Background: Osteoporosis is a frequent disease that is manifested by reduced in mineral density and raised in fracture risk. Recent studies have indicated that osteoporosis is caused by composite connections among local and systemic regulators of bone cell function.
Objective: The purpose of this study was to investigate the relationship between interleukin-2, interleukin-4, and some biochemical markers in Iraqi patients with osteoporosis.
Patients and Methods: Forty five osteoporotic patients were incorporated in this study (30 women and 15 men). Serum fasting glucose, lipid profile, alkaline phosphatase activity, calcium, magnesium, interleukin-2, and interleukin-4 were measured in osteoporotic patients and compared them with the control group.
Results: There was a significant increase in serum fasting glucose, lipid profile except high density lipoprotein cholesterol, and serum alkaline phosphatase activity in osteoporotic patients as compared to the control, (P=0.001). Also, there was a significant increase in interleukin-2 and interleukin-4 in osteoporotic patients as compared to the control, (P= 0.01). While there was a decrease in serum calcium and magnesium levels in osteoporotic patients as compared to the control. Also, there was a significant positive correlation between serum alkaline phosphatase activity with interleukin-2 and interleukin-4 levels in osteoporotic patients, (P= 0.01).
Conclusion: Elevated levels of interleukin-2 and interleukin-4 along with some biochemical markers like; serum alkaline phosphatase in osteoporotic patients might include significant functions in the pathogenesis of osteoporosis.
The study area intendes for agricultural investment and establishment stations of water pumping for human use to the nearby areas, southwest of Samawah city. Twelve Two-Dimension (2-D) survey points were performed by using Wenner-Schlumberger array configuration to take the measurements. The inverse models of two survey point appear the effect of the saline groundwater that raises from Rus Formation, which caused a significant reduction in resistivity of the groundwater-bearing zone within middle Dammam Formation along the fault plane.
In this paper, we introduce a new type of functions in bitopological spaces, namely, (1,2)*-proper functions. Also, we study the basic properties and characterizations of these functions . One of the most important of equivalent definitions to the (1,2)*-proper functions is given by using (1,2)*-cluster points of filters . Moreover we define and study (1,2)*-perfect functions and (1,2)*-compact functions in bitopological spaces and we study the relation between (1,2)*-proper functions and each of (1,2)*-closed functions , (1,2)*-perfect functions and (1,2)*-compact functions and we give an example when the converse may not be true .