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172<br />

ABDOMINAL ULTRASOUND<br />

Ultrasound appearances<br />

Most renal calculi are calcified foci located in the<br />

collecting system of the kidney. Careful scanning<br />

with modern equipment can identify over 90% of<br />

these. 16 Most stones are highly reflective structures<br />

which display distal shadowing (Fig. 7.16). The<br />

shadowing may, however, be difficult to demonstrate<br />

due to the proximity of hyperechoic sinus<br />

echoes distal to the stone, or due to the relatively<br />

small size of the stone compared to the beam<br />

width.<br />

The identification of reflective foci in the kidney<br />

is complicated by the fact that the normal renal<br />

sinus echoes are of similar echogenicity. This<br />

means that small stones may be missed on ultrasound.<br />

Differentiation of stones from sinus fat and<br />

reflective vessel walls is dependent upon careful<br />

technique and optimal use of the equipment. The<br />

operator must adjust the technique to display the<br />

distal shadow by using a variety of scanning angles<br />

and approaches and by ensuring that the suspected<br />

stone lies within the (narrowest) focal zone of the<br />

beam. The higher the frequency used, the better<br />

the chances of identifying the stone.<br />

Clearly the identification of large calculi is normally<br />

straightforward; however, for many of the<br />

reasons above, identification of small calculi can be<br />

difficult, especially in a patient with pain. Both<br />

false-positive and false-negative studies are well<br />

recognized. Although traditionally the plain film,<br />

that is kidneys, ureters, bladder (KUB), is often the<br />

first-line investigation for patients with suspected<br />

calculi, it is now being accepted that CT IVU is the<br />

best and most reliable diagnostic test for calculi<br />

detection (Fig. 7.16 C and D).<br />

RT KIDNEY<br />

A<br />

B<br />

C<br />

Figure 7.16 (A) A calculus within the PCS of the RK. Distal acoustic shadowing is easily seen. (B) A staghorn calculus<br />

fills the entire PCS of the kidney. A sagittal section through the lateral aspect of the kidney gives the impression of<br />

several separate stones, although this is, in fact, a single calculus. (C) CT IVU through the renal area. The right renal<br />

pelvis is mildly dilated (arrow) and a small amount of perirenal stranding is noted, suggestive of obstruction<br />

(arrowheads). (D) CT scan through the bladder showing a small calculus on the right (arrow) at the right vesicoureteric<br />

junction.<br />

D

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