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2.1.1 Soil compositionWhen dry soil is crushed in the hand, it can be seen that it is composed of all kinds of particles of different sizes.Most of these particles originate from the degradation of rocks; they are called mineral particles. Some originate from residues of plants or animals (rotting leaves, pieces of bone, etc.), these are called organic particles (or organic matter). The soil particles seem to touch each other, but in reality have spaces in between. These spaces are called pores. When the soil is "dry", the pores are mainly filled with air. After irrigation or rainfall, the pores are mainly filled with water. Living material is found in the soil. It can be live roots as well as beetles, worms, larvae etc. They help to aerate the soil and thus create favourable growing conditions for the plant roots (Fig. 26).Fig. 26. The composition of the soil2.1.2 Soil profileIf a pit is dug in the soil, at least 1 m deep, various layers, different in colour and composition can be seen. These layers are called horizons. This succession of horizons is called the profile of the soil (Fig. 27).Fig. 27. The soil profileA very general and simplified soil profile can be described as follows:a. The plough layer (20 to 30 cm thick): is rich in organic matter and contains many live roots. This layer is subject to land preparation (e.g. ploughing, harrowing etc.) and often has a dark colour (brown to black).b. The deep plough layer: contains much less organic matter and live roots. This layer is hardly affected by normal land preparation activities. The colour is lighter, often grey, and sometimes mottled with yellowish or reddish spots.c. The subsoil layer: hardly any organic matter or live roots are to be found. This layer is not very important for plant growth as only a few roots will reach it.d. The parent rock layer: consists of rock, from the degradation of which the soil was formed. This rock is sometimes called parent material.The depth of the different layers varies widely: some layers may be missing altogether.2.1.3 Soil textureThe mineral particles of the soil differ widely in size and can be classified as follows:Name of the particlesSize limits in mmDistinguisable with naked eyegravellarger than 1obviouslysand1 to 0.5easilysilt0.5 to 0.002barelyclayless than 0.002impossibleThe amount of sand, silt and clay present in the soil determines the soil texture.In coarse textured soils: sand is predominant (sandy soils).In medium textured soils: silt is predominant (loamy soils).In fine textured soils: clay is predominant (clayey soils).In the field, soil texture can be determined by rubbing the soil between the fingers (see Fig. 28).Farmers often talk of light soil and heavy soil. A coarse-textured soil is light because it is easy to work, while a fine-textured soil is heavy because it is hard to work.Expression used by the farmerExpression used in literaturelightsandycoarsemediumloamymediumheavyclayeyfineThe texture of a soil is permanent, the farmer is unable to modify or change it.Fig. 28a. Coarse textured soil is gritty. Individual particules are loose and fall apart in the hand, even when moist.Fig. 28b. Medium textured soil feels very soft (like flour) when dry. It can be easily be pressed when wet and then feels silky.Fig. 28c. Fine textured soil sticks to the fingers when wet and can form a ball when pressed.2.1.4 Soil structureSoil structure refers to the grouping of soil particles (sand, silt, clay, organic matter and fertilizers) into porous compounds. These are called aggregates. Soil structure also refers to the arrangement of these aggregates separated by pores and cracks (Fig. 29).The basic types of aggregate arrangements are shown in Fig. 30, granular, blocky, prismatic, and massive structure.Fig. 29. The soil structureWhen present in the topsoil, a massive structure blocks the entrance of water; seed germination is difficult due to poor aeration. On the other hand, if the topsoil is granular, the water enters easily and the seed germination is better.In a prismatic structure, movement of the water in the soil is predominantly vertical and therefore the supply of water to the plant roots is usually poor.Unlike texture, soil structure is not permanent. By means of cultivation practices (ploughing, ridging, etc.), the farmer tries to obtain a granular topsoil structure for his fields.Fig. 30. Some examples of soil structures GRANULAR BLOCKY PRISMATIC MASSIVE 2.2 Entry of water into the soil 2.2.1 The infiltration process 2.2.2 Infiltration rate 2.2.3 Factors influencing the infiltration rate
To keep drag low, wingspan must be limited, which also reduces the aerodynamic efficiency when flying slowly. Since a supersonic aircraft must take off and land at a relatively slow speed, its aerodynamic design must be a compromise between the requirements for both ends of the speed range.
The key to having low supersonic drag is to properly shape the overall aircraft to be long and thin, and close to a "perfect" shape, the von Karman ogive or Sears-Haack body. This has led to almost every supersonic cruising aircraft looking very similar to every other, with a very long and slender fuselage and large delta wings, cf. SR-71, Concorde, etc. Although not ideal for passenger aircraft, this shaping is quite adaptable for bomber use.
A sonic boom is the sound associated with the shock waves created whenever an object traveling through the air travels faster than the speed of sound. Sonic booms generate significant amounts of sound energy, sounding similar to an explosion or a thunderclap to the human ear. The crack of a supersonic bullet passing overhead or the crack of a bullwhip are examples of a sonic boom in miniature.
A key feature of these designs is the ability to maintain supersonic cruise for long periods, so low drag is essential to limit fuel consumption to a practical and economic level. As a consequence, these airframes are highly streamlined and the wings have a very short span. The requirement for low speeds when taking off and landing is met by using vortex lift: as the aircraft slows, lift must be restored by raising the nose to increase the angle of attack of the wing. The sharply swept leading edge causes the air to twist as it flows over the wing, speeding up the airflow locally and maintaining lift.
The very short version is whatever the cause of you needing a crown, a crack, decay, or break, causes some trauma to the nerve and the dentist fixing the problem causes more. The combination of the two things cause inflammation in the nerve which you experience as pain.
Removing decay, old filling material, cracks and just preparing the tooth for a crown happens all at once and is traumatic. This in addition to whatever was the cause for you to need a crown can push a tooth that felt fine over the edge and cause the tooth to hurt after the dental crown.
If this is the case you will lose the tooth. These cracks are hard to detect and unfortunately often receive expensive dental work before we can determine they have the crack. The tooth in my cracked tooth syndrome post was a tooth that a root canal was done on knowing that a significant crack was there. However, we can not always know this, in fact usually we do not.
Went to dentist for cracked tooth a few weeks ago. Had crown put on last week. He had to use alot of Novocain because of extreme sensitivity when putting new crown on. 6 days later the new crown came off! Immediately went back to dentist. (Yesterday). He did the Novocain again (just putting the topical on before the Novocain was painful) and put the crown back on. Everything was fine until the evening. Then I thought I was going to jump out of my skin the pain was so intense. What do I do now? I will call dentist and what should I expect him to do?
New dentist and new endo now treating me, seems much more carefully. Dentist fit me for a tooth guard, put sedative filling in 3 which also reduced it so teeth in that row are more even in height, warned may need crown as corner is now thin. Endo did 3-d scan and focuses on possible tissue after root canal in 2. Says perio and occlusion are OK. But symptom of pressure and bite pain began from the beginning when preparing tooth for crown, not after RC. Endo put me on antibiotics as first step to review in 2 weeks. Possible RC rework and if that fails, possible extraction of tooth 2. Tooth 3 may end up with root canal if ache continues after sedative filling. Did I mention tooth 31 below 2 is cracked. Not noticed until reduced for crown in 2. 31 will be reviewed later, but it did develop bite pain (I tried chewing on that side after install of final crown. I am back to only chewing on other side).
Sounds like heading to a root canal. Grinders often break or crack teeth. By the time they get sensitive putting a crown on it is not always successful. You need a crown so it is always the first step as it is more conservative.
At the beginning, the tooth had been sharply rocked when dental assistant tried removing temp crown (dentist cut it off). I heard crunching and felt pain. 3D x-ray shows nothing specific and I understand it would not show hairline crack. 3 months later, chewing is now more a discomfort than sharp pain with only firmer food chewed on other side.
Doctor, I need one more advice. Second opinion confirmed that I have a crack in my tooth because it hurts when I bite at appropriate angle. X-ray did not show any inflamed roots. During second opinion endodontist asked to bite plastic thing to determine where pain is coming from. The next day I felt this tooth on and off.