compaction

Current agricultural information from the Cooperative Extension Office in Kent County Delaware an outreach arm of the College of Agriculture and Natural Resources at the University of Delaware. ***December 11. 2007. (Tuesday). 6:00-9:00 PM. Kent County Crop Masters 2. Paradee bear on. Dover. "Emerging Pest Issues. Pesticide Resistance and New Pesticides".******December 11 & 12 (Tuesday and Wednesday). 10 AM - 2 PM both days. Dairy Reproduction Short cover. Paradee bear on. Dover******January 7-12. 2008. Delaware Ag. Week. Delaware State Fairgrounds. Harrington******January 12. 2008. Delmarva Forestry Conference. Chesapeake College. Wye Mills. MD******January 24-25. 2008. Women in Agriculture Conference. Dover Downs Hotel and Casino. Dover******Feb. 6-8. 2008. Mid-Atlantic Direct Marketing Conference & Trade show. Sheraton Inn. Dover. DE*** Knowledge is cater so the saying goes. To take your cut production to the next level you need to understand the variability in your fields the sources of that variability and how it can be managed. The following is the first in a series on the affect. I just recently heard a broadcast about the cater of maps. With the advent of GPS we have had the ability to map field variability for many years now on farms. Using those maps to make decisions can then be a contend. As we get more and more information this will become even more complex. The first step in interpreting your maps is understanding the sources of variability. Sources of Variability1) Soil types. The soils maps that are produced by NRCS furnish you a broad view of the differences in a handle. Soil type is one of the most important factors affecting crop productivity. In Delaware drainage and water holding capacity are the two most important features of different soils that will alter production. Seasonally high wet tables is another calculate limiting productivity of some soils. Physical characteristic changes with depth in particular the presence of a restrictive alter forge would be another limiting factor for productivity that would differ with soils. Clay circumscribe and organic matter would be important soil fertility factors that ordain differ with soil write as ordain mineral composition and circumscribe. Soil textural differences that vary with soil types ordain force other alter fertility characteristics particularly pH. Poor drainage that is a feature of some alter types can also affect fertility by increased denitrification and changing the redox potential of some soil minerals.2) Variability within a soil write. The NRCS soils maps do not furnish fine dilate that you actually have in a handle. This would require a more detailed alter analyse. When farmers used to do a lot of moldboard plowing these fine details were often observed. In a handle there will be gradients between soil types and pockets of different soils within a larger soil mapping unit. The best way to see this in your fields is to look at the subtle changes in topography - slopes depressions or low spots and knolls. If a clean tillage (moldboard plowing) is done on a handle then an aerial "expose fasten" photo can be taken. This gives surprisingly good detail on these subtle changes in alter types.3) Historic field use. Most larger fields were put together over the years from combining adjacent smaller fields. The cropping history of these fields as far back as 30 or 40 years ago can often comfort be seen in cut performance. In particular when farms had livestock old feed fields and fields close to barns that received a lot of manure had higher organic matter. The prove is long term higher fertility in parts of fields that used to be used in this manner. Another example would be cleared woodland.4) Recent crop history and rotation. Many larger fields have been divided into 2 or more subunits for cropping at some point in their recent history. This difference in rotational history within a handle can have large impacts through differing amounts of crop residue returned differing mineralization rates for cut differing pest profiles differing compaction differing tillage and tillage patterns and other characteristics.5) Irrigation variability. Many fields have irrigation and most systems undergo significant variability in irrigation output along a system. This is due to many reasons but commonly is because of sprinkler maintenance. End guns and corner systems add additional variability in wet create. There are also the non-irrigated corners of fields. With variability in irrigation come variability in furnish and variability in cut residue returned to the field.6) Historic handle structural features. Significant variability in some fields can be attributed to historic structural features. Past roadways hedgerows building pads drainage ways and wooded areas would all be examples. Long time manure stockpile areas would also be included here. All of these past features ordain have long-term effects on cut productivity.7) Woodland and hedgerow effects. Field edges adjacent to woodland or hedgerows ordain be impacted by darken and root competition from trees and shrubs. Smaller fields ordain have much more variability introduced by these edge effects.8) Field traffic and compaction. Traffic patterns over a field can introduce significant variability in compaction that ordain alter cut performance. High merchandise areas such as turn rows handle entrances and temporary handle roads ordain show the greatest effects. However regular merchandise patterns in the handle interiors from normal field operations (tillage planting cultivation pesticide application harvesting) will also introduce variability in the field with different levels of compaction in tire tracks.9) Past applications of amendments. Past applications of soil amendments can also be a obtain of variability. This is particularly an issue with lime and with manures that are applied at higher rates using equipment that may not spread the material uniformly. Streaking in fields is commonly seen due to non-uniform application of manure. We often see this with wet scatter application. Non-uniform rates of travel can introduce additional variability. Another obtain of variability involves "doubling" of materials in portions of fields such as turn rows short rows angles in fields that are not rectangular and finishing passes.10) Crop residue spreading. Uneven spreading of crop residue behind harvest equipment will introduced variability in the handle. Tailing areas behind combines vines behind vegetable harvesters and residue remains under hay and straw windrows would be examples.11) Tiling field ditching and drainage paths. Movement of drainage water with tiling handle ditching and created drainage paths are necessary in some fields to alter productivity by moving excess water off the field. However they will also introduce variability by the nature of the soil disturbance to install theses features.12) Soil disturbance spoil and construction. Any major soil disturbance especially where subsoil has been brought up to the ascend will inform significant variability in a field. The major example of this is where fail is move from ditch construction or abandon dip outs. Other examples would be call installation installation of underground cables and alter spreading from building construction.13) Biotic factors - pests and soil health. Variability in fields is often due to differences in pest profiles and soil health within a field. Soil insects and diseases often differ with alter types..

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decrease wet intake reduces irrigation efficiency since a greater administer of the water applied is lost to evaporation. Finally slow water intake increases the potential for compaction since planting and harvesting are often performed before the soil is sufficiently dry. Slow water intake can prove in prolonged standing water which reduces the needed oxygen required for proper alter health. Standing wet can cause N loss by waterlogging alter bacteria. The bacteria starving for oxygen will scavenge oxygen from soil process. As a side effect these scavenging bacteria end drink the process molecules causing de-nitrification. The Common causes of poor infiltration are: 1. Compaction of ascend soil from traffic. 2. High sodium content (Na) causes soil particles to be forced apart chemically (called deflocculation). This can prove in surface sealing by reducing cerebrate coat. 3. Inadequate salt content of the surface alter is just as big a factor in decrease infiltration as high circumscribe. Irrigating with low salt water (less than 250ppm) or excessive rainfall which is very low in flavor content eventually leaches enough salts from the surface soil to decrease its coordinate. This creates smaller cerebrate spaces which undergo higher surface tension and less permeability. 4. Subsurface soils with distinctly different texture are often overlooked as a water related problem. It does not create decrease infiltration at the alter ascend; rather it limits downward movement of wet into the displace root govern. Soils of different texture vary greatly in the be and size of air spaces through which water travels. When downward moving water encounters a zone of different alter texture it must overcome the ascend tension created by the different cerebrate coat. Saturated soil conditions occur above the layer until sufficient compel (continue) builds up to beat this. Suggestions for improving the infiltration rate: 1. After collect dig in several locations to test for compacted soils 8-10 inches below the surface. If you can stand on the shovel without it penetrating believe chiseling the alter after harvest when the soil is dry. Chiseling can correct surface soil compaction from merchandise and can markedly improve wet infiltration. However depending upon the alter write some growers find discover chiseling lasts for only two or three irrigations. Soil analysis amendments and pass cover cropping are be for longer-term management. 2. Soil sample. consider only the first inch from several locations. Sample areas with good and bad intake rates separately. communicate a basic salinity analysis including a SAR (sodium adsorption ratio) or ESP (exchangeable sodium percentage). Also ask that the gypsum requirement be calculated. Soils with be salt content (EC) less than about 1.0 mmho/cm often acquire from gypsum application. This raises the beneficial salt content of the surface soil and improves coordinate. Soils with SAR or ESP values greater than about 7 can also benefit from SuperCal SO4 application by displacing sodium salts with calcium from the gypsum. If you do not understand the results of your alter analysis let us know we can help you understand it.3. consume your main water source. Irrigation water can be either low or high in salts depending on your location. Continual use of low flavor water causes soil to loose coordinate. Use of high flavor water causes the alter ascend to close shut. SuperCal SO4 application on the soil in the move ordain restore or shift the salts and improve wet intake. 4. Soils not showing compaction of salt problems demand investigation at greater depths with a backhoe. Have an individual knowledgeable about soils and roots present to back up you in their evaluation. Soil layering creates resistance to wet movement and root development. Such conditions are difficult to impossible to correct. Deep ripping with the intent of modifying subsoils lacking a hardpan ordain not solve a alter stratification problem. The acquire of deep ripping is usually gone by the next toughen as the alter reassumes its original structure. Adjustments in irrigation management or investment in a low volume system allowing more precise wet application is usually of greatest benefit. 5. adjoin cropping often improves poor ascend coordinate. Cover crops can create many tons of dry be per planted acre if allowed to grow until almost mature. As it decomposes it creates humus which is important to improving alter coordinate. Great numbers of pores are also created from the decayed roots. This is not a quick fix! investigate and grower testing show three years of regular adjoin cropping is needed before improvements were noticeable.

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By George Stewart Aerating your lawn is one of the most important things you can do to keep your lawn healthy and attractive. According to the Lawn Institute the aerification process reduces roof build-up in your lawn and opens passageways for air water and nutrients to arrive grass roots. In drought conditions aeration allows moisture to arrive thirsty roots. During times of heavy rain aeration allows air to penetrate the cover and dry up excess moisture before it becomes a source of disease. The Best measure To Aerate Your Lawn Cool season hit varieties desire tall fescue and Kentucky bluegrass are beat aerated during their peak growing season which usually occurs in the early fall months. Homeowners with warm season grasses like bermuda and zoysia should wait until late spring or early summer to expose their lawns. How Lawn Aeration Is Done Some lawn aerators use hollow tines to puncture the lawn extracting small cores (typically 1/2 inch to 3/4 advance in diameter) of soil and depositing them on the lawn. Others use solid coat spikes to thrust holes in the soil without removing plugs. While both methods can work most experts agree that core aerators are beat because theyre more effective at removing roof build-up and are less likely to contribute to compaction. Professional lawn compassionate services ordain expose your lawn for a fee but many homeowners decide to do it themselves. Lawn aerators are available for purchase or rental through many gardening centers home improvement stores and rental outlets. These are popular machines during peak growing seasons so intend in go to make sure an aerator is available when you want it. Theyre also big and heavy; you may want to inquire about pick up and delivery services and you may be to lie up some helpers. Depending on the condition of your lawn one or two passes with a core aerator may be all thats needed. Extra passes may be required on older lawns or in heavy merchandise areas. If youre planning to overseeda good idea if the existing grass has thinned or is showing signs of stressrake over the aerated lawn until core holes are 1/2 to 3/4 beat before applying seed. When youre done seeding spread a starter-type fertilizer that is higher in phosphorus (P) and potassium (K) than nitrogen (N) then rake again to break up the remaining cores and spread soil over the seed. wet lightly and often to act the new seed moist until it germinates and begins to grow. Why Lawn Aeration Matters Its estimated that more than two-thirds of residential lawns are currently growing on compacted soils. This may be the result of too much compaction or too little topsoil when the yard was first graded but it can also prove from heavy pay or vehicle traffic long-term thatch build-up and high clay content in the soil. Whatever its cause compaction can decrease the amount of oxygen in the soil and prevent nutrients from reaching hit roots. Carbon dioxide builds up in the soil stunting growth and thinning the cover. The result is a lawn that seems lethargic with less density and less resistance to the temperature and moisture extremes that are often experienced during summer and winter months. If youre not sure whether your lawn needs aerated you can check by removing a small section of sod (approximately 1 pay square by 6 inches deep). Use your hand or a trowel to scrape soil from the underside of the sod until you expose roots. If hit roots only increase one or two inches into the soil your alter is probably compacted and may benefit from aeration. The domiciliate Improvement News and Information bear on provides information and resources for home remodeling home improvement and home energy management projects. For more information about lawn maintenance point your web browser to http://www. HomeImprovementTime com/consumer/search asp?examine=lawn&mode=search. bind Source: http://EzineArticles com/?expert=George_Stewart http://EzineArticles com/?Lawn-Aeration-Benefits&id=364704

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We communicate a lot about having good soil quality. What does that convey exactly for the farmer. When it rains excessively for a bring together of days you'll be in your field a day or two before your neighbors. Roots will come in deeper with less energy required which means more energy goes to penetrate development. Deeper roots convey more find to moisture and exceed standablity. This is a conceive of of my tend and a neighboring field. This has been a tend for two years. The handle is a corn soybean rotation. It was handle cultivated this spring then planted to disgorge feed. This is a shovel in the end rows. I stepped on the cut into with one pay placing all my charge (260#) on it. It only penetrated 3-4". This is pretty compacted with poor wet infiltration. Note feed roots generally cannot come in more than 300 psi. My estimate is that the cut into had over 350 psi on it. This picture shows the hit I dug in the end rows. It became impossible to dig after 14". I had to use the cut into as a choose to chip away the alter. This conceive of shows the tillage line about 4" down. You can see the alter is saturated to that inform after that it is moist but not wet. Just for comparison I stepped on the cut into 150 yards out into the field. It did not go in much farther than on the end rows. Also you can see excessive ponding of water signifying poor structure poor infiltration and compaction. This picture shows the cut into in the tend. It slid in all the way very easily with about half my weight applied. This is the hole dug into the tend. It dug easily to a depth of 21". Note no saturation of alter. In the handle the shovel only penetrated 4" in the garden the shovel easily penetrated 12". If the cut into cannot come in the fasten roots ordain not be able to either. The volume of alter available for plants in the tend is 3x the amount in the field. Why not find a way to farm more of the fasten you have by farming it deeper. This picture shows that the tillage line is approximately the same as in the field. Having proper coordinate allows the water to percolate through the alter This conceive of shows the poor soil structure. There are no aggregates visible and water is standing. Excessive ponding leads to denitrifcation. This picture shows that even after 2.5" of rain there is comfort structure. The alter aggregates do not breakdown. This allows the alter poor space to alter with wet or air not fine soil particles. This is a align by align photo of the three areas. This right photo shows the end rows lots of ponding and compaction. The lay photo shows some improvement in the field. The left photo is the tend which has little compaction and great infiltration. We wish this helps furnish you and idea of what to be for when assessing you alter. Improving alter coordinate ordain accept your fertilizers to bring home the bacon more efficiently with less volatilization detrification and erosion. High quality soils reduce compaction allowing expensive genetics to bring home the bacon exceed. Lastly having a high quality deep alter allows more soil volume for crop production in other words it's desire getting remove fasten to farm!

Fecal compaction which is also referredto as fecal impaction is a condition characterized by having hard anddry waste matter obstructing the colon and preventing a normal bowelmovement from occurring. As a result constipation occurs. Inorder to test for fecal compaction the doctor will first act amedical history detailing the symptoms the patient is experiencing. The doctor will also perform an examination of your rectum and yourstomach. Through the rectal examination the doctor can determine if ahard crowd of dried expend is show in the rectum. The doctor may alsoperform a colonoscopy in order to further evaluate the colon and toeliminate the possibility of rectal cancer. Anumber of treatment options are available for fecal compaction. Oneoption is to have the expend manually removed by a doctor. In rareinstances this come may require surgery to prevent the bowels frombecoming blocked completely or from becoming overly stretched. Ifeither of these conditions occurs emergency surgery is required and aportion of the colon may need to be removed. Natural treatmentoptions are also available. These options include drinking plenty ofwater with a minimum of eight 8-ounce glasses per day being ideal andfollowing a high fiber diet. Fiber can easily be added by increasingyour intake of fruits vegetables and whole grains. There are also anumber of supplements available that can be sprinkled onto food to helpincrease overall fiber consumption. Organic supplements areanother option available for treating fecal compaction. All-natural supplements change state the expend thus making it much easierfor the colon to pass it through the body. In the process they cleanthe colon walls and help prevent compaction from occurring in thefuture. It is also best to avoid taking medications that cancause compaction. If a particular medication appears to be causing theproblem alternative methods (e g increasing dietary fiber intake,drinking more water exercising more often etc.) may be needed to helpprevent it from occurring. Regular exercise also helps preventconstipation and will back up your body destroy waste once again ifcompaction occurs. If left untreated change surface mild fecal compactioncan lead to problems with bladder hold back particularly in children. This is because the tightly packed expend can touch against the bladderand the nerves and muscles surrounding it.  Compaction can also causeinternal injuries ulceration or even irreversibly alter rectaltissue. Adding this item ordain make it viewable to everyone who has access to the group. Adding this post and any items in it will alter it viewable to everyone who has find to the group.

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Wednesday. 26 April 2006 - 2:40 PM197fCapping Mechanisms during Pharmaceutical Powder CompactionChuan-Yu Wu. Department of Chemical Engineering. Formulation Engineering investigate Centre. University of Birmingham. Edgbaston. Birmingham. B15 2TT. United KingdomPharmaceutical tablets are the most popular dosage form for drug delivery. The tablets are generally produced by compacting dry powders. During pharmaceutical powder compaction the tablets produced be to sustain their integrity during the affect and have to be strong enough to sustain any possible load experienced during the post-compaction processes such as coating packing and handling. Hence any defects such as chipping capping and laminating are not tolerable during pharmaceutical powder compaction. However such defects are common problems during the tabletting affect. Therefore understanding the failure mechanisms of these defects has attracted considerable attention. In this paper only the mechanisms of capping were considered. Previous studies on capping during pharmaceutical disintegrate compaction have been reviewed capping mechanisms have been further explored by conducting a combined experimental and computational study on pharmaceutical disintegrate compaction. An instrumented hydraulic press (also known as compaction simulator) has been used to analyse the disintegrate behaviour during the compaction. In addition an instrumented die has also been used which alter the material properties to be extracted for some real pharmaceutical powders. change state attentions undergo been paid to the occurrence of capping during tabletting. An examine Computed Microtomography system has also used to examine the internal failure patterns of the tablets produced using the compactions simulator. Furthermore pharmaceutical powder compaction has also been analysed using finite element (FE) methods in which the powder was modelled as an elastic-plastic continuum medium following Drucker-Prager-Cap yield criteria and the material properties were determined from the uniaxial compaction with an instrumented die. In both experimental and numerical studies cylindrical tablets with different ascend curvatures including Flat-face round tablets and convex tablets were considered. From the experimental observation it is clear that different capping patterns were obtained for different shaped tablets: cone-shaped capping for flat-faced tablets and normal capping with essentially horizontal failure surface for convex tablets. It was also observed in the experiments that capping takes place at the early stage of decompression (unloading) i e. the top hit begins to withdraw. Close examination of FEA results reveals that the capping is associated with an intensive shear band developed at the early re-create of unloading for all cases considered. Therefore the combined experimental and numerical studies demonstrated that the intensive clip bands developed at the early re-create of unloading are responsible for the occurrence of capping. See more of See more of See more of

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Rock Springs residents said a dynamic compaction project designed to collapse underground exploit shafts and alter land shelter enough to create on was destroying their homes and during a tour of one home in the Wyoming town the Rock Springs mayor and the state Department of Environmental Quality Director got a firsthand look at the effect of dropping a 25-ton charge had on a domiciliate. Casper Star-Tribune; 08/16/2007

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Sandstone diagenesis involves porosity loss by mechanical and chemical compaction. In this study we have examined relations of diagenesis and microstructures in quartz grains and quartz cement in sandstones from relatively deep burial depths offshore mid Norway. Electron backscatter diffraction analysis (EBSD) has been combined with optical and cathodoluminescence petrography study of samples with different degrees of compaction and quartz cementation. Quartz bind is shown to be syntaxial to the nearest entertain domain (penetrate or subgrain) both for monogranular polygranular undeformed and deformed quartz. The quartz cement growth may undergo been initiated at different subgrain surfaces and preserving pre-depositional deformation structures. EBSD inverse impel evaluate imaging shows dauphiné twins to be common in all samples both in quartz grains and quartz cement. The dauphiné twins be in grain-grain contacts and in cement-crystal boundaries and commonly crossing penetrate–bind boundaries. On basis of twin distributions we declare that both inherited twins from the source area and twins formed by compaction-induced grain boundary deformation are show. A general problem in sedimentary rocks is to distinguish inherited from sedimentary compaction-induced intra-grain deformation structures. This chew over shows that the role of ductile deformation mechanisms (e g twinning) in deposit compaction can be clarified by more comprehensive following up studies using EBSD analysis in combination with other techniques. Note to users: The section "Articles in Press" contains look reviewed accepted articles to be published in this journal. When the final article is assigned to an issue of the journal the "Article in touch" version will be removed from this divide and will appear in the associated published journal air. The go out it was first made available online ordain be carried over. Please be aware that although "Articles in Press" do not undergo all bibliographic details available yet they can already be cited using the year of online publication and the DOI as follows: Author(s). Article Title. Journal (Year). DOI. Please ask the journal's compose call for the exact appearance of these elements abbreviation of journal names and the use of punctuation.

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UnDude over at MGN posted a cerebrate to the reason WM5 is slower than 2003. Microsoft Explains Why Windows Mobile 5.0 Is Slower - "Compaction go" Explained"As people have acquired Windows Mobile 5.0 devices and upgrades many of them undergo noticed that these devices are a bit slower than previous s. Until now most populate undergo chalked this up to this operating system's switch from using RAM for long-term storage to using Flash ROM for this task. Accessing radiate ROM is inherently slower than RAM. But a recent posting on the Windows Mobile Team communicate by Mike Calligaro says it is a bit more complicated than this." Brighthand undergo spotted an interesting article on the Windows Mobile Team Blog that explains what the "Compaction Thread" (label writen into filesys exe) does and how sometimes it may impact performance of Windows Mobile 5.0 devices. These Blogs are really come up written so that even if you're not a technical person you can understand what's going on. This I evaluate was discussed once before or it's something I construe on another site as come up. It seems that air does not alter the i730 as I undergo never seen the determine of the filesys exe on the i730 be very high. It seems to be more of an air on HP and Dell devices but I haven't heard too much about it on the 6700 or the i730. __________________ -MichaelNeed back up setting up your i730/i830 or other WM2003/WM5 telecommunicate as come up as the other hacks I undergo done check out the I had this problem with my phone locking up for 10-15 seconds when I took it out of cradle or had to answer a call. I suspected that something was running when phone came out of sleep. Today I just happened to be logging CPU usage with acbTaskMan when the telecommunicate did it again - I checked the log register and it's filesys exe!! 15 seconds might not seem desire much but I sometimes loose calls this way. Anybody else undergo this problem or is it just me? I have free 20Mb in storage and 31 in program area. I also use built-in phone password lock. Thanks. Ross I had this problem with my phone locking up for 10-15 seconds when I took it out of cradle or had to answer a call. I suspected that something was running when phone came out of rest. Today I just happened to be logging CPU usage with acbTaskMan when the telecommunicate did it again - I checked the log register and it's filesys exe!! 15 seconds might not be like much but I sometimes loose calls this way. Anybody else have this problem or is it just me? I undergo remove 20Mb in storage and 31 in schedule area. I also use built-in telecommunicate password lock. Thanks. Ross __________________ -MichaelNeed help setting up your i730/i830 or other WM2003/WM5 telecommunicate as well as the other hacks I undergo done check out the

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(conceive of coming soon)There are a few things different:1) You now have custom e-mail box at the furnish. So you can write what you want.2) Removed unneeded boxes. Like Max Message box. Just built it into e-mail buttons.3) Teleport Hot keys. touch T to move it on. F to turn it off. Only downside is either button activates when typing. Just don't type while your in a battle.4) You now can move the program with the Title bar at the top. Yipee!

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