Soil Compaction
                 Big dogs and beautiful lawns are not compatible. If you want 
                  a beautiful backyard, don't think that you can turn a dog or 
                  even rambunctious children loose to romp and stomp. 
                 The pitter-patter of little feet signal devastation to lawn 
                  grasses. Not only do grasses suffer, but all plants, even the 
                  majestic redwoods of California, cannot endure the consequences 
                  of foot steps. Giant Sequoia trees, over 2,000 years old, began 
                  to decline for no known reason. Finally it was discovered that 
                  hundreds of people walking around and around at the base of 
                  the trees and looking up—fascinated by the size and height 
                  of the trees—were trampling to death these natural monuments. 
                  The problem? Soil compaction.
                 Compaction destroys soil structure, thus increasing density, 
                  carbon dioxide concentrations (plant roots need oxygen to live 
                  and grow) and heat build-up. Additionally, it creates surface 
                  runoff rather than allowing water to penetrate the roots. Compaction 
                  subsequently decreases the amount of large pore space available, 
                  as well as oxygen in the soil, water penetration, and nutrient 
                  influx.
                 When compaction increases soil density, root elongation is 
                  inhibited, causing poor development of root systems essential 
                  for summer survival. This damage is more severe in drier, heavier 
                  soils.
                 Plant roots need oxygen to survive, and as the density of 
                  a compacted soil increases, carbon dioxide and other toxic gasses 
                  do not readily move from the root system. Their concentration 
                  can build up to the point that they actually become toxic to 
                  the root.
                 Compaction is very much a surface phenomenon affecting mainly 
                  the top 4 inches of soil. Compacted soils do not allow rapid 
                  water penetration, causing increased runoff. This means that 
                  more irrigation is necessary to adequately soak compacted areas 
                  to get water to the root-feeding zone during times of drought 
                  stress.
                  Compacted soils are hotter in the summer and colder in the winter 
                  because of the conductivity of tight soil particles. Lower temperatures 
                  in the spring could result in less root growth, delayed green-up 
                  and even winter- kill.
                 Porosity of compacted soil is less. Both the numbers of pores 
                  and their size are decreased. Small pores in soil are usually 
                  filled with water, so water begins to replace air in a compacted 
                  soil. In the absence of air, plant root cannot actively absorb 
                  nutrients, causing plant decline. Pathogenic fungus organisms 
                  thrive in higher soil temperatures in the presence of a lack 
                  of oxygen. Thus, the probability of summer disease problems 
                  is increased in a compacted soil. Weeds that can persist in 
                  low oxygen soils can gain the competitive edge over desirable 
                  grasses and take over.
                 Managing turf to minimize the negative effects of compaction 
                  is important. Management considerations that are helpful in 
                  this regard include aerification, traffic control, water management, 
                  soil modification, efforts to both improve drainage and irrigation 
                  design, and turf grass selection.
                 Core aerification is extremely beneficial in increasing air 
                  exchange, water infiltration rates, water retention, nutrient 
                  penetration and thatch decomposition. It also decreases surface 
                  runoff, therefore increasing water- use efficiency while reducing 
                  total irrigation requirements. Warm-season grasses such as St. 
                  Augustine and bermuda can be beneficially aerified from the 
                  time they green-up until the time they go dormant in the fall. 
                  Once-a-month aerification on heavily trafficked Bermuda grass 
                  would not be detrimental. Total number of aerifications per 
                  year needs to be linked to fertility levels and amount of traffic. 
                  Two to five aerifications per year should be considered average 
                  for heavily-trafficked turf.
                 Minimizing traffic whenever possible is important. Minimizing 
                  traffic when soil is wet is critical because compaction damage 
                  is greater on a wet soil than on a dry soil. Timing irrigation 
                  to allow adequate time for drainage prior to traffic can be 
                  a critical factor in reducing compaction damage. 
                 For more information about dog and animal compaction control, 
                  see: 
                http://aggie-horticulture.tamu.edu/plantanswers/turf/dog_lawn_problems.html