Change of Zone Application Prepared for Mile High Investments, LLC USDA United States A product of the National Custom Soil Resource Department of Cooperative Soil Survey, Agriculture a joint effort of the United Report for 4 NRCS States Department of Agriculture and other Weld County , Federal agencies, State Natural agencies including the Colorado , Resources Agricultural Experiment Conservation Stations, and local Service participants Southern Part Wells Ranch i r OF 4t .� 1 ., _ r' t ._ , j •A . - . . ' - -., / Yr , ` •.• 1 ' + r, � I IrlINw • - i S� v I 7; I - . T I. 0 8,000 ft - February 17, 2014 Preface Soil surveys contain information that affects land use planning in survey areas. They highlight soil limitations that affect various land uses and provide information about the properties of the soils in the survey areas. Soil surveys are designed for many different users, including farmers, ranchers, foresters, agronomists, urban planners, community officials, engineers, developers, builders, and home buyers. Also, conservationists, teachers, students, and specialists in recreation, waste disposal, and pollution control can use the surveys to help them understand, protect, or enhance the environment. Various land use regulations of Federal, State, and local governments may impose special restrictions on land use or land treatment. Soil surveys identify soil properties that are used in making various land use or land treatment decisions. The information is intended to help the land users identify and reduce the effects of soil limitations on various land uses. The landowner or user is responsible for identifying and complying with existing laws and regulations. Although soil survey information can be used for general farm, local, and wider area planning, onsite investigation is needed to supplement this information in some cases. Examples include soil quality assessments (http://www. nres.usda.gov/wps/portal/ nrcs/main/soils/health/) and certain conservation and engineering applications. For more detailed information, contact your local USDA Service Center (http:// offices.sc.egov. usda.gov/locator/app?agency=nres) or your NRCS State Soil Scientist (http://www.nres.usda.gov/wps/portal/nres/detail/soils/contactus/? cid=nrcs142p2_053951 ). Great differences in soil properties can occur within short distances. Some soils are seasonally wet or subject to flooding_ Some are too unstable to be used as a foundation for buildings or roads. Clayey or wet soils are poorly suited to use as septic tank absorption fields. A high water table makes a soil poorly suited to basements or underground installations. The National Cooperative Soil Survey is a joint effort of the United States Department of Agriculture and other Federal agencies, State agencies including the Agricultural Experiment Stations, and local agencies. The Natural Resources Conservation Service (NRCS) has leadership for the Federal part of the National Cooperative Soil Survey. Information about soils is updated periodically. Updated information is available through the NRCS Web Soil Survey, the site for official soil survey information. The U.S. Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, age, disability, and where applicable, sex, marital status, familial status, parental status, religion, sexual orientation, genetic information, political beliefs, reprisal, or because all or a part of an individual's income is derived from any public assistance program. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means 2 for communication of program information (Braille, large print, audiotape, etc.) should contact USDA's TARGET Center at (202) 720-2600 (voice and TDD). To file a complaint of discrimination, write to USDA, Director, Office of Civil Rights, 1400 Independence Avenue, S.W., Washington, D.C. 20250-9410 or call (800) 795-3272 (voice) or (202) 720-6382 (TDD). USDA is an equal opportunity provider and employer. 3 Contents Preface 2 Soil Map 5 Soil Map 6 Legend 7 Map Unit Legend 8 Map Unit Descriptions 8 Weld County, Colorado, Southern Part 10 41—Nunn clay loam, 0 to 1 percent slopes 10 51—Otero sandy loam, 1 to 3 percent slopes 11 Soil Information for All Uses 13 Soil Properties and Qualities 13 Soil Qualities and Features 13 Hydrologic Soil Group 13 Depth to Any Soil Restrictive Layer 17 Unified Soil Classification (Surface) 20 Soil Reports 25 Soil Physical Properties 25 Engineering Properties 25 References 29 4 Soil Map The soil map section includes the soil map for the defined area of interest, a list of soil map units on the map and extent of each map unit, and cartographic symbols displayed on the map. Also presented are various metadata about data used to produce the map, and a description of each soil map unit. 5 Custom Soil Resource Report N Soil Map tiO h 11/4.tl m o 531700 531800 531900 532000 532100 532200 40° 26'9"N 1 40° 26'9"N • I ' } , I. 1 • __ ....._.--L__ - -- _ . IL - - � 1 r+ri •c' . :t• r , • i ' Q • t �. ., _ .. ... . ., , __ ri , k \ ,, p.n. , ,. It. 1/ I 7, .;.,;44 l \1/2,4, , ci J Li C I/1F J 8 . NI- ,, 13 • ra O 8 YI r. U ri .11 1. I, f, ri it $ s 4 I ;ii i, i � $ I n y r Hi P 40° 25'39'N 40° 25'39"N 531700 531800 531900 532000 532100 532200 532300 3 3 X ZO Map Scale: 1:4,500 if printed on A portrait(8.5" x 11") sheeten Meters it N 5 100 200 300 .1 A — 'Feet 0 200 400 800 1200 Map pntection: Web Mentatrx Corner coordinates: WGS84 Edge tics: (JIM Zone 13N WGS84 6 4) a) "- d t3'> co Q C O O c • d a) m y0 L =Ezi M 0 U O •L as 0 • N N > co CI) U to Q Ola N r co "- b a) O L- to a; m Cu r I C .. U o c a) U Cr) 2 O .C 0 cn r to C is J+ 0 0 a M w U 2 •v d a) r- a) O C U U U N a) '0 .0 ° r ° 0 c t0 0 C ` E V 2 cv 4- to E cn to a� b E 4 I- o N = a' ` ° v t�� wcti : v to — o v (fl U 0 •� 'O LO .0 U r-- O .0 2 P 0 w Q (Ni as co Z E a) atvc) W till .c 4,, V) o E n vv �' O2 To to 15 C v >. M C l�6 U d p Q = '0 E l6 v c v a) C aL .n 'v 0 Or c tOn Q CO p v) E O a C o Z3 N Z N o 'a to E ca U ,`� W cn c v v oM o v co Q a nsarm E to .0 Q. to 0 a c � cn A/ ` U (Q . . c O N O0 03 O C to U co O O Q ca p a CO v4.- o v o 3 co U o to � N CO o � e ri ii LL C) v mC ° COim o c Nov 0>-. w •c � cv 3 � �- a E � � a to _0 a 'm ._ .c ° vag � � ova� Eo oc to t vvE Z c c � � cc t—vv � cm t� a) vao � � 0 .0 co� �' v , ° a) o w Q3 _ .a f.s. O n N a > 5 N ° U v a? 0 N O N ° < U N co CO ifs ii 6 U) cn a c.) iii y > ° O L C2 . it- .C E p N > .n Z Q' . . .a Q a M 0 — Cu a) o N O a en v CCU °' Lacaic� N v , •ics � RI ov, o N co E ,.c T .. vx o -0tT3 C a > >. o ° CO CZ •N co � 0 E ° � cy t� O c co ~ 00 o c n S c c6 ton .' C Q O '= (a t? CO a CO a) •�: o ?, ? - E al = c = c m � a N ° c6 u) ` •c v c v- o ° o ti v o Q Q rn v CO t0 a ° 'o c 2 o v v -- o 'y a`) Cu o Z, C 'v E .C v r- U t0 > >. co --g w Qc v +- tvn y ` � " to t; h.-. a ti a) to a) E � r a •av to E to a to cv to o o a .a? CD o to > — C -- its m r v E to 0 a, C N ca a) a) O a) o tD O to 9 — F w E o.. t°n o f toSU 2 a. vQ o tom- COW (n `o ON H ° .E t 0 a a) CC (1) U D O U) (1) tom-- Q� m N ciii . ,. �' E c ca c a. o a) CO 3 a U .C 12 rn tr, o) o D to o T c c = to t�6 a o co V N a O o -1 N a? -, O O L iA 0. m E ct< o a .- o O 41) >N L c t6 y •-• ..) a_ . U) 03 0 14.3 Cl) to > > O CO co o a S = 2 -J < 0 to C a) Z UV 4J e 4' q u' . 0. 0 c7) imi W " ± ( 1 , • c R c�C to It 03 W J in A C {i O ` a Q C c ' v) � C - (n Q �` c .22 m v n no a CO E 0) y w. N a� ro a o a`) c C C ` a 3 o ° . o 3 3 0 t ,. a) a) to n w cn O O w a RS 01a o ° > = o o 0 m c Co ' to Q ° ti o o > > c� m c u •.- -c cu 2 co y •O •O •O 4-. o Ot N o 2 2 (C4 f56 w C co a) o a t6 co c •- O CD < to CO CO •o m m U U 0 0 J -1 a a_ ft to to a) to to to g a c To m � � o ■ 9 ® X0 0 - 1 00 > + . . 0 as ► � < to Custom Soil Resource Report Map Unit Legend Weld County, Colorado, Southern Part (CO618) Map Unit Symbol Map Unit Name Acres In AOl Percent of AOI 41 Nunn clay loam, 0 to 1 percent 52.8 72.3% slopes 51 Otero sandy loam, 1 to 3 percent 20.2 27.7% slopes Totals for Area of Interest 73.1 100.0% Map Unit Descriptions The map units delineated on the detailed soil maps in a soil survey represent the soils or miscellaneous areas in the survey area. The map unit descriptions, along with the maps, can be used to determine the composition and properties of a unit. A map unit delineation on a soil map represents an area dominated by one or more major kinds of soil or miscellaneous areas. A map unit is identified and named according to the taxonomic classification of the dominant soils. Within a taxonomic class there are precisely defined limits for the properties of the soils. On the landscape, however, the soils are natural phenomena, and they have the characteristic variability of all natural phenomena. Thus, the range of some observed properties may extend beyond the limits defined for a taxonomic class. Areas of soils of a single taxonomic class rarely, if ever, can be mapped without including areas of other taxonomic classes. Consequently, every map unit is made up of the soils or miscellaneous areas for which it is named and some minor components that belong to taxonomic classes other than those of the major soils. Most minor soils have properties similar to those of the dominant soil or soils in the map unit, and thus they do not affect use and management. These are called noncontrasting, or similar, components. They may or may not be mentioned in a particular map unit description. Other minor components, however, have properties and behavioral characteristics divergent enough to affect use or to require different management. These are called contrasting, or dissimilar, components. They generally are in small areas and could not be mapped separately because of the scale used. Some small areas of strongly contrasting soils or miscellaneous areas are identified by a special symbol on the maps. If included in the database for a given area, the contrasting minor components are identified in the map unit descriptions along with some characteristics of each. A few areas of minor components may not have been observed, and consequently they are not mentioned in the descriptions, especially where the pattern was so complex that it was impractical to make enough observations to identify all the soils and miscellaneous areas on the landscape. The presence of minor components in a map unit in no way diminishes the usefulness or accuracy of the data. The objective of mapping is not to delineate pure taxonomic classes but rather to separate the landscape into landforms or landform segments that have similar use and management requirements. The delineation of such segments on the map provides sufficient information for the development of resource plans. If 8 Custom Soil Resource Report intensive use of small areas is planned, however, onsite investigation is needed to define and locate the soils and miscellaneous areas. An identifying symbol precedes the map unit name in the map unit descriptions. Each description includes general facts about the unit and gives important soil properties and qualities. Soils that have profiles that are almost alike make up a soil series. Except for differences in texture of the surface layer, all the soils of a series have major horizons that are similar in composition, thickness, and arrangement. Soils of one series can differ in texture of the surface layer, slope, stoniness, salinity, degree of erosion, and other characteristics that affect their use. On the basis of such differences, a soil series is divided into soil phases. Most of the areas shown on the detailed soil maps are phases of soil series. The name of a soil phase commonly indicates a feature that affects use or management. For example, Alpha silt loam, 0 to 2 percent slopes, is a phase of the Alpha series. Some map units are made up of two or more major soils or miscellaneous areas. These map units are complexes, associations, or undifferentiated groups. A complex consists of two or more soils or miscellaneous areas in such an intricate pattern or in such small areas that they cannot be shown separately on the maps. The pattern and proportion of the soils or miscellaneous areas are somewhat similar in all areas. Alpha-Beta complex, 0 to 6 percent slopes, is an example. An association is made up of two or more geographically associated soils or miscellaneous areas that are shown as one unit on the maps. Because of present or anticipated uses of the map units in the survey area, it was not considered practical or necessary to map the soils or miscellaneous areas separately. The pattern and relative proportion of the soils or miscellaneous areas are somewhat similar. Alpha- Beta association, 0 to 2 percent slopes, is an example. An undifferentiated group is made up of two or more soils or miscellaneous areas that could be mapped individually but are mapped as one unit because similar interpretations can be made for use and management. The pattern and proportion of the soils or miscellaneous areas in a mapped area are not uniform. An area can be made up of only one of the major soils or miscellaneous areas, or it can be made up of all of them. Alpha and Beta soils, 0 to 2 percent slopes, is an example. Some surveys include miscellaneous areas. Such areas have little or no soil material and support little or no vegetation. Rock outcrop is an example. 9 Custom Soil Resource Report Weld County, Colorado, Southern Part 41 —Nunn clay loam, 0 to 1 percent slopes Map Unit Setting Elevation: 4,550 to 5, 150 feet Mean annual precipitation: 12 to 18 inches Mean annual air temperature: 46 to 54 degrees F Frost-free period: 115 to 180 days Map Unit Composition Nunn and similar soils: 85 percent Minor components: 15 percent Description of Nunn Setting Landform: Terraces, plains Down-slope shape: Linear Across-slope shape: Linear Parent material: Mixed alluvium and/or eolian deposits Properties and qualities Slope: 0 to 1 percent Depth to restrictive feature: More than 80 inches Drainage class: Well drained Capacity of the most limiting layer to transmit water (Ksat): Moderately low to moderately high (0.06 to 0.20 in/hr) Depth to water table: More than 80 inches Frequency of flooding: None Frequency of ponding: None Calcium carbonate, maximum content: 15 percent Maximum salinity: Nonsaline (0.0 to 2.0 mmhos/cm) Available water capacity: High (about 9.1 inches) Interpretive groups Farmland classification: Prime farmland if irrigated Land capability classification (irrigated): 2e Hydrologic Soil Group: C Ecological site: Clayey Plains (R067BY042CO) Typical profile 0 to 9 inches: Clay loam 9 to 29 inches: Clay loam 29 to 60 inches: Sandy loam Minor Components Heldt Percent of map unit: 7 percent Dacono Percent of map unit: 4 percent Altvan Percent of map unit: 4 percent 10 Custom Soil Resource Report 51 —Otero sandy loam, 1 to 3 percent slopes Map Unit Setting Elevation: 4,700 to 5,250 feet Mean annual precipitation: 12 to 15 inches Mean annual air temperature: 48 to 52 degrees F Frost-free period: 130 to 180 days Map Unit Composition Otero and similar soils: 85 percent Minor components: 15 percent Description of Otero Setting Landform: Plains Down-slope shape: Linear Across-slope shape: Linear Parent material: Eolian deposits and/or mixed outwash Properties and qualities Slope: 1 to 3 percent Depth to restrictive feature: More than 80 inches Drainage class: Well drained Capacity of the most limiting layer to transmit water (Ksat): Moderately high to high (0.57 to 5.95 in/hr) Depth to water table: More than 80 inches Frequency of flooding: None Frequency of ponding: None Calcium carbonate, maximum content 10 percent Maximum salinity: Nonsaline to very slightly saline (0.0 to 4.0 mmhos/cm) Available water capacity: Moderate (about 7.7 inches) interpretive groups Farmland classification: Prime farmland if irrigated and the product of I (soil erodibility) x C (climate factor) does not exceed 60 Land capability classification (irrigated): 3e Land capability (nonirrigated): 4e Hydrologic Soil Group: B Ecological site: Sandy Plains (R067BY024CO) Typical profile 0 to 12 inches: Sandy loam 12 to 60 inches: Fine sandy loam Minor Components Kim Percent of map unit 10 percent 11 Custom Soil Resource Report Vona Percent of map unit: 5 percent 12 Soil Information for All Uses Soil Properties and Qualities The Soil Properties and Qualities section includes various soil properties and qualities displayed as thematic maps with a summary table for the soil map units in the selected area of interest. A single value or rating for each map unit is generated by aggregating the interpretive ratings of individual map unit components. This aggregation process is defined for each property or quality. Soil Qualities and Features Soil qualities are behavior and performance attributes that are not directly measured, but are inferred from observations of dynamic conditions and from soil properties. Example soil qualities include natural drainage, and frost action. Soil features are attributes that are not directly part of the soil. Example soil features include slope and depth to restrictive layer. These features can greatly impact the use and management of the soil. Hydrologic Soil Group Hydrologic soil groups are based on estimates of runoff potential. Soils are assigned to one of four groups according to the rate of water infiltration when the soils are not protected by vegetation, are thoroughly wet, and receive precipitation from long- duration storms. The soils in the United States are assigned to four groups (A, B, C, and D) and three dual classes (ND, B/D, and C/D). The groups are defined as follows: Group A. Soils having a high infiltration rate (low runoff potential) when thoroughly wet. These consist mainly of deep, well drained to excessively drained sands or gravelly sands. These soils have a high rate of water transmission. Group B. Soils having a moderate infiltration rate when thoroughly wet. These consist chiefly of moderately deep or deep, moderately well drained or well drained soils that have moderately fine texture to moderately coarse texture. These soils have a moderate rate of water transmission. 13 Custom Soil Resource Report Group C. Soils having a slow infiltration rate when thoroughly wet. These consist chiefly of soils having a layer that impedes the downward movement of water or soils of moderately fine texture or fine texture. These soils have a slow rate of water transmission. Group D. Soils having a very slow infiltration rate (high runoff potential) when thoroughly wet. These consist chiefly of clays that have a high shrink-swell potential, soils that have a high water table, soils that have a claypan or clay layer at or near the surface, and soils that are shallow over nearly impervious material, These soils have a very slow rate of water transmission. If a soil is assigned to a dual hydrologic group (ND, B/D, or CID), the first letter is for drained areas and the second is for undrained areas. Only the soils that in their natural condition are in group D are assigned to dual classes. 14 j Custom Soil Resource Report Map—Hydrologic Soil Group to S ° g 531700 531800 531900 532000 532100 532200 40" 26'9'N r vr: _ . --- ,I - 40° 26'9"N . • , • . 71 - I ;' selp } ' _ -.. _ l - . 11-1 •— 0 ; , r %Y a ia/ re .I ! :> i VJ. $ O k 3 i ; '4 . . li O1 1 ,,1 1 O a ri R O ri .. - � . - T7 t Cu cr In 3 60 I i • g - [ 4- g .. . _ 4 i 1110 g 0, 40° 2519'N 40° 25 39"N 531700 531800 531900 532000 532100 532200 532300 1 to NN Map Scale: 1:4,500 if printed on A portrait(8.5" x 11")sheet m Meters a $ N 0 50 100 200 300 a Feet 1\4 0 200 400 800 1200 Map projection: Web Mercator Comer coordinates: WGS84 Edge tics: UTM Zone 13N WGS84 15 6 a> a) o o oC m a c' `o °' ` u>N 8 r CL) — no 6 0 m L N O N CO Ota la O N t06 ti- • O p 't ea ro 'C r 'S VC U O C cN V ca p C a> -o to v> r N Z O (U C o V U coa c0 ,n w 3 LO N n- a) TS O O .C _ o = a 1:7) lijN p c a> w Q ca Ni O ca E (O o 4- O ttJ O o U 5- m N N .0 o O N •am o. w 9 C o0 O co N Cn o E d a) a> `0 2 E cca — = a> cu CD os a> -6 W or Q 0 co 3 N o E o ca. C a N o Z 015 to N v o o .Q � coU �, � co a Q L 5 O , W ro o a O on o N al q id oa � ro NoL .O at2 (I) or a CLN re , U co ..- ... L a> N p a> a N U Ct C° cv o v Q al Ili co a T > y p o a O a) a .. r co a o O E >.+ c0 co2 ro O N O 4) d a) O C co a Z a O o O C C N _ L _01 Q) a> a) p a5 0 76 L C) O co O in n a) a. E a a>) O Q) U ro tZ O Dv O ` N T n E L B a) 0 3 p CJ Q) a) a) Q> 3 N CL r p n ZDE L2 L Q aO C a> .-. co a) O N O E to E � � t r T � � ins � gNyj c6 2 ro a _Qlo) coNE> p p L V C N Q O ?. a) U Mal ro 4-',..., N " co O O c0 a) C C COF- o O C (n = '0 q ro +•-N t0 O 'O Q N co a) c c`9 2 0 CO CON m r -- p a .� "J a`> U n to Z �' r a> m L >fD C •� to 'O a) O p O p ca O N .O m L a) p p ` co Q •C O m t— > W C Ti. N a ;v U) S U 2 Cif < o t— _a (n U) CO o O c'> i_ U .� O a a) CC a) U I- z O U) ft r _ m O _ m E CO o o m Q 0 t2.5 VS' C Cr) O) `o c = N v -o 0 V O 2 o to o 0 E co o C 0 F.. co 2.9_ Ill CC o co i o C.) 0 Z s cor Q c D J Q O co P C (7P. CO W J a) a) 25 3 a co m o :> S Y W Vl O O O a a a) h L.. Ca O O r O D < O >4 ca m r C C '- m . a° o 0 Q 0 n 0 0 o p o°. o 0 a) Q os < a [0 (n U U 0 Z Of < a co m U U O Z as cc a w n d C C a Ces 73 no I ® ■ ■ r. ® 1 1 1 1 1 1 1 : _ ■ ■ ■ ■ [- y 'o 0 'j o 0 -1 'o co co co 4 cn Custom Soil Resource Report Table -Hydrologic Soil Group Hydrologic Soil Group— Summary by Map Unit — Weld County, Colorado, Southern Part (CO618) Map unit symbol Map unit name Rating Acres in AOI Percent of AOI 41 Nunn clay loam, 0 to 1 C 52.8 72.3% percent slopes 51 Otero sandy loam, 1 to 3 B 20.2 27.7% percent slopes Totals for Area of Interest 73.1 100.0% Rating Options—Hydrologic Soil Group Aggregation Method: Dominant Condition Component Percent Cutoff.. None Specified Tie-break Rule: Higher Depth to Any Soil Restrictive Layer A "restrictive layer" is a nearly continuous layer that has one or more physical, chemical, or thermal properties that significantly impede the movement of water and air through the soil or that restrict roots or otherwise provide an unfavorable root environment. Examples are bedrock, cemented layers, dense layers, and frozen layers. This theme presents the depth to any type of restrictive layer that is described for each map unit. If more than one type of restrictive layer is described for an individual soil type, the depth to the shallowest one is presented. If no restrictive layer is described in a map unit, it is represented by the "> 200" depth class. This attribute is actually recorded as three separate values in the database. A low value and a high value indicate the range of this attribute for the soil component. A "representative" value indicates the expected value of this attribute for the component. For this soil property, only the representative value is used. 17 Custom Soil Resource Report N Map—Depth to Any Soil Restrictive Layer h ° 531700 531800 531900 532000 532100 532200 53 40° 26'9"N 40° 26 9'N „ .r. < • _ • I yF SS i O S. • ri i ei I. • (B _ O CC n Q U In I 1 in • I a. 0 ' t 8 40° 25139"N 40° 25 39"N 531700 531800 531900 532000 532100 532200 532300 3 3 IR to Map Scale: 1:4,500 if printed on A portrait (8.5`x 11")sheet M yk N 0 50 100 200 300 -' A Feet 0 200 400 800 1200 Map projection: Web Merzabor Comer000rrjinates: WGS84 Edge tics: UTM Zone 13N WaS84 18 O a) » ) O7 O O O) p C O) N N 0 r C Q C O L O co S 0 -- CO is N U (n U 03 O ll• O 0 us to U p C U p7 p L 4) u) r N o C U 00 U tU `O �- a) .- N p -C -o O C v to 4- N E co 0 O 'LJ N E w- C U N co a. Q) O O ` ^ .. 'C N co _. V Q) (n 0 C a) L Z as coto -- o ` u�i � � � (°n � o E °'co am °� (oc °p a� . to U) O E a 0a) �' O a) Ts v c 10 o ai aTi U o f° a) -4- 6 `o Q ~ �' o � � `o a c � � aa)) -o ail m z N ilt ° o a) Q o C in E co o o W N c N 5 Q a) w m 'n � 03 E 0 as c0 L o C a o n o 0. c c 1.o (U L m w o Q c a =1;3i, ` cn o cco (aa o a) Q U Et Li :O O a� � 3m � � � ° � � �; -' U o) roomy LL. o m o v) o o N 3 O ` o v E o � r co o °a5 0 E � as c.) Z (n .a -CD o - .c n2 a) o c y a� E �. EO c a) o C U (a L aJ co Q) .O d O N a N G < >, � � � a) Cl) o m �- U o a� � > °� 3 `mew 0 as E (n .c �, � to J v) N � Co ro w en n c . N ns O CD Z L) Q0 CD a) .. c�6 Q) O N O co E O2 co ) (la a) a a • .as (n C to iv O) 1O O *25 = p c d O 4) U O ') 0 c0 E O co + C F— O C U) L -O -' O .,^ -L7 Q Ca O 'D O. a O C a O a) _ •.-. C m 0 .5 C -c L C (n u) to a c v >,-. E Etn a) Edo = c 0 o auk = o o `� � . CD CI) n _ 0) m Q) O - a) p O Z Q ` co(O o rn MI E s a) > a) (n c o cn co o D �', ca W v V a) a) Cl) C (n co U O (n U C d a) (n N O 'a. E ca (n (v (U j .n `o a. •� c_o c) 0 > — Z .� ca :' o a' .c (U c `!) co -5 a) a) o o p (a o 0 -0 co c a) o o (ao L of m E- w E au) a E w � U a � Q v E- L (n0) u) o aN i_. v .,_ t 0 a a) CC a) 0 t_ D 0 C f ic- 0 n N E T t1V C N C 0 p (l CO C O .C ill 0) = v) 'p - 0 z O C 0 U -co 0t. Oa) ct O .c a) a ( a- E (� o`0 CO to y CC O pTo O W a To' +�-� u) 6" O 8 Z a (n ow a n 2 _, < 3 it V p ea d L W 2 ti C W J tv 3 .a a m m SQ di O O ;) in a 0 0 c0 O o ton o y 0ofi 0 y o u) o < O >. 0 0 r N a 0 0 r N C 0 0 .- N to to r i t O L. C U') U) r t I 0 m to to r t ) o co O N a O O N a p ,.,., i t a a O m ` n' t U) O o tf) N O J t to O 0 to N O a N to O O to N `, < Ca O N U) e- r /t Z C) O N U) r r A Z Q) O N to r r A a) C C C Tr+ i= a3 i3 . to O O O -- d .o ® to N Q to Custom Soil Resource Report Table -Depth to Any Soil Restrictive Layer Depth to Any Soil Restrictive Layer— Summary by Map Unit— Weld County, Colorado, Southern Part (CO618) Map unit symbol Map unit name Rating (centimeters) Acres in AOl Percent of AOI , 41 Nunn clay loam, 0 to 1 >200 52.8 72.3% percent slopes 51 Otero sandy loam, 1 to 3 >200 20.2 27.7% percent slopes Totals for Area of Interest 73.1 100.0% I Rating Options—Depth to Any Soil Restrictive Layer Units of Measure: centimeters Aggregation Method: Dominant Component Component Percent Cutoff- None Specified Tie-break Rule: Lower Interpret Nulls as Zero: No Unified Soil Classification (Surface) The Unified soil classification system classifies mineral and organic mineral soils for engineering purposes on the basis of particle-size characteristics, liquid limit, and plasticity index. It identifies three major soil divisions: (i) coarse-grained soils having less than 50 percent, by weight, particles smaller than 0.074 mm in diameter; (ii) fine- grained soils having 50 percent or more, by weight, particles smaller than 0.074 mm in diameter; and (iii) highly organic soils that demonstrate certain organic characteristics. These divisions are further subdivided into a total of 15 basic soil groups. The major soil divisions and basic soil groups are determined on the basis of estimated or measured values for grain-size distribution and Atterberg limits. ASTM D 2487 shows the criteria chart used for classifying soil in the Unified system and the 15 basic soil groups of the system and the plasticity chart for the Unified system. The various groupings of this classification correlate in a general way with the engineering behavior of soils. This correlation provides a useful first step in any field or laboratory investigation for engineering purposes. It can serve to make some general interpretations relating to probable performance of the soil for engineering uses. For each soil horizon in the database one or more Unified soil classifications may be listed. One is marked as the representative or most commonly occurring. The representative classification is shown here for the surface layer of the soil. 20 Custom Soil Resource Report Map—Unified Soil Classification (Surface) Co M Yi, 53170 531800 531900 532000 532100 532:2CC Ars..•: 40° 26 9 Pl = jam— _ } r ���';—ilt,._ r 40° 26'9"N 't ,,- 1 .„ CD - T U-• - - 4 1• rye .1i.:',. 1 3 $ . I - -%;41111 ille I g ' I v O _, 8 1: O U . ri ,liti . „ I 41 0 4 ri 0 S 4 , ri i .___• �� _�� ri La, , 0 4 ;Sl' f l i 40° 25139"N 531700 531800 531900 532000 532100 532200 532300 Co Map Scale: 1:4,500 if painted on A portrait (8.5" x 11")sheet M Meters N 0 50 100 200 300 $ Feet A 0 200 400 800 1200 Map projection: Web Mercator Corner coordinates: WGS84 Edge tics: UTM Zone 13N WGS84 21 a) In In m cn > Tzt .� 0 C n v v CZ? (v N N N cn N w cu a 4i w o 0 a a a 0 0 0 o a c C a o O 2 o o 2 o O 2 .O cn ay Q .a, a a a a a a. U 2 2 Y 0 H Q Y 9 1 f w v) c9 u) cn co ati in Z S I J J J J J I I -J H O a 2 a. d_ (L S 0 a) c l4 2 2 2 2 `a 2 2 2 O O O d in � cn co cn (� co co (o z 3 U z a w rts d a O m X ,, N l6 �I Cu 3 I- .31 ca cu > to .-v. -o a v v CD 0 y L. a s a s a P O o 0` O 2 0 2 U 2 y a a J a a 0 U 5 a (n (n El Q Y 2 O H C7 C? O C? 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J a a 0 U a a. a a a. m o Q Y S O H O O 0 y O CO Q Y O f— macuL. o a) ant J J J J J J 0 U 5 2 CL CL 7 § 2 = _ _ = J Q en c 0 U U U U U U O 0 C7 0 0 0 0 0 C7 2 2 2 2 2 TG td y u s ' , ® , ■ ® ® ® I ® ® ® D ` 'o 0 a O a) a' O c) O C Q) a) as to co 1- CD C a) 'O (Op Y V Cu Cj U cat cn > U rn o .�- l. . 0 to _ a) p CU L.N., cQ co (V t-' r I y c «. U O C O a p C a) V as to t"' p O Id C V O V ca0 cts monO Q �— O O •C O Z) ?? -.5- ._. - N •—• ,..,c 4co - — U N a. mco 5 co ccoo C o t�'u .. O U tC CL) O N N O E a) a ca ; N coo coo w a) co N to O E O.. O a) N Q) U C6 CJ c6 N o•r)• c as N U Cnitt *- Q -C- .C ca a) a) O _c O N -D CC p r .C u9 p w .n a) E U . co ca L o Q' C M o .ccu c act co c0 n .c co N o �. n .c 2 cn o c c o. c �- co 4) U io .—. ..as c a) u' a ry c -a-- V Oct !v o o Q -o_ O To 3 ca N V ° C a) -? 0 O) '� ui > >, > o o °� 3 o Y o co O CL a) a) — O O to O O U a) E o ,c S] N .O ZJ a3 .+ ro o Q -O . cu 7-7 )- ••-• O N N CY V. .n m cn t p o3 O N c) •O co n N I] a) A � � om v Ica) _ a. .a? ao ,D -n -a i5 v a) � ° a) E O >, Q) 'D a) cn ► �j • a O O O co > O Q) N n L C..) 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O ,_ o co c0 LL w c4 t4 O a) c 3 .3 Q D Z C J A O 2 u Custom Soil Resource Report Table -Unified Soil Classification (Surface) Unified Soil Classification (Surface)— Summary by Map Unit -- Weld County, Colorado, Southern Part (CO618) Map unit symbol Map unit name Rating Acres In AOl Percent of AOI 41 Nunn clay loam, 0 to 1 CL 52.8 72.3% percent slopes 51 Otero sandy loam, 1 to 3 SC 20.2 27.7% percent slopes Totals for Area of Interest 73.1 100.0% Rating Options—Unified Soil Classification (Surface) Aggregation Method: Dominant Condition Component Percent Cutoff.. None Specified Tie-break Rule: Lower Layer Options (Horizon Aggregation Method): Surface Layer (Not applicable) 24 Custom Soil Resource Report Soil Reports The Soil Reports section includes various formatted tabular and narrative reports (tables) containing data for each selected soil map unit and each component of each unit. No aggregation of data has occurred as is done in reports in the Soil Properties and Qualities and Suitabilities and Limitations sections. The reports contain soil interpretive information as well as basic soil properties and qualities. A description of each report (table) is included. Soil Physical Properties This folder contains a collection of tabular reports that present soil physical properties. The reports (tables) include all selected map units and components for each map unit. Soil physical properties are measured or inferred from direct observations in the field or laboratory. Examples of soil physical properties include percent clay, organic matter, saturated hydraulic conductivity, available water capacity, and bulk density. Engineering Properties This table gives the engineering classifications and the range of engineering properties for the layers of each soil in the survey area. Hydrologic group is a group of soils having similar runoff potential under similar storm and cover conditions. Soil properties that influence runoff potential are those that influence the minimum rate of infiltration for a bare soil after prolonged wetting and when not frozen. These properties are depth to a seasonal high water table, saturated hydraulic conductivity after prolonged wetting, and depth to a layer with a very slow water transmission rate. Changes in soil properties caused by land management or climate changes also cause the hydrologic soil group to change. The influence of ground cover is treated independently. There are four hydrologic soil groups, A, B, C, and D, and three dual groups, A/D, B/D, and C/D. In the dual groups, the first letter is for drained areas and the second letter is for undrained areas. The four hydrologic soil groups are described in the following paragraphs: Group A. Soils having a high infiltration rate (low runoff potential) when thoroughly wet. These consist mainly of deep, well drained to excessively drained sands or gravelly sands. These soils have a high rate of water transmission. Group B. Soils having a moderate infiltration rate when thoroughly wet. These consist chiefly of moderately deep or deep, moderately well drained or well drained soils that have moderately fine texture to moderately coarse texture. These soils have a moderate rate of water transmission. Group C. Soils having a slow infiltration rate when thoroughly wet. These consist chiefly of soils having a layer that impedes the downward movement of water or soils of moderately fine texture or fine texture. These soils have a slow rate of water transmission. 25 Custom Soil Resource Report Group D. Soils having a very slow infiltration rate (high runoff potential) when thoroughly wet. These consist chiefly of clays that have a high shrink-swell potential, soils that have a high water table, soils that have a claypan or clay layer at or near the surface, and soils that are shallow over nearly impervious material. These soils have a very stow rate of water transmission. Depth to the upper and lower boundaries of each layer is indicated. Texture is given in the standard terms used by the U.S. Department of Agriculture. These terms are defined according to percentages of sand, silt, and clay in the fraction of the soil that is less than 2 millimeters in diameter. "Loam," for example, is soil that is 7 to 27 percent clay, 28 to 50 percent silt, and less than 52 percent sand. If the content of particles coarser than sand is 15 percent or more, an appropriate modifier is added, for example, "gravelly." Classification of the soils is determined according to the Unified soil classification system (ASTM, 2005) and the system adopted by the American Association of State Highway and Transportation Officials (AASHTO, 2004). The Unified system classifies soils according to properties that affect their use as construction material. Soils are classified according to particle-size distribution of the fraction less than 3 inches in diameter and according to plasticity index, liquid limit, and organic matter content. Sandy and gravelly soils are identified as GW, GP, GM, GC, SW, SP, SM, and SC; silty and clayey soils as ML, CL, OL, MH, CH, and OH; and highly organic soils as PT. Soils exhibiting engineering properties of two groups can have a dual classification, for example, CL-ML. The AASHTO system classifies soils according to those properties that affect roadway construction and maintenance. In this system, the fraction of a mineral soil that is less than 3 inches in diameter is classified in one of seven groups from A-1 through A-7 on the basis of particle-size distribution, liquid limit, and plasticity index. Soils in group A-1 are coarse grained and low in content of fines (silt and clay). At the other extreme, soils in group A-7 are fine grained. Highly organic soils are classified in group A-8 on the basis of visual inspection. If laboratory data are available, the A-1 , A-2, and A-7 groups are further classified as A-1 -a, A-1 -b, A-2-4, A-2-5, A-2-6, A-2-7, A-7-5, orA-7-6. As an additional refinement, the suitability of a soil as subgrade material can be indicated by a group index number. Group index numbers range from 0 for the best subgrade material to 20 or higher for the poorest. Rock fragments larger than 10 inches in diameter and 3 to 10 inches in diameter are indicated as a percentage of the total soil on a dry-weight basis. The percentages are estimates determined mainly by converting volume percentage in the field to weight percentage. Percentage (of soil particles) passing designated sieves is the percentage of the soil fraction less than 3 inches in diameter based on an ovendry weight. The sieves, numbers 4, 10, 40, and 200 (USA Standard Series), have openings of 4.76, 2.00, 0.420, and 0.074 millimeters, respectively. Estimates are based on laboratory tests of soils sampled in the survey area and in nearby areas and on estimates made in the field. Liquid limit and plasticity index (Atterberg limits) indicate the plasticity characteristics of a soil. The estimates are based on test data from the survey area or from nearby areas and on field examination. References: 26 Custom Soil Resource Report American Association of State Highway and Transportation Officials (AASHTO). 2004. Standard specifications for transportation materials and methods of sampling and testing. 24th edition. American Society for Testing and Materials (ASTM). 2005. Standard classification of soils for engineering purposes. ASTM Standard 02487-00. 27 22 K u o H o oin N 'I 7 a A d fl a � or N Z u) Z 13 es N a' E Q.V N M N 43 J � o o U) t) o MNs- iiir N N N O o o CO r 40 er to IC.1-i E N N- CD N CO COo O c at N m 0 0 to o o co N 1 / ci it coo 00 IO[) coO CD O a�> 0 GI 0 0 0 a 0 0 N I O O C a) m S co c v 0_ a a 2 r a o u d 0 0 N a co -C a H Ow E � t = = c o = E• M o 6 4 a a C p _ Cl)a) c) t 13 O 2 am a a n co a. N �v Ce U) `o c o 0 0 0 0 '1 0 a) Sig a o 2 Cn F- 1- d =o O i' c = Q Q Q co t 8 O Q CD 1- N N N a) I— V u a Q Q Q <L Q CO a ._ ' (I) to m co c J U f!) 6 J V) co r E cu " c O CO `o � m � � O ) Ei 0 0 a) COU 0 C) a U ° CV c a. m N Q) 7 >, E 0 E 3 as ° °mj f of al Scc Q E E 0› o o c�., t0 c o " E co a N W o >+ �+ ccv o y co a _c m m m m c a-' U U V) C/) LL N t t N p, 0 0 p) a) CO N CD a, 6 0)a) N 6 r- -▪a N ob. a a tea) ° Ct = 0) U CO 4 CO 0 N O o O O a a) o O N -a c) E N N H E a o O O m Q W .00to TA ° -O c gin c -rs8 ;, C C in = d M S Zr C O O 2 a c c - w .. Z 6 References American Association of State Highway and Transportation Officials (AASHTO). 2004. Standard specifications for transportation materials and methods of sampling and testing. 24th edition_ American Society for Testing and Materials (ASTM). 2005. Standard classification of soils for engineering purposes. ASTM Standard D2487-00. Cowardin, L.M. , V. Carter, F.C. Golet, and E.T. LaRoe. 1979. Classification of wetlands and deep-water habitats of the United States. U.S. Fish and Wildlife Service FWS/OBS-79/31 . Federal Register. July 13, 1994. Changes in hydric soils of the United States. Federal Register. September 18, 2002. Hydric soils of the United States. Hurt, G.W. , and L.M. Vasilas, editors. Version 6.0, 2006. Field indicators of hydric soils in the United States. National Research Council. 1995. Wetlands: Characteristics and boundaries. Soil Survey Division Staff. 1993. Soil survey manual. Soil Conservation Service. U.S. Department of Agriculture Handbook 18. http://www.nres.usda.gov/wps/portal/nres/ detail/national/soils/?cid=nrcs142p2_054262 Soil Survey Staff. 1999. Soil taxonomy: A basic system of soil classification for making and interpreting soil surveys. 2nd edition. Natural Resources Conservation Service, U.S. Department of Agriculture Handbook 436. http://www.nres.usda.gov/wps/portal/ nres/detail/national/sails/?cid=nres142p2_053577 Soil Survey Staff. 2010. Keys to soil taxonomy. 11th edition. U.S. Department of Agriculture, Natural Resources Conservation Service. http://www. nres.usda.gov/wps/ portal/nres/detail/national/soils/?cid=nres142p2_053580 Tiner, R.W. , Jr. 1985. Wetlands of Delaware. U.S. Fish and Wildlife Service and Delaware Department of Natural Resources and Environmental Control, Wetlands Section. United States Army Corps of Engineers, Environmental Laboratory. 1987. Corps of Engineers wetlands delineation manual. Waterways Experiment Station Technical Report Y-87-1 . United States Department of Agriculture, Natural Resources Conservation Service. National forestry manual. http://www.nres.usda.gov/wps/portal/nres/main/national/ landuse/forestry/pub/ United States Department of Agriculture, Natural Resources Conservation Service. National range and pasture handbook. http://www.nrcs.usda.gov/wps/portal/nrcs/ detail/national/landuse/rangepastu re/?cid=stelprdb1043084 29 Custom Soil Resource Report United States Department of Agriculture, Natural Resources Conservation Service. National soil survey handbook, title 430-VI . http://www. nrcs.usda.gov/wps/portal/ nres/detail/soils/scientists/?cid=nres142p2_054242 United States Department of Agriculture, Natural Resources Conservation Service. 2006. Land resource regions and major land resource areas of the United States, the Caribbean, and the Pacific Basin. U.S. Department of Agriculture Handbook 296. http:l/www. nres.usda.gov/wps/portal/nres/detail/national/soils/? cid=nrcs142p2_053624 United States Department of Agriculture, Soil Conservation Service. 1961 . Land capability classification. U.S. Department of Agriculture Handbook 210. http:// www.nres.usda.gov/Internet/FSE_DOCUMENTS/nres142p2_052290.pdf 30 Hello