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<br />r-- <br /> <br />y~ <br />":'"~"l <br />01 <br />(~.:.-~ <br />C <br /> <br />fan having less than a one percent gradient. Only scattered small tracts <br />and some broad areas of bottom land have an uneven surface rendering irri- <br />gation practices more difficult or requiring considerable leveling and SOme <br />grading. Extensive areas of bottom land bordering the streams and several <br />hummocky, gravelly-soil tracts on the outwash plains have a topographic <br />character which precludes their economical development. <br /> <br />The system of sUbirrigation, somewhat exclusively practiced in other <br />parts of the San Luis Valley, is demanding of an exacting micro-relief and <br />nearly smooth land surface in order that the level of ground waters can be <br />maintained at a uniform, shallow depth to achieve maximum crop production, <br />The prcvision of an adequate water supply for the Conejos Division would <br />favor an increase in th8 present extent to which subirrigation is employed, <br />and considerable land leveling would, therefore, be undertaken to attain <br />the finer degree of gradient and surface requisite for this practice. <br /> <br />".-, , <br /> <br />Drainage <br /> <br />The higher-lying, coarse-textured soils of the outwash plains exhibit <br />good to excessive drainage characteristics, altheugh there are numerous <br />scattered depressions and swales where some seepage and accumulation of <br />water occurs. The principal preblem of inadequate drainage extends through_ <br />out the bottom lands and in a region of floWing wells north of Manassa and <br />Sanford where ground water from the higher lands accumulates, bringing the <br />water table close to the surface. The necessity for flood control is <br />apparent where seasonal floods inundate the lowcst tracts along the river <br />and contribute to high water table conditions, but substr~tial lowering of <br />the high ground-water table will not be effected by the control of floods <br />alone. <br /> <br />Salinity and Alkalinity <br /> <br />The majority of soils are relatively free cf excessive concentrations <br />of ~oluble salts and are not highly alkaline. Coincident with seepage and <br />drainage problems, the lower-lying lands, particularly those situated <br />north of Sanford, are affected by mCderate to high accumulations of salines, <br />the soluble salt content in many cases exceeding one percent. Many of, them <br />are open, porous and r.ot strongly alkaline, and the possibility of their <br />reclamation by leaChing, drainage and other measures appears favorable. <br />Several areas of structure less, solonetzic soils cannot be Successfully <br />reclaimed. <br /> <br />Land Classification <br /> <br />A detailed classification of the lands in the Conejos Division was <br />completed to determine the extent and character of the lands and their <br />suitability for irrigation agriculture (See Conejos Division'General Land <br />Classific~tion,Map). The survey involved the determination and delineation <br />of the lands into six classes acc~rding to productive capacity, establishad <br />in respect to and by consideration of factors of SOils, topography and <br />draina<ge. The classification standards used in the survey to accomplish <br />thi~ ,segregation are defined as follows: <br /> <br />1'7 <br /> <br />, <br />