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ge equal to one square kilometer or 1 hectares. The design of the field lay out is perfect checker-board design with cane roads running parallel to each other 1,0 meters apart in general northwest to southeast direction on one side and the crossing roads running from northeast to southwest in the other direction. IV-2 Of the total 1 lots, as result of the governments decision to hand back land to owners who had their lands expropriated, total of 4 lots will be or have already been returned to their previcus owners. 2. Soils The soils of the Victoria de Julio cane supply area can be generally grouped into two orders: mollisols and vertisols. Mollisols, or locally known as "Suelos Rojisos", have been classified into four series: Chilamatillo (ch), Finlandia (Fn) El Triunfo (Tr) and Los Laureles (Lr). These soils are of volcanic origin and occupy the higher elevations and present gentle undulation to near flat level soils. Their depth runs to 8 -1 centimeters overlying semipermeable horizon. These soils have good physical and chemical properties although it is reported that available phosphorous is moderate to low. Vertisols are known locaiiy as "Suelos negros" and are made of over 1 different soil series, the major ones being: San Nicolas (Sn), San Isidro (Si), Malacatoya (My), and El Coyol (Ec). These soils were formed by alluvial deposits or by erosion from areas of higher ground and occupy the lower areas of the project. Generally they lie over cemented volcanic material with depths to this horizon ranging from 8 to 1 centimeters. These soils do not show signs of erosion. They are generally heavy soils with high clay content. It is reported that up to 7% of the clay constituent is of the montmorillonitic type. These clays expand when wet and contract and crack when dry. When wet they become almost impermeable and very difficult to work with. Judging from cane yields-to-date since the projects first crop, it would appear as if th