Difference between revisions of "Ultrasonography of kidney stone disease"

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==Evaluation==
 
==Evaluation==
[[File:Ultrasonography of renal stone located at the pyeloureteric junction.jpg|thumb|Figure 1. Renal stone located at the pyeloureteric junction with accompanying hydronephrosis.<ref name="Hansen2015" />]]
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With ultrasonography, larger stones (>5–7 mm) within the kidney, i.e., in the calyces, the pelvis and the pyeloureteric junction, can be differentiated, especially in the cases with accompanying hydronephrosis (Figure 1 and Figure 2). Hyperechoic stones are seen with accompanying posterior shadowing. Additional twinkling artifacts below the stone can often be seen using Doppler US. Large stones filling the entire collecting system are called coral stones or staghorn calculi and are easily visualized with US (Figure 3). Stones in the ureters are usually not visualized with US due to the air-filled intestines obscuring the insonation window. However, ureteral stones near the ostium can be visualized with a scan position over the bladder. An exam of the ureteric orifices and the excretion of urine to the bladder can be performed by inspecting the ureteric jets in the bladder with color Doppler US (Figure 4.).
With US, larger stones (>5–7 mm) within the kidney, i.e., in the calyces, the pelvis and the pyeloureteric junction, can be differentiated, especially in the cases with accompanying hydronephrosis (Figure 1 and Figure 2). Hyperechoic stones are seen with accompanying posterior shadowing. Additional twinkling artifacts below the stone can often be seen using Doppler US. Large stones filling the entire collecting system are called coral stones or staghorn calculi and are easily visualized with US (Figure 3). Stones in the ureters are usually not visualized with US due to the air-filled intestines obscuring the insonation window. However, ureteral stones near the ostium can be visualized with a scan position over the bladder. An exam of the ureteric orifices and the excretion of urine to the bladder can be performed by inspecting the ureteric jets in the bladder with color Doppler US (Figure 4.).
 
  
 
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File:Ultrasonography of renal stone located at the pyeloureteric junction.jpg|Figure 1. Renal stone located at the pyeloureteric junction with accompanying hydronephrosis.<ref name="Hansen2015" />
 
File:Ultrasonography of centrally-located stone with posterior shadowing.jpg|Figure 2. Centrally-located stone with posterior shadowing. No hydronephrosis is present. Measurement of kidney length on the US image is illustrated by ‘+’ and a dashed line.<ref name=Hansen2015/>
 
File:Ultrasonography of centrally-located stone with posterior shadowing.jpg|Figure 2. Centrally-located stone with posterior shadowing. No hydronephrosis is present. Measurement of kidney length on the US image is illustrated by ‘+’ and a dashed line.<ref name=Hansen2015/>
 
File:Ultrasonography of staghorn calculi filling the entire collecting system.jpg|Figure 3. Staghorn calculi filling the entire collecting system and creating pronounced shadowing.<ref name=Hansen2015/>
 
File:Ultrasonography of staghorn calculi filling the entire collecting system.jpg|Figure 3. Staghorn calculi filling the entire collecting system and creating pronounced shadowing.<ref name=Hansen2015/>

Revision as of 13:39, 8 November 2018

Authors: Mikael Häggström; Authors of Creative Commons article[1] [notes 1]

Planning

Need for imaging

Imaging is indicated in cases of flank pain and hematuria.[2]

Choice of modality

Algorithm for kidney stone disease, developed in the US.[3]
  • Ultrasonography of kidney stone disease is the first-line imaging modality for patients <14 years of age and those who are pregnant. It is also the first-line investigation for thin (BMI <30) patients and there is a strong suspicion of kidney stone disease.[2] In the algorithm at right, hydronephrosis may count as a diagnostic finding of urolithiasis.
  • CT of kidney stone disease is recommended for older patients, as well as those who have higher BMI and/or less specific findings.[2]

Evaluation

With ultrasonography, larger stones (>5–7 mm) within the kidney, i.e., in the calyces, the pelvis and the pyeloureteric junction, can be differentiated, especially in the cases with accompanying hydronephrosis (Figure 1 and Figure 2). Hyperechoic stones are seen with accompanying posterior shadowing. Additional twinkling artifacts below the stone can often be seen using Doppler US. Large stones filling the entire collecting system are called coral stones or staghorn calculi and are easily visualized with US (Figure 3). Stones in the ureters are usually not visualized with US due to the air-filled intestines obscuring the insonation window. However, ureteral stones near the ostium can be visualized with a scan position over the bladder. An exam of the ureteric orifices and the excretion of urine to the bladder can be performed by inspecting the ureteric jets in the bladder with color Doppler US (Figure 4.).

Report

  • Presence or absence of hydronephrosis.
  • Location and size of any stones. The absence of visible stones is not necessary to report, since the high risk of missing them may result in a false reassurance.

Notes

  1. For a full list of contributors, see article history. Creators of images are attributed at the image description pages, seen by clicking on the images. See Radlines:Authorship for details.

References

  1. 1.0 1.1 1.2 1.3 1.4 Content initially copied from: Hansen, Kristoffer; Nielsen, Michael; Ewertsen, Caroline (2015). "Ultrasonography of the Kidney: A Pictorial Review ". Diagnostics 6 (1): 2. doi:10.3390/diagnostics6010002. ISSN 2075-4418.  (CC-BY 4.0)
  2. 2.0 2.1 2.2 Brisbane, Wayne; Bailey, Michael R.; Sorensen, Mathew D. (2016). "An overview of kidney stone imaging techniques ". Nature Reviews Urology 13 (11): 654–662. doi:10.1038/nrurol.2016.154. ISSN 1759-4812. 
  3. Brisbane, Wayne; Bailey, Michael R.; Sorensen, Mathew D. (2016). "An overview of kidney stone imaging techniques ". Nature Reviews Urology 13 (11): 654–662. doi:10.1038/nrurol.2016.154. ISSN 1759-4812.