The high prevalence and recurrence rate of urolithiasis has attracted more and more attention. A complete understanding of calculi information before treatment helps select a reasonable and practical treatment plan and improve the treatment success rate, such as the composition type, size and location of calculi. The composition of calculi has different physical and solid properties, which directly affect the success of treatment[16]. Calcium oxalate calculi are the most common composition of urolithiasis. It has a dense structure, hard texture, smooth surface or mulberry shape, and the treatment effect of extracorporeal shock wave lithotripsy (ESWL) is poor. Carbonate apatite is an infectious calculi which should be removed as much as possible during the operation, and urinary tract infection and acidified urine should be actively controlled after operation to prevent recurrence and rapid growth of calculi. Uric acid calculi are soft and can be treated with medicine. Therefore, understanding the composition of calculi before treatment is both an advantage and a trend.
Currently, there are many studies on applying NCCT to predict the composition of urinary calculi. Torricelli et al. found that the HU value of cystine calculi was 648 ± 122 HU and that of calcium oxalate calculi was 1099 ± 239 HU, which successfully distinguished calcium oxalate calculi from cystine calculi[17]. Pareek et al. found that HU value ≤ 500 HU and urinary pH ≤ 5.5 could be used to distinguish uric acid calculi from calcium-containing calculi[18–19]. Similarly, the HU value of calcium-containing calculi was higher in adults compared with uric acid calculi and cystine calculi[17]. Lee et al. showed that the HU value of uric acid calculi, phosphate calculi and calcium oxalate calculi were 513 ± 197 HU, 1660 ± 292 HU and 1684 ± 290 HU, respectively, which successfully distinguishing uric acid calculi from calcium-containing calculi[20]. In our study, we distinguished the composition of the subgroup calculi, and the results showed that the cut-off value of calcium oxalate dihydrate calculi for distinguishing carbonate apatite calculi and anhydrous uric acid calculi were 1063.00HU and 644.00 HU, respectively. The cut-off value of anhydrous uric acid calculi to distinguish carbonate apatite and calcium oxalate monohydrate calculi was 644.00 HU, respectively. In summary, an HU value ≤ 644.00 could be used to distinguish calcium-containing calculi from anhydrous uric acid calculi. Our results are consistent with previous studies, showing that the HU value of calcium-containing calculi is higher than that of anhydrous uric acid calculi, and the HU value of NCCT can be used to distinguish calcium-containing calculi from anhydrous uric acid calculi.
Although NCCT has become the gold standard for diagnosing of urolithiasis, ultrasound is widely used to diagnose urinary calculi in the daily examination, which is economical, convenient and safe. Recent studies have reported that the sensitivity and specificity of ultrasound in the diagnosis of urolithiasis are 90–93% and 95–100%, respectively[21]. Ultrasound can provide clinicians with rich information, including the calculi size, number, location, and degree of obstruction. The accuracy and information ultrasound provides in diagnosing urinary calculi are similar to that of NCCT. Therefore, in this study, we made a quantitative analysis of the strong echo and posterior acoustic shadow by using the ultrasonic characteristics of urinary calculi to analyze the feasibility of the preliminary prediction of the composition of urinary calculi by ultrasound. The results showed that the grayscale value of strong echo of calcium-containing calculi in this study was higher than that of anhydrous uric acid calculi. The cut-off value of calcium-containing calculi and anhydrous uric acid calculi was 200.29; that is, the grayscale value of strong echo of calculi on ultrasound was ≤ 200.29, which can preliminarily distinguish calcium-containing calculi and anhydrous uric acid calculi. The results were similar to those of NCCT in predicting calculi composition.
For the posterior acoustic shadow of urinary calculi, the degree of the ultrasonic manifestation is different, and the influence of the different chemical compositions of urinary calculi on the posterior acoustic shadow has been widely discussed. King et al. showed that the chemical composition of the calculi had no apparent effect on the posterior acoustic shadow. At the same time, the rough texture of the tissue could affect the posterior acoustic shadow behind the small calculi[22]. Rubin et al. revealed that surface topography, such as roughness and radian of calculi, could affect the clarity of the posterior acoustic shadow[23]. The posterior acoustic shadow of the calculi with a rough surface and small radian is clear. In contrast, the posterior acoustic shadow of calculi with a smooth surface and large radian is shallow. However, some scholars indicated that the more calcium in tissues, the more pronounced the sound attenuation[24], i.e., the lower the degree of posterior acoustic shadow echo and the lower the grayscale value. According to our findings, the posterior acoustic shadow grayscale values in the CA group were lower than in the UA0 group and more apparent than in the UA0 group, which indicates a relationship between the chemical composition of the calculi and the echo degree of the posterior acoustic shadow, which may be related to the difference in the number of calcium elements and elements of different substances. The CA group contains high calcium and has more substantial ultrasonic acoustic attenuation, lower echo, and more apparent posterior acoustic shadow. In contrast, the UA0 group does not contain calcium elements, has relatively weaker acoustic attenuation, higher echo, and produces lighter acoustic shadow and higher grayscale value. The results of calculi composition analysis by using energy spectral CT showed that high atomic number substances mainly produce photoelectric absorption effects. Carbonate apatite contains high-order chemical elements (Ca, P, S) with strong x-ray attenuation. In contrast uric acid contains low-order chemical elements (H, C, N, O) with low x-ray attenuation, suggesting a correlation between acoustic attenuation and the order of chemical elements. This is similar to our findings that calcium-containing calculi are significantly more posteriorly attenuated than non-calcium-containing calculi, with lower posterior acoustic echoes and grayscale values.
This study also found a relationship between the HU value of calculi and the grayscale value of calculi strong echo. It is suggested that the echo of calculi on ultrasound is more substantial, its HU value may be more significant, and its calcium content is more. The more pronounced the posterior attenuation is, the lower the echo of the posterior acoustic shadow is. On the contrary, the echo of calculi on ultrasound is reduced. Its HU value may be smaller, with less calcium or non-calcium content, and the posterior acoustic shadow is lighter. The results of this study still have some implications for the treatment of urolithiasis. For example, uric acid calculi, negative calculi without X-ray development, can be identified by ultrasound. The grayscale value of the strong echo and the posterior acoustic shadow determined the calculi properties. Uric acid calculi can be dissolved clinically by alkalinizing urine with drugs to avoid ESWL or surgical treatment[25]. In addition, the treatment of urolithiasis is not only concerned with the chemical composition of the calculi; calculi size is also a critical factor in determining the treatment plan for urolithiasis[26]. In order to improve the accurate measurement of the calculi size by ultrasound, the width of the posterior acoustic shadow is used as an additional measure, especially for calculi size ≤ 5 mm[27–29]. Most calculi without posterior acoustic shadows were ≤ 5 mm, and these had the highest possibility of spontaneous calculi discharge[30]. Therefore, the accurate measurement of calculi size by posterior acoustic shadow is also of guiding significance for urolithiasis treatment.
In this study, the sensitivity and specificity of using HU value to distinguish calcium-containing calculi from anhydrous uric acid calculi were 85.87% − 95.24% and 66.67% − 95.43%, respectively. The sensitivity and specificity were 38.84%-96.00% and 37.56% − 96%, respectively, for distinguishing calcium-containing calculi from anhydrous uric acid calculi using the grayscale value of the calculi and the posterior acoustic shadow on ultrasound. Although the sensitivity of ultrasound to predict urinary calculi composition is lower than that of NCCT, it may be due to the small number of patients in the subgroup of this study. In addition, the ROIs of the strong echo of calculi and the posterior acoustic shadow are artificially determined. Determining the possible boundary may need to be more accurate to affect the study results. However, this study quantified the characteristics of calculi on ultrasound. It made a preliminary prediction of calculi composition, which provided an empirical basis for future research, aiming to hope that ultrasound may be a valuable tool for predicting urinary calculi composition and providing more information for the treatment choice and follow-up review of urolithiasis.