Holmium:YAG lithotripsy yields smaller fragments than lithoclast, pulsed dye laser or electrohydraulic lithotripsy

Holmium:YAG laser for urinary stones

OBJECTIVE

To evaluate the results of Holmium:YAG (Ho:YAG) laser lithotripsy in the treatment of urinary stones.

MATERIAL AND METHODS

Between 1993 and 1997, 59 patients with 85 urinary stones were treated with the Ho:YAG laser lithotripsy. Retrospective evaluation was done on the 64 procedures available, comprising 53 ureteric, 8 bladder, and 2 renal calculi, and one stone in a ureterocele.

RESULTS

The Ho:YAG laser fragmented all types of calculi. Of 38 patients, 29 (76%) with ureteric stones were stone-free and 7 (18%) had stone fragments smaller than 2 mm left 1-3 months after the lithotripsy, resulting in a total clinical success rate of 95%. The procedure caused four ureteric perforations. One ureteric stricture, after repeated treatments for a Steinstrasse formation, led to nephrectomy.

CONCLUSIONS

The Ho:YAG laser was reliable and effective for most of the urinary stones. The largest stones in any location, and stones of hard composition, however, were treated with combined disintegration methods. Four minor ureteric perforations and one ureteric stricture were related to laser use.

Holmium: YAG lithotripsy: optimal power settings

PURPOSE

We tested the hypothesis that holmium:YAG laser lithotripsy speed is best maximized by using low pulse energy at high pulse frequency.

MATERIALS AND METHODS

To demonstrate that optical fiber damage increases with pulse energy and irradiation, the 365-microm optical fiber irradiated calcium hydrogen phosphate dihydrate (CHPD), calcium oxalate monohydrate (COM), cystine, magnesium ammonium phosphate hexahydrate (MAPH), and uric acid calculi at pulse energies of 0.5 to 2.0 J. Optical energy output was measured with an energy detector after 10 J to 200 J of total energy. To demonstrate that lithotripsy efficiency varies with power, fragmentation was measured at constant power settings at total energies of 200 J and 1 kJ with the 365-microm optical fiber. Fragmentation was measured for the 272-microm optical fiber at pulse energies of 0.5 J to 1.5 J at 10 Hz. To demonstrate that low pulse energy produces smaller fragments than high pulse energy, fragment size was characterized for COM and uric acid calculi after 0.25 kJ of irradiation using the 272-microm to 940-microm optical fibers at 0.5 J to 1.5 J.

RESULTS

Damage to the 365-microm optical fiber was greatest for irradiation of CHPD, followed by MAPH, and COM (P<0.001). There was no significant optical fiber damage after cystine and uric acid lithotripsy. For the 365-microm optical fiber and CHPD, fragmentation after 200 J was greatest for pulse energies < or =1.0 J (P< 0.001). For other compositions, fragmentation was not statistically different among the power settings for constant irradiation. No significant difference was noted in fragmentation for any composition at different pulse energies (1.0 v. 2.0 J) for 1-kJ irradiation. However, for all compositions, the calculated lithotripsy speed was greatest at high power settings (P<0.001). For the 272-microm optical fiber, CHPD fragmentation was greatest for the 1.0-J pulse energy. The mean fragment size and relative quantity of fragments > or =2 mm both increased as pulse energy increased.

CONCLUSIONS

Optical fiber degradation varies with stone composition, irradiation, and pulse energy. Holmium:YAG lithotripsy speed is maximized with higher power (either increased pulse energy or higher pulse frequency). Because low pulse energy may be safer and yields smaller fragments than high pulse energy, holmium:YAG lithotripsy speed is best increased by using pulse energies < or =1.0 J at a high repetition rate.

Holmium:YAG lithotripsy for large renal and bladder calculi: strategies for efficient lithotripsy

Holmium:YAG lithotripsy is effective for all stone compositions, and high success rates may be expected. Large renal and bladder calculi may be treated effectively with Ho:YAG lasertripsy. Using angled optical fibers and increasing power settings may be particularly useful to increase lithotripsy speed.

Identifying stone composition using infrared analysis of filtered urine after ureteroscopic lithotripsy

BACKGROUND AND PURPOSE

With the development of small-caliber ureteroscopes and lithotripsy devices, it is now possible to perform intracorporeal stone fragmentation without dilatation of the ureteral orifice. Ureteral stones are typically fragmented into small particles that can be difficult to retrieve for stone analysis. Infrared spectroscopy (IRS) of the precipitate from urine after intracorporeal lithotripsy represents a method for obtaining stone analysis.

PATIENTS AND METHODS

A total of 69 patients underwent ureteroscopic lithotripsy with the holmium laser or the electrohydraulic probe for stones in the ureter (N = 65) or kidney (N = 4). Each patient's bladder was then drained and the urine filtered. The resulting precipitate was analyzed using IRS.

RESULTS

The amount of material for analysis was < or =1 mg in 56 patients (82%). Stone composition was positively identified in 44 patients (64%). Material suitable for analysis was recovered from 73% of patients when the bladder was drained with a cystoscope sheath compared with 43% when a urethral catheter was used (P = 0.03). There was no significant difference in pretreatment stone size in the patients who had a positive v a negative result (11.7 mm v 10.9 mm; P = 0.06). Similarly, the stone location was not significantly related to the likelihood of positive analysis (P = 0.29).

CONCLUSION

Straining the urine after ureteroscopic intracorporeal lithotripsy and analyzing the precipitate with IRS is able to identify stone composition in the majority of patients. This method is especially useful in the setting of holmium laser lithotripsy, in which the majority of the stone is converted to spontaneously passable particles.

Electrokinetic lithotripsy: safety, efficacy and limitations of a new form of ballistic lithotripsy

OBJECTIVE

To investigate the safety and efficacy of electrokinetic lithotripsy (EKL), a ballistic lithotripter which uses high-energy magnetic fields to propel an impactor to fragment calculi.

PATIENTS AND METHODS

The records and radiographs of 121 patients who underwent ureteroscopy using the EKL for stones in the upper (26), mid (28) or lower (67) ureter were reviewed retrospectively. Ureteroscopy was performed with an 8.5 F semi-rigid ureteroscope, through which a 3 F EKL probe was passed.

RESULTS

A total of 148 stones (mean stone size 11.5 mm, range 6-40) in 121 patients were treated using the EKL. One patient was lost to follow-up. Of 148 stones, 147 (99.3%) were fragmented, including five that had resisted fragmentation with either pulsed-dye laser or electrohydraulic lithotripsy. Despite this, only 45 of 56 patients (80%) with a single stone in the lower ureter were rendered stone-free after a single ureteroscopic procedure. Seven patients in this group (12%) required shock-wave lithotripsy for fragments that had been propelled into the kidney, while four patients (7%) required repeat ureteroscopy for retained ureteric fragments. Complications were limited to minor ureteric perforations in two patients, both of which were treated with a stent.

CONCLUSION

EKL is an inexpensive and reliable endoscopic method which fragments nearly all urinary calculi. Its limitations include the propulsion of fragments and the need to use an offset, semi-rigid ureteroscope. We recommend the use of a basket or graspers to remove fragments of >/=4 mm after EKL.

Ureteroscopic lithotripsy

The indications for ureteroscopic lithotripsy have increased with endoscope miniaturization and powerful, precise endoscopic lithotrites like the holmium: yttrium-aluminum-garnet laser. Successful ureteropyeloscopic treatment with the currently available instrumentation and techniques is independent of the size, composition, and location of stones in the upper urinary tract. Extracorporeal shockwave lithotripsy maintains a major role in treating uncomplicated, moderately sized upper urinary tract calculi. Complex upper urinary tract calculi, however, are best treated endoscopically. In addition, the endoscopic treatment of ureteral calculi is efficacious and definitive, albeit more invasive than extracorporeal shock wave lithotripsy.

Holmium: YAG lithotripsy: photothermal mechanism

OBJECTIVE

A series of experiments were conducted to test the hypothesis that the mechanism of holmium:YAG lithotripsy is photothermal.

METHODS AND RESULTS

To show that holmium:YAG lithotripsy requires direct absorption of optical energy, stone loss was compared for 150 J Ho:YAG lithotripsy of calcium oxalate monohydrate (COM) stones for hydrated stones irradiated in water (17+/-3 mg) and hydrated stones irradiated in air (25+/-9 mg) v dehydrated stones irradiated in air (40+/-12 mg) (P < 0.001). To show that Ho:YAG lithotripsy occurs prior to vapor bubble collapse, the dynamics of lithotripsy in water and vapor bubble formation were documented with video flash photography. Holmium:YAG lithotripsy began at 60 microsec, prior to vapor bubble collapse. To show that Ho:YAG lithotripsy is fundamentally related to stone temperature, cystine, and COM mass loss was compared for stones initially at room temperature (approximately 23 degrees C) v frozen stones ablated within 2 minutes after removal from the freezer. Cystine and COM mass losses were greater for stones starting at room temperature than cold (P < or = 0.05). To show that Ho:YAG lithotripsy involves a thermochemical reaction, composition analysis was done before and after lithotripsy. Postlithotripsy, COM yielded calcium carbonate; cystine yielded cysteine and free sulfur; calcium hydrogen phosphate dihydrate yielded calcium pyrophosphate; magnesium ammonium phosphate yielded ammonium carbonate and magnesium carbonate; and uric acid yielded cyanide. To show that Ho:YAG lithotripsy does not create significant shockwaves, pressure transients were measured during lithotripsy using needle hydrophones. Peak pressures were <2 bars.

CONCLUSION

The primary mechanism of Ho:YAG lithotripsy is photothermal. There are no significant photoacoustic effects.

Percutaneous nephrolithotomy in infants and preschool age children: experience with a new technique

OBJECTIVES

To develop a less invasive method for performing percutaneous nephrolithotomy (PCNL) with the intent of decreasing the morbidity of the procedure in young children.

METHODS

A novel percutaneous renal access technique ("mini-perc") was developed using an 11F peel-away vascular access sheath. Tract dilation and insertion of the sheath into the collecting system was performed with a single pass over an access wire. PCNL was performed using pediatric instruments and electrohydraulic lithotripsy. Sheath design improvements were implemented that make it specific for pediatric PCNL.

RESULTS

Eleven procedures have been performed with the 11F sheath. Patient age ranged from 2 to 6 years (mean 3.4) and weight from 5 to 24 kg (mean 12.5). The average stone burden was 1.2 cm2. Mean procedure time, estimated blood loss, and length of hospitalization were 203 minutes, 25 mL, and 6 days, respectively. Six (85%) of 7 patients are currently stone free with an average follow-up of 12 weeks. No patient required transfusion, developed urosepsis, or had a procedure-related complication. One procedure was performed in an outpatient setting with no postoperative nephrostomy tube.

CONCLUSIONS

The 11F "mini-perc" technique was successful in rendering 85% of patients stone free with minimal morbidity. Its advantages over obtaining access with standard 24 to 34F access sheaths include a smaller skin incision, single-step dilation and sheath placement, good working access for pediatric instruments, variable length, and lower cost. In addition, the hypothesized decrease in renal and body wall trauma may result in less pain, reduced severity or risk of complications, and shorter hospital stays including the possibility of performing "tubeless" outpatient PCNLs. Further study is needed to confirm these possibilities.

Holmium:yttrium-aluminum-garnet lithotripsy efficiency varies with stone composition

OBJECTIVES

To test the hypothesis that holmium:yttrium-aluminum-garnet (YAG) lithotripsy efficiency varies with stone composition.

METHODS

Single pulses of holmium:YAG energy were delivered using 272-, 365-, 550-, and 940-microm optical fibers to human calculi composed of calcium oxalate monohydrate (COM), calcium hydrogen phosphate dihydrate (CHPD), cystine, magnesium ammonium phosphate hexohydrate (MAPH), and uric acid. Energy/pulse settings were 0.2, 0.5, 1.0, and 1.5 J. Stone crater width and depth were characterized with reflectance light microscopy.

RESULTS

For similar energies overall MAPH yielded the deepest and widest craters. CHPD, cystine, and uric acid yielded craters of intermediate width and depth. COM yielded the smallest craters. Within any given composition, increased pulse energy yielded craters of increased width and depth.

CONCLUSIONS

Holmium:YAG lithotripsy efficiency varies with stone composition. The rank order of crater size appears to correlate with thermal threshold for each composition. Increased holmium:YAG energy produces larger craters for all compositions.

Holmium:YAG lithotripsy: photothermal mechanism converts uric acid calculi to cyanide

PURPOSE

Holmium:YAG lithotripsy fragments stones through a photothermal mechanism. Uric acid when heated is known to be converted into cyanide. We test the hypothesis that holmium: YAG lithotripsy of uric acid calculi produces cyanide.

MATERIALS AND METHODS

Human calculi of known uric acid composition were irradiated with holmium:YAG energy in water. Stones received a total holmium:YAG energy of 0 (control), 0.1, 0.25, 0.5, 0.75, 1.0 or 1.25 kJ. The water in which lithotripsy was performed was analyzed for cyanide concentration. A graph was constructed to relate holmium:YAG energy to cyanide production.

RESULTS

Holmium:YAG lithotripsy of uric acid calculi in vitro produced cyanide consistently. Cyanide production correlated with total holmium:YAG energy (p <0.001).

CONCLUSIONS

Holmium:YAG lithotripsy of uric acid calculi risks production of cyanide. This study raises significant safety issues.

Holmium:YAG lithotripsy efficiency varies with energy density

PURPOSE

We test the hypothesis that holmium:YAG lithotripsy efficiency varies with optical fiber size and energy settings (energy density).

MATERIALS AND METHODS

The 272, 365, 550 and 940 microm. optical fibers delivered 1 kJ. total holmium:YAG energy to calcium oxalate monohydrate calculi at energy output/pulse of 0.2 to 1.5 J. Stone mass loss was measured for each fiber energy setting. Stone crater width was characterized for single energy pulses. Fiber energy outputs were compared before and after lithotripsy.

RESULTS

Stone mass loss correlated inversely with optical fiber diameter (p <0.05). Stone loss correlated with energy/pulse for the 365, 550 and 940 microm. fibers (p <0.001). The 272 and 365 microm. fibers yielded equivalent stone loss at 0.2 and 0.5 J. per pulse. At energies of 1.0 J. per pulse or greater the 272 microm. optical fiber was prone to damage, and yielded reduced energy output and stone loss compared to the 365 microm. fiber (p <0.01). Stone crater width for single pulse energies correlated with energy settings for all fibers (p <0.001).

CONCLUSIONS

Lithotripsy efficiency with the holmium:YAG laser depends on pulse energy output and diameter of the optical delivery fiber, implying that lithotripsy efficiency correlates with energy density. The 365 microm. fiber is indicated for most lithotripsy applications. The 272 microm. fiber is susceptible to damage and inefficient energy transmission at energies of 1.0 J. per pulse or greater. The 272 microm. fiber is indicated at energies of less than 1.0 J. per pulse for small caliber ureteroscopes or when maximal flexible ureteroscope deflection is required.