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7-14-04; 17:40 ;Lester Bullding ;3203955376 # 21/ 28 <br /> Article Request Page Page 19 of 26 <br /> on a comparison of the bulk density of in-situ hydrated concrete(2.2+Mg/m3)and that for <br /> normally-hydrated concrete with a 0.26 W/C ratio(�1.9 Mghn3). Second,the confinement of a dry <br /> mix prior to hydration helps keep particles together during the hydration process and ttris <br /> counteracts the hydrostatic pressures that work to drive the particles apart when excessive water is <br /> brought into a mix.Third,during the normal hydration process,cement particles begin to giow <br /> while the ingredients are still bein�mixed,and these growing particles are surrounded by water. <br /> Consequently,the hydrating cement particles aze not in direct contact with aggregates and other <br /> cement particles during early stages of hydration,and when there is excessive water in a mi7c,they <br /> may make only minimal contact after hydration is complete. <br /> Uniformity of Compacted Miz <br /> The main advantage that normally-hydra.ted concrete has over in-situ hydrated concrete is that <br /> mixing of ingredients after the addition of water helps disperse cement particles more uniformly <br /> thmughout the mix. In other words,water serves as a cement-dispersing agent in normally-hydrated <br /> mixes.In the case of in-situ hydration,one must rely on the pmper mixing and placing of the dry <br /> ingredients,that is,mixing and placing that does not result in the separa.tion of cement,fine <br /> aggregates and coarse aggregates.Separation of cement and fine and coarse aggregates can occur <br /> as bagged dry mix is transported,as dry mix is taken from the bag and placed into forms/molds, <br /> and as it is vibrated or otherwise compacted into forms/molds.Variations in the degree of such <br /> separation from footing to footing would explain the higher than expected differences between <br /> footing replicates as highlighted in Table 3. <br /> Research is needed to assess m�thods for producing dry conerete mixes that will be characterized <br /> by a uniform dispersion of cement after being compacted into forms/molds. Such methods include <br /> (1)special treatmenta that adhere/attach dry cement particles to aggregate surfaces prior to bagging, <br /> and(2)methods to reduce segregation during bagging,transporation and placement of dry concrete <br /> mixes. <br /> Introdncing Water into a Dry Concrete Miz <br /> When in-situ hydration was found to produce concrete with significant stcength during the post <br /> uplift resistance study(Bohnhoi�e�al.,2001),one of the main unanswered questions was"Where <br /> did the water come from7"More specifically,was the dry concrete mix hydrated by rainwater <br /> movitwg down thmugh the ground via gravitational forces,or water drawn into the mix and <br /> surrounding area by surface tension(i.e.,capillary action)?It was primarily in pw�suit of an answer <br /> to this question that led to the three water treatmenta featured in this study.Water treaiment A was <br /> eatablished to provide a situation in which all dry concrete mix would be hydrated via the capillary <br /> rise of water.Water treatment B represented a situation in wluch in-situ hydration was prunarily <br /> due to water moving downward by gravitational forces.Water treatment C represented hydration <br /> by a combination of gravitational flow and capillary rise. <br /> Based on averages listed in Table 3 and plotted in figure 14,one can conclude that there was not a <br /> significant difference in the compressive strengths of footings subjectsd to water treatments A and <br /> thoae subjected to water treatment B.This is not surprising since water treatments A and B <br /> produced somewhat similar soil moisture content levels at the various monitored depths(see <br /> figiues 8 and 9).'Thie becomes clearer when the sawtooth plots in figure 9 are smoothed. <br /> � Similar soil moisture content profiles in tanks 1 and 2 and tanks 3 and 4 can be attributed to a <br /> combination of�factors.First, groundwater table heights in tanlcs 1 and 2 were probably only <br /> about 5 cm(2 in.)}ugher than in tanks 3 and 4. Second,capiUary fringe depth was approximately <br /> , equal to the depth of sand in each tank(i.e.,capillary fringe depth is equal to the total height of <br /> capillary rise above the water table).Thus,even though water was not sprinkled on the tops of <br /> http://asae.frymulti.com/request2.asp?JID=S&AID=14082&CID=1n�003&v=&i=&T=1 6/4/2004 <br />