The adult human body’s skeleton comprises 206 bones. They support our frame and our structure. We need them to stand up and walk. We need them to move about.
Sometimes, after a long, tiring day, we may collapse like a sack of potatoes on our couch and feel like we don’t have any bones left… But they’re always there.
These bones are essential for our daily activities, but yet we don’t give that much thought to them because they’re hidden from plain sight — underneath multiple layers of skin cells and muscles.
But yet, things can happen to them as we age. We can be involved in accidents where we fracture our bones. We can’t see it, but we can sure feel it. The pain, the cast, the inability to do certain things… It sure feels annoying!
The more insidious killer is osteoporosis. The bone structure remains intact externally, but internally, the support structure is being eroded. The density of the bone cells inside the bone is gradually being reduced, and that results in a weaker, more porous (hence “porosis”) bone structure.
The weakening of this bone structure does not bode well for older people, especially if they fall and fracture major bones in their hip or pelvic region.
Because much of the arterial blood flow through to our legs goes through the hip and pelvic regions, hence a fracture in that area can disrupt blood circulation and spell trouble for blood transport down to our lower limbs.
But how does the bone structure become porous, you may ask?
There are 3 major types of bone cells: the osteoblasts, osteocytes and osteoclasts, which can be described as such:
OSTEOCLASTS are large cells that dissolve the bone. They come from the bone marrow and are related to white blood cells. They are formed from two or more cells that fuse together, so the osteoclasts usually have more than one nucleus. They are found on the surface of the bone mineral next to the dissolving bone.
OSTEOBLASTS are the cells that form new bone. They also come from the bone marrow and are related to structural cells. They have only one nucleus. Osteoblasts work in teams to build bone. They produce new bone called “osteoid” which is made of bone collagen and other protein. Then they control calcium and mineral deposition. They are found on the surface of the new bone.
When the team of osteoblasts has finished filling in a cavity, the cells become flat and look like pancakes. They line the surface of the bone. These old osteoblasts are also called LINING CELLS. They regulate passage of calcium into and out of the bone, and they respond to hormones by making special proteins that activate the osteoclasts.
OSTEOCYTES are cells inside the bone. They also come from osteoblasts. Some of the osteoblasts turn into osteocytes while the new bone is being formed, and the osteocytes then get surrounded by new bone. They are not isolated, however, because they send out long branches that connect to the other osteocytes. These cells can sense pressures or cracks in the bone and help to direct where osteoclasts will dissolve the bone.
Our bones are made up of living cells. We have osteoblasts that control calcium deposition in the bone, osteocytes that signal bone damage, and osteoclasts that eliminate damaged bone for osteoblasts to direct more calcium to the damaged areas to repair the damage.
The activity of these 3 cells are maintained at a healthy equilibrium for ensuring a healthy bone structure:
However, there are situations where this equilibrium can be disrupted, and one of the major contributing situations is this idea of mild chronic inflammation:
In mild chronic inflammation, the pro-inflammatory nuclear factor kappa B (NF-κB) transcription pathway is upregulated to signal the production of more inflammatory cytokines, such as tumour necrosis factor alpha (TNF-α) and interleukin 1β (IL-1β).
The problem, then, is the sequence of biochemical activities that follow:
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