Laserfiche WebLink
CYCC - .Sediment Yield Demonstration Eckman Park Area 41 <br />• 1.0 INTRODUCTION <br />Colorado Yampa Coal Company (CYCC) is in the process of requesting a Phase Iii bond release for Area 41 <br />(238.41 acres). This area is covered under Colorado Yampa Coal Company (CYCC) -Mine 1, Mine 2, and <br />Eckman Park Permit No. C-81-07I and is located approximately 20 miles southwest of Steamboat Springs, <br />Colorado. CYCC has developed the following sedimentology demonstration in support of this application. <br />According to Division of Minerals and Geology (DMG) Regulation 3.03.1(3)(b), no more than 60 percent of the <br />bond can be released until the applicant demonstrates that existing conditions will result in equivalent or lesser <br />sediment contributions to surface runoff when compared with predisturbance conditions or undisturbed areas. <br />The following information is provided to meet the requirements of the specified demonstration. <br />The post-mining land use for Eckman Park has been defined as pastureland. Slopes average approximately 12% <br />across the reclaimed area. The maximum slope, approximately 49%, in this reclaimed azea is located on the <br />overburden stockpile #2. <br />The approved reference area is the pastureland reference site located just west of Pond A in Eckman Par1c. The <br />topography in the Pasture Reference Area varies significantly from the reclaimed areas in Eckman Park in that a <br />much gentler slope prevails. The average slope measured on the Pastureland Reference Area is approximately <br />2.1%, while the average slope of the reclaimed areas is approximately 12%. Due to the significant topographic <br />difference between the reference area and the reclaimed area, it is inappropriate to develop a direct sediment yield <br />comparison between the areas to satisfy DMG Regulation 3.03.L(3)(b). In the alternative, CYCC will utilize a <br />• model to compare the runoff from Blocks East and West to adjacent undisturbed pasturelands. <br />A SEDCAD+ model has been developed by CYCC to demonstrate that runoff from the reclaimed area results in <br />equivalent or lesser sediment contributions to surface runoff when compared to adjacent undisturbed conditions. <br />SEDCAD + is a computer software program developed to assist in the evaluation of stornwater runoff, erosion, <br />and sediment control management techniques. <br />The 1998 Area 41 vegetation survey conducted by CYCC and available soils information from the existing permit <br />document were utilized as input to the SEDCAD+ program. To develop a comparative model for unmined <br />adjacent areas, CYCC utilized vegetation information derived from the 1998 Eckman Park Reference Area <br />vegetation survey conducted coincident with the Area 41 survey. This reference area has been established as being <br />representative of the vegetation found in adjacent, unmined lands. OI/ <br />The reclaimed area and associated reference area boundaries do not coincide with watershed boundaries; therefore, <br />representative portions of the areas are modeled on a small scale tt~th model inputr selected as appropriate to <br />^ distinguish those characteristics unique to the reclaimed area. Grading practices which enhance surface <br />111~"AJ roughness, reduce the length of overland flow, and increase infiltration are the primary modeled attributes which <br />strengthen the reclaimed areas ability to reduce suspended solids concentrations. <br />To model areas with similar topography and soil apes. CYCC combined the vegetation survey information for the <br />Pastureland Reference Area with information on the topography and soil types determined for Eckman Pazk. The <br />so es and topo ttnd-in Ec k are similar to the soils and topography found in adjacent <br />unmined ar Thc Reference Arca soil hpe an vegetation data were modeled with the topography of the <br />• reclaimed areas small watershed for comparison with the reclaimed areas. By <br />modeling comparable adjacent areas in this manner, the sediment }field demonstration provides a reasonable <br />companson of the success of the rcvegctatton efforts and their effectr on surface runoff and sediment loads. <br />• i rn~enrimmnrnul4YAm`hunJrcl!v.a41 d.x <br />