Assesment of Criteria in Differentiation of Ureteral Stones from Phleboliths with Thin-Slice Unenhanced Computed Tomography
1Özel Muğla Hastanesi, Radyoloji, MUĞLA, Türkiye
2Fırat Üniversitesi Tıp Fakültesi, Radyoloji, ELAZIĞ, Türkiye
3Başkent Üniversitesi Tıp Fakültesi, Radyoloji, ADANA, Türkiye
4Akdeniz Üniversitesi Tıp Fakültesi, Radyoloji, ANTALYA, Türkiye
Keywords: Computed tomography, ureteral stone, phlebolith, Bilgisayarlı tomografi, üreter taşı, flebolit
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Gereç ve Yöntemler: Altı aylık zaman periyodunda taşı olan 31 hastaya ve toplam 80 fleboliti olan 43 hastaya 3 cm uzunluğunda ince kesit (kesit kalınlığı: 2 mm, pitch: 1) olmak üzere kontrastsız helikal BT çekimi yapıldı. Her kalsifikasyonun boyut, şekil, santral lüsensi, yumuşak doku halka işareti, kuyruklu yıldız işareti, densite değerleri ve profil analizi kaydedildi.
Bulgular: Flebolitlerin 52'si (%65) yuvarlak, 28'i oval (%35) şekilliydi. Taşların ise 10'u (%32) yuvarlak, 8'i (%26) oval şekilliydi. Taşların 13'ü (%42) geometrik şekilli iken hiçbir flebolit geometrik şekilli değildi. Flebolit ve taşların ortalama densite değerleri sırasıyla 386,5 HU (131 HU/935 HU) ve 1088 HU (526 HU - 1594 HU) ölçülmüş olup bu değerler arasındaki fark istatistiksel olarak anlamlı idi (p<0,05). Onsekiz flebolitte (%23) santral lüsensi ve profil analizinde çift tepe bulgusu varken, tüm taşlarda profil analizinde tek tepe bulgusu izlendi ve hiçbirinde santral lüsensi yoktu. Kuyruklu yıldız işareti flebolitlerin 12'sinde (%15) varken bu bulguya hiçbir taşta rastlanılmadı.
Sonuç: Bu çalışmanın sonuçları kontrastsız BT nin üreter taşlarını flenolitlerden ayırtetmede güvenilir ayırtedici kriterlere sahip olduğunu göstermektedir. Bu çalışmada bahsedilen tüm kriterlerin kullanılması üreter taşları ile flebolitlerin ayırtedilmesini kolaylaştıracaktır.
Materials and Methods: Between October 2004 and April 2005, we performed 3 cm length thin-slice (2 mm section thickness, pitch:1) helical CT on 31 patients with urinary stones and on 43 patients with 80 phleboliths. The size, shape, central lucency, soft tissue rim sign, comet-tail sign, density values and profile analysis of each calcification were recorded.
Results: Fifty two (65%) of 80 phleboliths were round and 28 (35%) were oval shape. On the contrary, ten (32%) of 31 stone were round, 8 (26%) of them were of oval shape. Geometric configuration was seen in thirteen (42%) stones but not in any phleboliths. Mean densities of phleboliths and stones were 386,5 HU (131 HU/935 HU) and 1088 HU (526 - 1594), respectively. This difference was statistically significant (p<0,05). Eighteen (23%) of 80 phleboliths had central lucency and bifid peak on profile analysis. All 31 stones had a single peak at profile analysis. Although comet-tail sign was seen at 12 (15%) of 80 phleboliths, we did not observe this sign at stones. We observed soft tissue rim sign on 21 (67%) of 31 stones. However this sign was never seen on phleboliths.
Conclusion: The results of this study indicate that unenhanced helical CT has reliable findings in the differentiation of stones from phleboliths. It is easier to differentiate urinary stones from phleboliths with thin-slice CT. Applying of all criteria mentioned in this study may be useful in differentiation of distal urinary stones from phleboliths on unenhanced helical CT.
Introduction
Materials and Methods
We performed second helical CT on these patients which was focused on stone and with thin slice. Before all CT examinations, we had scout views with 40 cm length, including abdomen and pelvis. Scout view parameters were 250 mA and 120 kV. The window level and window width were 130 and 40, respectively. Helical images were performed with focusing stone on scout image. If stone was not seen on scout image, helical imaging was performed with the aid of KUB film or intravenous urography. The length of helical image was 3 cm. CT was performed with 120 kV, 200 mA, 2 mm/rotation and 2 mm section thickness (pitch: 1). Informations acquired with helical imaging were reconstructed with 2 mm interval. Analysis of digital images were performed on workstation.
Pelvic phlebolith group included patients who had abdominal CT for other reasons and evaluated with symptoms related to other system disorders, Forty three patients (25 men, 18 women) were included in this group. In these 43 patients, 80 phleboliths located along the expected course of the pelvic ureter were identified and included in this analysis. We performed 3 cm length helical CT on these patients with the same parameters as stone group. CT examinations were performed with focusing on calcification detected on scout view and abdominal CT. All CT examinations were performed with Toshiba X-Vision CT scanner. An institutional review board and ethics committee approval, and informed consent from each patient was obtained.
After performing CT examinations, shape (round, oval, geometric), presence of central lucency, soft tissue rim sign (circumferential edema of the ureteral wall surrounding a calculus) and comet-tail sign (adjacent eccentric, tapering soft-tissue mass corresponding to the noncalcified portion of a pelvic vein abutting a phlebolith) of whole stone and phlebolith were investigated. To investigate the presence of central lucency, soft tissue rim sign and comet-tail sign on stones and phleboliths, magnified images with x2 zoom factor were used. Bone window (350 HU/1300 HU) settings were used to see central lucency in addition to soft tissue window settings (45 HU/450 HU). Profile analysis which is a graphic representation of attenuation in each pixel along a line drawn through each calcification was performed. With this analysis, presence of central lucency in calcification (was seen as bifid peak at profile analysis) or uniform attenuation (was seen as single peak at analysis) were evaluated objectively.
We also measured size and densities of stones and phleboliths. On the calcification area, 200 pixels were measured with using 10x20 pixel area. The lowest, highest and mean densities were recorded. In addition to density measurements, maximum transvers and vertical size of stones and phleboliths were measured. Window level and width for density and size measurement were 350 and 1300 respectively.
Two radiologists independently interpreted the CT images and discrepancies were resolved by consensus. All measurements and assesments were done for two times and first measurements were used in the study since there was no statistically difference between two measurements. Mann - Whitney U test was used for comparing the size and density values of distal urinary stones and pelvic phleboliths. Chi-square test was used to compare central lucency, profile analysis, soft tissue rim sign and comet tail sign between two groups. Statistical significance was regarded as P less than 0.05.
Results
Table 1: Mean size end density values of distal ureter stones and pelvic phleboliths.
Fifty two of 80 phleboliths were round (65%) and 28 (35%) were oval shape. On the contrary, ten (32%) of 31 stone were round (Figure 1A), 8 (26%) of them were of oval shape. Geometric configuration was seen in thirteen (42%) stones (Figure 1B) but not in any phleboliths (Table 2). For urinary stones, the positive predictive value of a geometric shape was 100%.
Figure 1: Round (A) and geometric (B) shaped stones are seen on left distal ureters in different patients.
Table 2: The results of shape assesment of distal urinary stones and phleboliths.
Mean densities of phleboliths and stones were 386,5 HU (131 HU/935 HU) and 1088 HU (526 - 1594) (Figure 2), respectively (Table 1). This difference was statistically significant (p<0,05). Although 62 (78%) of 80 phleboliths had density value lower than 524 HU, all stones had density values more than 524 HU.
Figure 2: A geometric shaped stone in left distal ureter. Density measurement revealed mean density as 1473 HU.
Eighteen (23%) of 80 phleboliths had central lucency (Figure 3A) and bifid peak (two peaks of high attenuation spanning a central region of lower attenuation) on profile analysis (Figure 3B). Sixty two (77%) phleboliths showed single peak on profile analysis (Figure 3C). There was neither subjective nor objective evidence at unenhanced helical CT of central low attenuation in any of the 31 stone, all of which had a single peak at profile analysis (Figure 3D). The difference between stones and phleboliths regarding central lucency and bifid peak on profile analysis was statistically significant. For phleboliths, the positive predictive value of both a central lucency and bifid peak at profile analysis was 100% (Table 3).
Figure 3: Central lucencies in phleboliths (A). Bifid peak is seen in a phlebolith on profile analysis (B). Single peak is seen in a phlebolith (C) and single peak in a right distal urinary stone (D).
Table 3: The criteria which can be used to differentiate phleboliths from distal urinary Stones.
Although comet-tail sign was seen at 12 (15%) of 80 phleboliths (Figure 4A), we did not observe this sign at stones. We observed soft tissue rim sign on 21 (67%) of 31 stones (Figure 4B). However this sign was never seen on phleboliths (Table 3). These differences were statistically significant.
Figure 4: Comet-tail sign is seen on phlebolith (A). Soft tissue rim sign representing periureteral edema is seen around the right distal urinary stone (B).
Resultantly, independent variables that correlated best with the diagnosis of a phlebolith were a central lucency, a bifid peak at profile analysis, and the comet-tail sign. Independent variables that correlated best with the diagnosis of a calculus were geometric shape, a single peak at profile analysis, the soft tissue rim sign, and mean attenuation greater than 524 HU.
Discussion
According to literature shape, central lucency, density measurements, soft tissue rim sign, comet tail sign and profile analysis are all recommended for differentiation of phleboliths and urinary stones4,6,7,8. In this study, we assessed the efficacies of these criteria in differentiation.
In our study, 35% of phlebolithis were oval, 65% were round. None of them were geometric. However 32% of stones were round, 26% were oval and 42% were geometric. The sensitivity, specificity and PPV of geometric shape for stones were 42%, 100% and 100%, respectively. These results indicates that shape feature can be used for differentiation of stones from phleboliths. Especially, geometric shape with its high specificity and high PPV, may strongly suggest the possibility of stone and enhances diagnosis in the pelvic calcifications (Figure 1B).
Another criteria investigated in this study was density. We think that standardisation is critical in the measurement of densities. Centralization of calcification and exclusion of soft tissues from measurement area must be carefully applied (Figure 2). In our study mean densities of phleboliths and stones were significantly different from each other. However, these results differ from other studies in literature. In their study Bell et al. measured the mean density of phleboliths and stones as 160 HU (80 -278 HU) and 305 HU (221 – 530 HU) respectively4. The difference between these results may be attributed to different composition of stones and phleboliths in Turkish people. Although different density levels for stones and phleboliths are reported in literature, we think that mean density value is an objective criteria in distinction since it is a quantitative data. According to the measurements, densities of 62 (78%) of 80 phleboliths were under 524 HU, and density values of all stones were over 524 HU. The density values under 524 HU had 100% specificity and PPV for phleboliths in our study. Thus, our findings suggest density measurement as a reliable indicator for differentiation between stones and phleboliths.
A central lucency in a calcification can be seen ideally in a magnified bone window (500 HU/2000 HU) images (Figure 3A). In vitro studies state that phleboliths tends to be round and contain central lucency, that calculi have opposite tendencies9. None of stones showed central lucency in our study. Although central lucency seems to be a specific indicator for phleboliths with its high specificity (100%) and PPV (100%) for phleboliths in our study reports in the literature stated that this finding could be shown in stones too7,10. We think that making profile analysis and showing bifid peak in this analysis is a more objective method for depicting low density in the central part of calcification than subjective visual assesment of central lucency. In our study, 23% of phleboliths showed central lucency and bifid peak on profile analysis (Figure 3B). In other studies, Fox et al. and Traubici et al. reported that these findings are not useful for stone-phleboliths differentiation. However Bell et al. suggested that these criteria may be helpful in differential diagnosis4,7,10. In our opinion, appropriate window setup and profile analysis facilitate the availability of these findings for this purpose.
Comet-tail sign, a linear or curvilinear soft-tissue structure extending from an abdominal or pelvic calcification, generally indicates that a calcification is a phlebolith4,11. We found comet-tail sign in 15% of phleboliths, but not in any of the stones (Figure 4A). High specificity (100%) and PPV (100%) of this sign for phleboliths indicates its value in the distinction between phleboliths and urinary stones.
The sensitivity of central lucency and bifid peak on profile analysis (23%) and comet-tail sign (15%) is low in the differentiation of distal urinary stones and phleboliths. Pre-sence of these criteria is significant in the distinction because their presence refers only phleboliths with their 100% value of specificity for phleboliths but has limited value because of low incidence.
Soft tissue rim sign was found in 67% of stones and none of phleboliths. The specificity and PPV of this sign for stones are 100%. Also high NPV (86%) of this sign for urinary stones indicates its reliability. However Heneghan et al. and Bell et al. found this sign in 8% and 2% of phleboliths4,6. The difference of these studies from our study in this subject may be according to CT technique. We used 2 mm section thickness and 2 mm gap that would prevent misdiagnosis of noncalcified portion of pelvic vein as soft tissue rim sign (Figure 4B).
The results of this study indicate that unenhanced helical CT has reliable findings in the differentiation of stones from phleboliths. Presence of central lucency, bifid peak on profile analysis and comet tail sign have 100% specificity and PPV for diagnosis of phleboliths. These findings are not seen usually (23%, 23% and 15% respectively) but presence of them in a calcification means no possibility for stone. Geometric shape and soft tissue rim sign have high sensitivity and specificity values for stone detection. Differences in density values of stones and phleboliths are reliable and distinctive criteria for this purpose. It is easier to differentiate urinary stones from phleboliths with thin-slice CT. Applying of all criteria mentioned in this study may be useful in differentiation of distal urinary stones from phleboliths on unenhanced helical CT.
The results of this study indicate that unenhanced helical CT has reliable findings in the differentiation of stones from phleboliths. It is easier to differentiate urinary stones from phleboliths with thin-slice CT. Applying of all criteria mentioned in this study may be useful in differentiation of distal urinary stones from phleboliths on unenhanced helical CT.
References
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