Key TakeawaysKey PointsLong bones are those that are longer than they are wide.The end of the long bone is the epiphysis and the shaft is the diaphysis. When a human finishes growing these parts fuse together.The outside of the flat bone consists of a layer of connective tissue called the periosteum.The interior part of the long bone is the medullary cavity with the inner core of the bone cavity being composed of marrow.Flat bones have broad surfaces for protection or muscular attachment.Flat bones are composed of two thin layers of compact bone that surround a layer of cancellous (spongy) bone. In an adult, most red blood cells are formed in the marrow in flat bones.Key Termsendosteum: A thin vascular membrane of connective tissue that lines the surface of the bone tissue that forms the medullary cavity of long bones.
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medullary cavity: The medullary cavity, also known as the marrow cavity, is the central cavity of bone shafts where red bone marrow and/or yellow bone marrow (adipose tissue) is stored.diaphysis: The central shaft of any long bone.epiphyseal plate: A hyaline cartilage plate in the metaphysis, located at each end of a long bone where growth occurs in children and adolescents.
Bones support and protect the body and its organs. They also produce various blood cells, store minerals, and provide support for mobility in conjunction with muscle. Bone is made of bone tissue, a type of dense connective tissue.
Bone (osseous) tissue is the structural and supportive connective tissue of the body that forms the rigid part of the bones that make up the skeleton. Overall, the bones of the body are an organ made up of bone tissue, bone marrow, blood vessels, epithelium, and nerves.
There are two types of bone tissue: cortical and cancellous bone. Cortical bone is compact bone, while cancellous bone is trabecular and spongy bone.
Cortical bone forms the extremely hard exterior while cancellous bone fills the interior. The tissues are biologically identical but differ in the arrangement of their microstructure.
The following are the different types of bone cells:Osteoblasts-involved in the creation and mineralisation of boneOsteocytes and osteoclasts: These are involved in the reabsorption of bone tissue. The mineralized matrix of bone tissue has an organic component—mainly made of collagen—and an inorganic component of bone mineral made up of various salts.
There are different types of bone. These are:Long bonesShort bonesFlat bonesSesamoid bonesIrregular bones
Long bone: A long bone is longer than it is wide. Growth occurs by a lengthening of the diaphysis. located in the center of the long bone.
Long bones grow primarily by elongation of the diaphysis (the central shaft), with an epiphysis at each end of the growing bone. The ends of epiphyses are covered with hyaline cartilage (articular cartilage). At the cessation of growth, the epiphyses fuse to the diaphysis, thus obliterating the intermediate area known as the epiphyseal plate or growth plate. The long bones in the body are as follows:Legs: The femur, tibia, and fibula.Arms: The humerus, radius, and ulna.The clavicles or collar bones.Metacarpals, metarsals, phalanges.
The outside of the bone consists of a layer of connective tissue called the periosteum. The outer shell of the long bone is compact bone, below which lies a deeper layer of cancellous bone (spongy bone), as shown in the following figure. The interior part of the long bone is called the medullary cavity; the inner core of the bone cavity is composed of marrow.
Short bones are about as wide as they are long. These provide support with less movement. Examples of short bones include the carpal and tarsal bones of the wrist and feet. They consist of a thin layer of cortical bone with cancellous interiorly.
Compact bone and spongy bone: The hard outer layer of bones is composed of compact bone tissue, so-called due to its minimal gaps and spaces. Its porosity is 5–30%. Inside the interior of the bone is the trabecular bone tissue, an open cell, porous network that is also called cancellous or spongy bone.
Flat bones are broad bones that provide protection or muscle attachment. They are composed of two thin layers of compact bone surrounding a layer of cancellous (spongy) bone.
These bones are expanded into broad, flat plates, as in the cranium (skull), ilium (pelvis), sternum, rib cage, sacrum, and scapula. The flat bones are named:OccipitalParietalFrontalNasalLacrimalVomerScapulaOs coxæ (hip bone)SternumRibs
Sesamoid bones are smaller bones that are fixed in tendons to protect them. An example is the patella (knee cap) located in the patellar tendon. Other examples include the small bones of the metatarsals and the pisiform bones of the carpus.
The irregular bones are named for their nonuniform shape. Examples include the bones of the vertebrae. These typically have a thin cortical layer with more cancellous bone in their tissue.
Supply of Blood and Nerves to Bone
The blood and nerve supply to bones are carried in Haversian canals that run along the long axis of bones.
Describe the blood and nerve supply of bones
Key TakeawaysKey PointsHaversian canals typically run parallel to the surface and along the long axis of the bone and generally contain one or two capillaries and nerve fibers.Volkmann’s canals are channels that assist with blood and nerve supply from the periosteum to the Haversian canal.The vascular supply of long bones depends on several points of inflow.Except for a few with double or no foramina (places in bone where capillaries enervate), 90% of long bones have a single nutrient foramen in the middle third of the shaft.Young periosteum is more vascular and its vessels communicate more freely with those of the shaft compared to adult periosteum.Key Termsperichondrium: A layer of dense irregular connective tissue that surrounds the cartilage of developing bone.Volkmann’s canal: Also known as perforating holes, these are microscopic structures found in the compact bone that carry small arteries throughout the bone.anastomose: Joined or run together.Haversian canal: A hollow channel in the center of an osteon, running parallel to the length of a bone.
Blood is supplied to mature compact bone through the Haversian canal. Haversian canals are formed when individual lamellae form concentric rings around larger longitudinal canals (approx. 50 µm in diameter) within the bone tissue.
Haversian canals typically run parallel to the surface and along the long axis of the bone. The canals and the surrounding lamellae (8–15) are called a Haversian system or an osteon. A Haversian canal generally contains one or two capillaries and nerve fibers.
The Haversian canals also surround nerve cells throughout the bone and communicate with osteocytes in lacunae (spaces within the dense bone matrix that contain the living bone cells) through canaliculi. This unique arrangement is conducive to the storage of mineral salt deposits that give bone tissue its strength.
Haversian canal: The Haversian canals surround blood vessels and nerve cells throughout the bone.
The vascular supply of long bones depends on several points of inflow, which feed complex sinusoidal networks within the bone. These in turn drain to various channels through all surfaces of the bone except that covered by articular cartilage.
Volkmann’s canals are channels that assist with blood and nerve supply from the periosteum to the Haversian canal. One or two main diaphyseal nutrient arteries enter the shaft obliquely through one or two nutrient foramina leading to nutrient canals. Their sites of entry and angulation are almost constant and characteristically directed away from the growing epiphysis.
Except for a few with double or no foramina, 90% of long bones have a single nutrient foramen in the middle third of the shaft. The nutrient arteries divide into ascending and descending branches in the medullary cavity. These approach the epiphysis dividing into smaller rami. Near the epiphysis, they anastomose with the metaphyseal and epiphyseal arteries.
The blood supply of the immature bones is similar, but the epiphysis is a discrete vascular zone separated from the metaphysis by the growth plate. Epiphyseal and metaphyseal arteries enter on both sides of the growth cartilage, with anastamoses between them being few or absent.
Growth cartilage receives its blood supply from both sources and also from an anastamotic collar in the adjoining perichondrium. Young periosteum is more vascular, has more metaphyseal branches, and its vessels communicate more freely with those of the shaft than adult periosteum.
Microscopic Anatomy of Bone
The basic microscopic unit of bone is an osteon, which can be arranged into woven bone or lamellar bone.
Classify woven bone and lamellar bone
Key TakeawaysKey PointsWoven bone is found on the growing ends of an immature skeleton or, in adults, at the site of a healing fracture.Woven bone is characterized by the irregular organization of collagen fibers and is mechanically weak, but forms quickly.Lamellar bone is much stronger than woven bone, and is highly organized in concentric sheets with a much lower proportion of osteocytes to mineralized tissue.When the same lamellar bone is loosely arranged, it is referred to as trabecular bone. Trabecular bone gets its name because of the spongy pattern it displays on an x-ray.After a fracture, woven bone forms initially and is gradually replaced by lamellar bone during a process known as bony substitution.Key Termsosteoblast: A mononucleate cell from which bone develops.osteocytes: A star-shaped type of bone cell that is found in the cells of mature bone.lamellar bone: A bone with a regular, parallel alignment of collagen into sheets (lamellae) that is mechanically strong.woven bone: Characterized by an irregular organization of collagen fibers, this bone is mechanically weak.
Bones are composed of bone matrix, which has both organic and inorganic components. Bone matrix is laid down by osteoblasts as collagen, also known as osteoid. Osteoid is hardened with inorganic salts, such as calcium and phosphate, and by the chemicals released from the osteoblasts through a process known as mineralization.
The basic microscopic unit of bone is an osteon (or Haversian system). Osteons are roughly cylindrical structures that can measure several millimeters long and around 0.2 mm in diameter.
Each osteon consists of a lamellae of compact bone tissue that surround a central canal (Haversian canal). The Haversian canal contains the bone’s blood supplies. The boundary of an osteon is called the cement line. Osteons can be arranged into woven bone or lamellar bone.
Osteon: A photo taken through a microscope that shows the anatomy of compact bone with a detailed view of an osteon.
Woven bone is found on the growing ends of an immature skeleton or, in adults, at the site of a healing fracture. Woven bone is characterized by the irregular organization of collagen fibers and is mechanically weak, but forms quickly.
The criss-cross appearance of the fibrous matrix is why it is referred to as woven. It has a high proportion of osteocytes to hard inorganic salts that leads to its mechanical weakness.
Woven bone is replaced by lamellar bone during development. In contrast to woven bone, lamellar bone is highly organized in concentric sheets with a much lower proportion of osteocytes to surrounding tissue. The regular parallel alignment of collagen into sheets, or, lamellae, causes lamellar bone to be mechanically strong.
Lamellar bone makes up the compact or cortical bone in the skeleton, such as the long bones of the legs and arms. In a cross-section, the fibers of lamellar bone can be seen to run in opposite directions in alternating layers, much like in plywood, assisting in the bone’s ability to resist torsion forces.
When the same lamellar bone is loosely arranged, it is referred to as trabecular bone. Trabecular bone gets its name because of the spongy pattern it displays in an x-ray. The spaces within trabecular bone are filled with active bone marrow.
After a fracture, woven bone forms initially, but it is gradually replaced by lamellar bone during a process known as bony substitution.
Chemical Composition of Bone
Acid-base imbalances, including metabolic acidosis and alkalosis, can produce severe, even life-threatening medical conditions.
Differentiate among the acid-base disorders
Key TakeawaysKey PointsMetabolic acidosis can produce, among other symptoms, chest pains, altered mental states, nausea, abdominal pain, and muscle weakness.Rapid, deep breathing during metabolic acidosis is an attempt to lower carbon dioxide levels and return pH to normal.Extreme acidemia can lead to coma, seizures, heart arrhythmias, and low blood pressure.Slowed breathing, which results in retaining more CO2, is the primary method of reducing metabolic alkalosis.Chronic respiratory acidosis is a result of COPD, obesity hypoventilation syndrome, ALS, and thoracic deformities.Respiratory alkalosis can be caused by excessive mechanical ventilation, psychiatric problems, stroke, drug use, traveling to high altitude regions, lung disease, fever, and pregnancy, among other factors.Key Termsmetabolic alkalosis: A metabolic condition in which the pH of tissue is elevated beyond the normal range ( 7.35 to 7.45 ). This is the result of decreased hydrogen ion concentration, leading to increased bicarbonate concentration, or a direct result of increased bicarbonate concentration.respiratory acidosis: A medical condition in which decreased ventilation (hypoventilation) causes increased blood carbon dioxide concentration and decreased pH (a condition generally called acidosis).metabolic acidosis: A condition that occurs when the body produces too much acid or when the kidneys are not removing enough acid from the body.
Traveling to a high altitude can cause an acid-base imbalance due to reduced levels of oxygen in the atmosphere, and, therefore, in the blood. To compensate for this, the traveler begins to hyperventilate, trying to expel excess carbon dioxide and bring pH back to normal. However, if the traveler stays at high altitude, it may take several days for their pH to fully return to normal.
Acid-base imbalance is an abnormality of the human body’s normal balance of acids and bases that causes the plasma pH to deviate out of normal range (7.35 to 7.45). In the fetus, the normal range differs based on which umbilical vessel is sampled (umbilical vein pH is normally 7.25 to 7.45; umbilical artery pH is normally 7.18 to 7.38). Acid-base imbalances can exist in varying levels of severity, some life-threatening.
An excess of acid is called acidosis and an excess in bases is called alkalosis. The process that causes the imbalance is classified based on the etiology of the disturbance (respiratory or metabolic) and the direction of change in pH (acidosis or alkalosis).
Mixed disorders may feature an acidosis and alkalosis excess at the same time that partially counteract each other, or there can be two different conditions affecting the pH in the same direction. The phrase mixed acidosis, for example, refers to metabolic acidosis in conjunction with respiratory acidosis.
In medicine, metabolic acidosis is a condition that occurs when the body produces too much acid or when the kidneys are not removing enough acid from the body. If unchecked, metabolic acidosis leads to acidemia, that is, blood pH is less than 7.35 due to increased production of hydrogen by the body, or because of the body’s inability to form bicarbonate (HCO3-) in the kidneys.
Acidosis refers to a low pH in tissue. Acidemia refers to a low pH in the blood. Symptoms may include chest pain, palpitations, headache, altered mental status such as severe anxiety due to hypoxia, decreased visual acuity, nausea, vomiting, abdominal pain, altered appetite (either loss of or increased) and weight loss (longer term), muscle weakness, and bone pains.
Rapid deep breaths increase the amount of carbon dioxide exhaled, thus lowering the serum carbon dioxide levels, resulting in some degree of compensation. Overcompensation via respiratory alkalosis to form an alkalemia does not occur.
Neurological complications include lethargy, stupor, coma, seizures. Cardiac complications include arrhythmias (ventricular tachycardia) and decreased response to epinephrine; both lead to hypotension (low blood pressure).
Metabolic alkalosis is a metabolic condition in which the pH of tissue is elevated beyond the normal range (7.35 to 7.45). This is the result of decreased hydrogen ion concentration, leading to increased bicarbonate concentration, or as a direct result of increased bicarbonate concentrations. Alkalosis refers to a high pH in tissue.
Alkalemia refers to a high pH in the blood. The causes of metabolic alkalosis can be divided into two categories, depending upon urine chloride levels. Chloride-responsive causes result from the loss of hydrogen ions via vomiting or the kidneys. Vomiting results in the loss of hydrochloric acid (hydrogen and chloride ions) with the stomach contents.
The kidneys compensate for these losses by retaining sodium in the collecting ducts at the expense of hydrogen ions (sparing sodium/potassium pumps to prevent further loss of potassium), and leads to metabolic alkalosis. The excess sodium increases extracellular volume and the loss of hydrogen ions creates a metabolic alkalosis.
Later, the kidneys respond through the aldosterone escape to excrete sodium and chloride in urine. Compensation for metabolic alkalosis occurs mainly in the lungs, which retain carbon dioxide (CO2) through slower breathing, or hypoventilation (respiratory compensation).
CO2 is then consumed towards the formation of the carbonic acid intermediate, thus decreasing pH. Renal compensation for metabolic alkalosis, less effective than respiratory compensation, consists of increased excretion of HCO3– (bicarbonate), as the filtered load of HCO3– exceeds the ability of the renal tubule to reabsorb it.
Respiratory acidosis is a medical condition in which decreased ventilation (hypoventilation) causes an increase in blood carbon dioxide concentration and decreased pH (a condition generally called acidosis). Carbon dioxide is produced constantly as the body’s cells respire, and this CO2 will accumulate rapidly if the lungs do not adequately expel it through alveolar ventilation.
Acute respiratory acidosis occurs when an abrupt failure of ventilation occurs. This failure in ventilation may be caused by depression of the central respiratory center by cerebral disease or drugs, an inability to ventilate adequately due to neuromuscular disease (e.g., myasthenia gravis, amyotrophic lateral sclerosis, Guillain-Barré syndrome, muscular dystrophy), or airway obstructions related to asthma or chronic obstructive pulmonary disease (COPD) exacerbation.
Respiratory alkalosis is a medical condition in which increased respiration (hyperventilation) elevates the blood pH (a condition generally called alkalosis). There are two types of respiratory alkalosis: chronic and acute.
Acute respiratory alkalosis occurs rapidly. During acute respiratory alkalosis, the person may lose consciousness whereupon the rate of ventilation will resume to normal.
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Chronic respiratory alkalosis is a more long-standing condition. Respiratory alkalosis may be produced accidentally (iatrogenically) during excessive mechanical ventilation. Other causes include: psychiatric causes, drug use, fever, and pregnancy.