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TREE PRESERVATION POLICY <br />die or appear to be dying within one year of planting by the person <br />responsible for the planting. <br />c. Before any construction or grading takes place, snow <br />fencing or erosion control fencing shall be placed around the <br />borders of woodlots of the driplines of large trees to be <br />preserved. Signs shall be placed along this fence line prohibiting <br />grading beyond the fence line. <br />SECTION V. TREE AND SITE RELATED DISTURBANCES <br />A. Tree protection zones, specimen trees or stands of trees <br />designated to be saved must be protected from the following damages <br />which may occur during all phases of land disturbance and <br />construction processes. Methods of tree protection and disturbance <br />prevention are provided in Section IV. <br />1. Direct physical root damage <br />2. Indirect root damage <br />3. Trunk and crown disturbance <br />B. Direct physical root damage most frequently occurs during -s -ite <br />clearing and grading operations, where transport or feeder roots <br />are cut, torn, or removed. <br />1. Transport and feeder roots tend to tangle and fuse among <br />the roots of adjacent trees. The removal of trees with heavy <br />machinery along the outer periphery of a tree save area. <br />2. The most substantial form of root damage for all root types <br />occurs in the form of cut roots. Roots are cut in grade reduction, <br />or from trenching for underground utilities, sanitary sewer, or <br />storm sewer lines. <br />3. A more subtle type of root damage is the loss of feeder <br />roots. Feeder roots normally occur within the organic layer, and <br />the surface four inches of top soil, subsequently, these roots can <br />be easily damaged by the track action from a single bulldozer pass. <br />The stripping of top soil within a tree's critical root zone can <br />totally eliminate its feeder root system. <br />C. Indirect root damage through site modification can result from <br />positive grade changes, temporary storage of fill material, the <br />sedimentation of erosion materials, soil compaction, and soil <br />chemical changes. <br />1. Positive grade changes from fill and sedimentation causes <br />a decrease in soil oxygen levels. An increase in soil carbon <br />dioxide and other toxic gases can also occur, leading to large <br />areas of anaerobic conditions. Anaerobic soil conditions cause a <br />decrease in the root respiration process which is essential for the <br />uptake and transport of minerals and nutrients. <br />2. Anaerobic soil conditions are also,produced by soil <br />compaction, the increase in soil bulk density with a decrease in <br />soil spore space. Compacted soil is also impervious to root <br />penetration, and thus inhibits root development. Soil compaction is <br />generally caused by the weight and vibrations of heavy machinery, <br />vehicle parking, and the storage of fill and /or construction <br />Page 4 <br />