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The Esophagus


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of a portion of the bolus because of weakening of the amplitude of primary peristalsis at the transition zone between the striated and smooth muscle portions of the esophagus, a clinically trivial phenomenon known as proximal escape [136].

      Varices

Photo depicts diffuse esophageal spasm. (A) Prone single-contrast view shows multiple lumen-obliterating, nonperistaltic contractions that compartmentalize the esophagus, producing the classic corkscrew appearance associated with diffuse esophageal spasm. (B) Prone single-contrast view in another patient shows multiple nonperistaltic contractions of mild-to-moderate severity (white arrows) with tapered, beak-like narrowing of the distal esophagus (black arrow) secondary to lower esophageal sphincter dysfunction.

       Uphill varices

      Esophageal varices are characterized on CT by a thickened, lobulated esophageal wall containing tubular structures that enhance markedly after intravenous administration of contrast material [139]. Additional varices may be seen elsewhere in the abdomen at other sites of communication between the portal and systemic venous circulations. Angiography of the celiac or superior mesenteric arteries can be used to confirm the presence of varices in and around the distal esophagus. However, the need for portal venography for presurgical planning of portosystemic shunts has decreased with the widespread use of transjugular intrahepatic portosystemic shunting procedures.

Photo depicts esophageal varices. Single-contrast view shows multiple large serpiginous defects in the lower third of the esophagus in a patient with portal hypertension and uphill esophageal varices.

       Downhill varices

      One of the most common causes of downhill varices is bronchogenic carcinoma with mediastinal metastases and superior vena cava obstruction [139]. Additional causes include other primary or metastatic tumors involving the mediastinum, mediastinal irradiation, sclerosing mediastinitis, substernal goiter, and central catheter‐related thrombosis of the superior vena cava. Most patients with downhill varices present clinically with the superior vena cava syndrome.

      Downhill varices typically appear as serpiginous longitudinal filling defects, which, unlike uphill esophageal varices, are confined to the upper or mid esophagus [139]. Venography may be performed to confirm the presence of superior vena cava obstruction, and chest radiographs or CT may be performed to determine the underlying cause.

      Foreign body impactions

Photos depict esophageal food impaction. (A) On the initial barium study, an impacted bolus of meat in the distal esophagus appears as a polypoid defect (arrows) with complete obstruction at this level. (B) A repeat study 10 days after endoscopic removal of the bolus reveals a lower esophageal ring (arrow) as the cause of the impaction.

      In the past, barium studies were often performed on patients with suspected esophageal food impaction, and if an impaction was present, the fluoroscopist sometimes attempted to relieve the impaction by administration of an oral effervescent agent, intravenous glucagon, or both. Because endoscopy is a more effective technique for relieving esophageal food impactions, and because residual barium above an impaction can impede endoscopic visualization or retrieval of the impacted food bolus, endoscopy has become the diagnostic and therapeutic test of choice for these patients [141].

      Fistulae