Ureterolithiasis, also known as ureteric calculi, is the presence or formation of stones within the ureters, which are the tubes responsible for the passage of urine from the kidneys to the bladder.
Most of these stones, approximately 80%, are found to be composed predominantly of calcium. Comparatively, approximately 15% of these ureter stones are made of struvite, which is magnesium ammonium phosphate formed by urea-splitting gram-negative bacteria. A smaller percentage of these ureter stones is made up of uric acid stones, while an even smaller number of them contain cysteine.
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The environmental factor considered to be the most important cause of stone formation is inadequate fluid intake. Other factors implicated in the etiopathogenesis include diet, heredity, urinary tract anatomical abnormalities, chronic urinary tract infections (UTIs), hormonal imbalances, metabolic dysfunction, and dry/hot climates.
Ureterolithiasis may cause a patient to experience colicky pain that is abrupt in onset and accompanied by symptoms such as nausea, vomiting, and hematuria, or blood in the urine. Depending on where within the ureters the stones are impacted, the pain may radiate to the back, flank, and/or lower abdomen.
A number of imaging modalities, together with urinalysis and blood tests, may be employed to aid in the diagnosis of ureteric calculi. Most notably, ultrasonography, kidney-ureter-bladder (KUB) radiographs, and computed tomography (CT) scans may be used. Other less frequently used diagnostic approaches are pyelography and renal nuclear scans with radioisotopes.
Several factors, such as stone composition, size, and associated symptoms are taken into account when determining what treatment approaches to take for the management of ureteric calculi. Some stones require only observation and analgesics with the anticipation that they will pass spontaneously. In contrast, other stones may require pharmacotherapy, mechanical or surgical therapy.
Observation and analgesics
The wait-and-watch approach is adopted for stones that are small, which is defined as a stone with a diameter of less than 4 mm. These smaller stones have a higher chance of passing out of the body spontaneously in the urine.
Spontaneous passage of ureteric calculi is inversely proportional to the size. Moreover, the larger the stone, the less likely it is to pass on its own.
Other predictors of spontaneous stone passage are the exact location within the ureter and the shape of the stone. Stones lodged at the ureteropelvic junction, for example, are more difficult to pass. Patients are encouraged to increase their fluid intake during the observation period.
Ureteric calculi that are composed of uric acid or cysteine may be managed with drug therapy to bring about their dissolution.
Alkalization of the urine at a pH between 6.5 – 7.0 may be achieved with agents like potassium citrate to encourage the dissolution of uric acid stones. This is because these stones are fostered by acidic environments; thus, making the urine more alkaline inhibits the formation of new calculi and further growth of existing calculi.
This approach can also be used for the dissolution of cystine calculi; however, these stones are more difficult to dissolve. In contrast to both uric acid and cysteine calculi, it is impossible to dissolve calcium stones by pharmacotherapy.
Stones that fail to pass spontaneously, those that are too large to pass, or stones associated with other serious complications are candidates for surgical therapy. Infection is a particular complication that requires urgent attention. Surgical options include stenting, ureteroscopy, and extracorporeal shockwave lithotripsy (ESWL).
Stents are inserted endoscopically into the affected ureter to keep the ureter patent and ensure that the ureter will be able to drain urine from the kidneys to the bladder. Furthermore, these stents act as stabilizing landmarks during ESWL; however, they may cause the patient some discomfort.
ESWL, as opposed to stenting and ureteroscopy, is the least invasive of the three methods. To this end, ESWL employs sound waves at very high energy to break up large ureteric calculi into smaller chunks that are capable of being passed in the urine. This mode of therapy is appropriate for stones that are smaller than 20 mm in diameter; however, ESWL is not suitable even then in some situations.
For example, pregnancy is a contraindication to the use of ESWL. Stones that are between 10 to 20 mm can be manipulated by ureteroscopy, which is performed with the help of an endoscope equipped with a basket to capture stones. In some cases, extra laparoscopic ports are used to introduce special tools to fragment slightly larger stones before capturing them.