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The leg venous system carries deoxygenated blood from the legs back to the heart. It consists of superficial, deep, and perforating veins.
The leg venous system carries deoxygenated blood from the legs back to the heart. It consists of superficial, deep, and perforating veins.
The leg venous system is the network of veins in the legs responsible for returning deoxygenated blood and metabolic waste products from the leg tissues back to the heart. Unlike the arterial system, which transports blood away from the heart, the venous system must work against gravity – especially when standing upright or walking.
The leg venous system is of great clinical importance, as it is commonly affected by conditions such as varicose veins, deep vein thrombosis (DVT), and chronic venous insufficiency (CVI).
The leg venous system is divided into three functional components:
The superficial venous system lies directly beneath the skin, above the muscular fascia. It includes two main trunks:
The deep venous system lies beneath the muscular fascia and carries the majority of venous blood (approximately 80–90%) back to the heart. Key veins include:
Perforating veins are short connecting vessels that link the superficial and deep venous systems. They penetrate (Latin: perforare) the muscular fascia and enable blood to transfer from the superficial to the deep system. Their valves ensure that blood flows in only one direction – from outside to inside and from below upward.
A key feature of the leg venous system is the venous valves (valvulae venosae). These pocket-shaped structures open when blood flows toward the heart and close when backflow is imminent. This prevents blood from flowing back down due to gravity.
When venous valves become incompetent or fail, venous reflux occurs – the pathological backflow of blood. This is a primary cause of varicose veins and chronic venous insufficiency.
Since blood in the leg veins must travel against gravity toward the heart, several mechanisms facilitate this process:
Varicose veins are permanently dilated, tortuous superficial veins. They develop due to incompetent venous valves and primarily affect the great saphenous vein and its branches. Symptoms include visibly protruding veins, heaviness, pain, and swelling in the legs.
Deep vein thrombosis occurs when a blood clot (thrombus) forms in the deep venous system, most commonly in the calf or thigh. It can be life-threatening if the clot detaches and causes a pulmonary embolism.
Chronic venous insufficiency describes a long-term impairment of venous return. It leads to congestion-related conditions such as edema, skin changes, and in advanced stages to venous leg ulcers (venous ulcus cruris).
Spider veins are fine, web-like visible capillaries just beneath the skin surface. They are generally harmless but can be a cosmetic concern and may indicate underlying venous disease.
The most important diagnostic method for assessing the leg venous system is duplex ultrasound (color-coded Doppler ultrasonography). It allows visualization of blood flow, valve function, and thromboses without radiation exposure. In specific cases, phlebography (X-ray with contrast agent) or MR angiography may also be used.
Treatment of leg vein disorders depends on the type and severity of the condition:
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