# 12 - 330 Nephrolithiasis

## 330 Nephrolithiasis

COVID-19 AND MICROVASCULAR DISEASE
The COVID-19 pandemic, cause by SARS-CoV-2, has led to many com­
plications, including both macrovascular and microvascular thrombo­
ses. SARS-CoV-2 attaches to the cell membrane via interaction of the 
viral spike protein with the ACE2 protein and then enters the cell via 
endocytosis, leading to increased cytokine release, inflammatory cell 
activation, and cellular and tissue damage. Endothelial injury and dys­
function in the setting of COVID-19 have led to many microvascular 
phenotypes including renal injury, heart disease, liver complications, 
strokes, and respiratory distress syndrome. In response to SARSCoV-2, endothelial exocytosis occurs, releasing von Willebrand factor 
and P-selectin from granules. Autopsy specimens have shown evidence 
of small-vessel occlusions in the heart, kidneys, and lungs. Certain fac­
tors related to microvascular damage, such as ADAMTS13, VEGF-A, 
and Angpt-2, have been shown to predict mortality. In the renal sys­
tem, autopsies showed diffuse proximal tubule injury, which is thought 
to be due to the immune dysregulation and inflammatory cytokines, 
in addition to poor renal perfusion. In certain instances, viral particles 
have been observed in the tubular epithelium, although direct infection 
of SARS-CoV-2 in the kidney remains controversial. Having previous 
chronic kidney disease or diabetic nephropathy is a risk factor for 
developing acute kidney injury with COVID-19. Treatment includes 
antiviral medications and remdesivir, with these medications needing 
to be adjusted or avoided based on kidney function.

PART 9
Disorders of the Kidney and Urinary Tract
Acknowledgment
Ronald S. Go and Nelson Leung contributed to this chapter in the 
21st edition and some material from that chapter has been retained here.
■
■FURTHER READING
Al-Nouri ZL et al: Drug-induced thrombotic microangiopathy: A 
systematic review of published reports. Blood 125:616, 2015.
Barbhaiya M et al: ACR/EULAR APS Classification Criteria Collabo­
rators. The 2023 ACR/EULAR antiphospholipid syndrome classifica­
tion criteria. Arthritis Rheumatol 75:1687, 2023.
Brocklebank V et al: Thrombotic microangiopathy and the kidney. 
Clin J Am Soc Nephrol 13:300, 2018.
Fakhouri F et al: How I diagnose and treat atypical hemolytic uremic 
syndrome. Blood 141:984, 2023.
George JN, Nester CM: Syndromes of thrombotic microangiopathy. 
N Engl J Med 371:1847, 2014.
Go RS et al: Thrombotic microangiopathy care pathway: A consensus 
statement for the Mayo Clinic Complement Alternative PathwayThrombotic Microangiopathy (CAP-TMA) Disease-Oriented 
Group. Mayo Clin Proc 91:1189, 2016.
Liu N et al: Direct promoter repression by BCL11A controls the fetal to 
adult hemoglobin switch. Cell 2018173:430, 2018.
Zabatta E et al: Therapy of scleroderma renal crisis: State of the art. 
Autoimmun Rev 17:882, 2018.
Gary C. Curhan

Nephrolithiasis
Nephrolithiasis, or kidney stone disease, is a common, painful, and 
costly condition. Each year, billions of dollars are spent on nephroli­
thiasis-related activity, with the majority of expenditures on surgical 
treatment of existing stones. While a stone may form due to crystalliza­
tion of lithogenic factors in the upper urinary tract, it can subsequently 
move into the ureter and cause renal colic. Although nephrolithiasis 
is rarely fatal, patients who have had renal colic report that it is the 
worst pain they have ever experienced. The evidence on which to base 

clinical recommendations is not as strong as desired; nonetheless, most 
experts agree that the recurrence of most, if not all, types of stones 
can be prevented with careful evaluation and targeted recommenda­
tions. Preventive treatment may be lifelong; therefore, an in-depth 
understanding of this condition must inform the implementation of 
tailored interventions that are most appropriate for and acceptable to 
the patient.
There are several types of kidney stones. It is clinically important to 
identify the stone type, which informs prognosis and selection of the 
optimal preventive regimen. Calcium oxalate stones are most common 
(~75%); next, in order, are calcium phosphate (~15%), uric acid (~8%), 
struvite (~1%), and cystine (<1%) stones. Many stones are a mixture 
of crystal types (e.g., calcium oxalate and calcium phosphate) and also 
contain protein in the stone matrix. Rarely, stones are composed of 
medications, such as acyclovir, atazanavir, and triamterene. Stones that 
form as a result of an upper tract infection, if not appropriately treated, 
can have devastating consequences and lead to end-stage renal disease. 
Consideration should be given to teaching practitioners strategies to 
prevent recurrence of all stone types and the related morbidity.
■
■EPIDEMIOLOGY
Nephrolithiasis is a global disease. Data suggest an increasing preva­
lence, likely due to Westernization of lifestyle habits (e.g., dietary 
changes, increasing body mass index). National Health and Nutrition 
Examination Survey data for 2007–2016 indicate that up to 20% of 
men and 10% of women will develop at least one stone during their 
lifetime. The prevalence is ~50% lower among black individuals than 
among whites. The incidence of nephrolithiasis (i.e., the rate at which 
previously unaffected individuals develop their first stone) also varies 
by age, sex, and race. Among white men, the peak annual incidence 
is ~3.5 cases/1000 at age 40 and declines to ~2 cases/1000 by age 70. 
Among white women in their thirties, the annual incidence is ~2.5 
cases/1000; the figure decreases to ~1.5/1000 at age 50 and beyond. 
In addition to the medical costs associated with nephrolithiasis, this 
condition also has a substantial economic impact, as those affected are 
often of working age. Once an individual has had a stone, the preven­
tion of a recurrence is essential. Published recurrence rates vary by the 
definitions and diagnostic methods used. Some reports have relied on 
symptomatic events, while others have been based on imaging. Most 
experts agree that radiographic evidence of a second stone should 
be considered to represent a recurrence, even if the stone has not yet 
caused symptoms.
■
■ASSOCIATED MEDICAL CONDITIONS
Nephrolithiasis is a systemic disorder. Several conditions predispose 
to stone formation, including gastrointestinal malabsorption (e.g., 
Crohn’s disease, gastric bypass surgery), primary hyperparathyroid­
ism, obesity, type 2 diabetes mellitus, and distal renal tubular acidosis. 
A number of other medical conditions are more likely to be present in 
individuals with a history of nephrolithiasis, including hypertension, 
gout, cardiovascular disease, cholelithiasis, reduced bone mineral den­
sity, and chronic kidney disease.
Although nephrolithiasis does not directly cause upper urinary tract 
infections (UTIs), a UTI in the setting of an obstructing stone is a uro­
logic emergency (“pus under pressure”) and requires urgent interven­
tion to reestablish drainage.
■
■PATHOGENESIS
In the consideration of the processes involved in crystal formation, it 
is helpful to view urine as a complex solution. A clinically useful con­
cept is supersaturation (the point at which the concentration product 
exceeds the solubility product). However, even though the urine in 
most individuals is supersaturated with respect to one or more types 
of crystals, the presence of inhibitors of crystallization prevents the 
majority of the population from continuously forming stones. The 
most clinically important inhibitor of calcium-containing stones is 
urine citrate. While the calculated supersaturation value does not per­
fectly predict stone formation, it is a useful guide as it integrates the 
multiple factors that are measured in a 24-h urine collection.

Recent studies have changed the paradigm for the site of initiation 
of stone formation. Renal biopsies of stone formers have revealed 
calcium phosphate in the renal interstitium. It is hypothesized that 
this calcium phosphate deposits at the thin limb of the loop of Henle 
and then extends down to the papilla and erodes through the papillary 
epithelium, where it provides a site for deposition of calcium oxalate 
and calcium phosphate crystals. The majority of calcium oxalate stones 
grow on calcium phosphate at the tip of the renal papilla (Randall’s 
plaque). Tubular plugs of calcium phosphate may be the initiating 
event in calcium phosphate stone development. Thus, the process of 
stone formation may begin years before a clinically detectable stone is 
identified. The processes involved in interstitial deposition are under 
active investigation.
■
■RISK FACTORS
Risk factors for nephrolithiasis can be categorized as dietary, nondi­
etary, or urinary. These risk factors vary by stone type and clinical 
characteristics.
Dietary Risk Factors 
Patients who develop stones often change 
their diet; therefore, studies that retrospectively assess diet may be 
hampered by recall bias. Some studies have examined the relation 
between diet and changes in the lithogenic composition of the urine, 
often using calculated supersaturation. However, the composition of 
the urine does not perfectly predict risk, and not all components that 
modify risk are included in the calculation of supersaturation. Thus, 
dietary associations are best investigated by prospective studies that 
examine actual stone formation as the outcome. Dietary factors that 
are associated with an increased risk of nephrolithiasis include animal 
protein, oxalate, sodium, sucrose, and fructose. Dietary factors associ­
ated with a lower risk include calcium, potassium, phytate, and higher 
fluid intake.
CALCIUM  The role of dietary calcium deserves special attention. 
Although in the distant past dietary calcium had been suspected of 
increasing the risk of stone disease, several prospective observational 
studies and a randomized controlled trial have demonstrated that 
higher dietary calcium intake is related to a lower risk of stone forma­
tion. The reduction in risk associated with higher calcium intake may 
be due to a reduction in intestinal absorption of dietary oxalate that 
results in lower urine oxalate. Low calcium intake is contraindicated 
as it increases the risk of stone formation and may contribute to lower 
bone density in stone formers.
Despite similar bioavailability, supplemental calcium may increase 
the risk of stone formation. The discrepancy between the risks from 
dietary calcium and calcium supplements may be due to the timing of 
supplemental calcium intake or to higher total calcium consumption 
leading to higher urinary calcium excretion.
OXALATE  Urinary oxalate is derived from both endogenous produc­
tion and absorption of dietary oxalate. Owing to its low and often 
variable bioavailability, much of the oxalate in food may not be read­
ily absorbed. However, absorption may be higher in stone formers. 
Although observational studies demonstrate that dietary oxalate is only 
a weak risk factor for stone formation, urinary oxalate is a strong risk 
factor for calcium oxalate stone formation, and efforts to avoid high 
oxalate intake should thus be beneficial.
OTHER NUTRIENTS  Several other nutrients have been studied and 
implicated in stone formation. Higher intake of animal protein may 
lead to increased excretion of calcium and uric acid as well as to 
decreased urinary excretion of citrate, all of which increase the risk of 
stone formation. Higher sodium and sucrose intake increases calcium 
excretion independent of calcium intake. Higher potassium intake 
decreases calcium excretion, and many potassium-rich foods increase 
urinary citrate excretion due to their alkali content. Other dietary 
factors that have been inconsistently associated with lower stone risk 
include magnesium and phytate.
Vitamin C supplements are associated with an increased risk of 
calcium oxalate stone formation in men, possibly owing to raised levels 
of oxalate in urine. Thus, male calcium oxalate stone formers should 

be advised to avoid high-dose vitamin C supplements. Although high 
doses of supplemental vitamin B6 may be beneficial in selected patients 
with type 1 primary hyperoxaluria, the risk is not reduced in other 
patients.

FLUIDS AND BEVERAGES  The risk of stone formation increases as 
urine volume decreases. When the urine output is <1 L/d, the risk of 
stone formation more than doubles. Fluid intake is the main determi­
nant of urine volume, and the importance of fluid intake in preventing 
stone formation has been demonstrated in observational studies and 
in a randomized controlled trial. Observational studies of individual 
beverages have found that coffee, tea, beer, wine, and orange juice are 
associated with a reduced risk of stone formation. Sugar-sweetened 
beverage consumption may increase risk.
Nondietary Risk Factors 
Age, race, body size, and environment 
are important risk factors for nephrolithiasis. The incidence of stone 
disease is highest in middle-aged white men, but stones can form in 
infants as well as in the elderly. There is geographic variability, with 
the highest prevalence in the southeastern United States. Weight gain 
increases the risk of stone formation, and the increasing prevalence of 
nephrolithiasis in the United States may be due in part to the increasing 
prevalence of obesity. Environmental and occupational influences that 
may lead to lower urine volume, such as working in a hot environment 
or lack of ready access to water or a bathroom, are important consid­
erations. Several observational studies, but not all, have reported that 
antibiotic use in early adulthood and middle age is associated with 
higher risk for nephrolithiasis in later life. The largest of these studies 
found an increased risk for five different classes of antibiotics.
CHAPTER 330
Nephrolithiasis
Urinary Risk Factors 
URINE VOLUME  Lower urine volume results in higher concentrations 
of lithogenic factors and is a common and readily modifiable risk fac­
tor. A randomized trial has demonstrated the effectiveness of higher 
fluid intake in increasing urine volume and reducing the risk of stone 
recurrence.
URINE CALCIUM  Higher urine calcium excretion increases the likeli­
hood of formation of calcium oxalate and calcium phosphate stones. 
While the term hypercalciuria is often used, there is no cutoff that 
distinguishes between normal and abnormal urine calcium excretion. 
In fact, the relation between urine calcium and stone risk appears to be 
continuous; thus, the use of an arbitrary threshold should be avoided. 
Levels of urine calcium excretion are higher in individuals with a 
history of nephrolithiasis; however, the mechanisms remain poorly 
understood. Greater gastrointestinal calcium absorption is one impor­
tant contributor, and greater bone turnover (with a resultant reduction 
in bone mineral density) may be another. Primary renal calcium loss, 
with lower serum calcium concentrations and elevated serum levels 
of parathyroid hormone (PTH) (and a normal 25-hydroxy vitamin D 
level), is rare.
URINE OXALATE  Higher urine oxalate excretion increases the likeli­
hood of calcium oxalate stone formation. As for urine calcium, no 
definition for “abnormal” urine oxalate excretion is widely accepted. 
Given that the relation between urine oxalate and stone risk is continu­
ous, simple dichotomization of urine oxalate excretion is not helpful 
in assessing risk. The two sources of urine oxalate are endogenous 
generation and dietary intake. Dietary oxalate is the major contribu­
tor and also the source that can be modified. Notably, higher dietary 
calcium intake reduces gastrointestinal oxalate absorption and thereby 
reduces urine oxalate.
URINE CITRATE  Urine citrate is a natural inhibitor of calcium-containing 
stones; thus, lower urine citrate excretion increases the risk of stone 
formation. Citrate reabsorption is influenced by the intracellular pH of 
proximal tubular cells. Metabolic acidosis, including that due to higher 
animal flesh intake, will lead to a reduction in citrate excretion by 
increasing reabsorption of filtered citrate. However, a notable propor­
tion of patients have lower urine citrate for reasons that remain unclear.

URINE URIC ACID  Higher urine levels of uric acid—a risk factor for 
uric acid stone formation—are found in individuals with excess purine 
consumption and rare genetic conditions that lead to overproduction 
of uric acid. This characteristic is not associated with the risk of cal­
cium oxalate stone formation.

URINE pH  Urine pH influences the solubility of some crystal types. 
Uric acid stones form when the urine pH is consistently ≤5.5, whereas 
calcium phosphate stones are more likely to form when the urine pH 
is ≥6.5. Cystine is more soluble at higher urine pH. Calcium oxalate 
stones are not influenced by urine pH.
Genetic Risk Factors 
The risk of nephrolithiasis is more 
than twofold greater in individuals with a family history of stone 
disease. This association is likely due to a combination of genetic 
predisposition and similar environmental exposures. While a number 
of rare monogenic disorders cause nephrolithiasis, genome-wide asso­
ciation studies have begun to reveal genetic contributors to common 
forms of stone disease.
The two most common and well-characterized rare monogenic 
disorders that lead to stone formation are primary hyperoxaluria and 
cystinuria. Primary hyperoxaluria is an autosomal recessive disorder 
that causes excessive endogenous oxalate generation by the liver, with 
consequent calcium oxalate stone formation and crystal deposition in 
organs. Intraparenchymal calcium oxalate deposition in the kidney can 
eventually lead to renal failure. Cystinuria is an autosomal recessive dis­
order that causes abnormal reabsorption of filtered basic amino acids. 
The excessive urinary excretion of cystine, which is poorly soluble, 
leads to cystine stone formation. Cystine stones are visible on plain 
radiographs and often manifest as staghorn calculi or multiple bilateral 
stones. Repeat episodes of obstruction and instrumentation can cause 
a reduction in the glomerular filtration rate (GFR).
PART 9
Disorders of the Kidney and Urinary Tract
APPROACH TO THE PATIENT
Nephrolithiasis
Evidence-based guidelines for the evaluation and treatment of 
nephrolithiasis have been published. Although there is limited evi­
dence for several aspects, there are standard approaches to patients 
with acute and chronic presentations that can reasonably guide the 
clinical evaluation.
It typically requires weeks to months (and often much longer) 
for a kidney stone to grow to a clinically detectable size. Although 
the passage of a stone is a dramatic event, stone formation and 
growth are characteristically clinically silent. A stone can remain 
asymptomatic in the kidney for years or even decades before signs 
(e.g., hematuria) or symptoms (e.g., pain) become apparent. Thus, 
it is important to remember that the onset of symptoms, typically 
attributable to a stone moving into the ureter, does not provide 
insight into when the stone actually formed. The factors that induce 
stone movement are unknown. 
CLINICAL PRESENTATION AND DIFFERENTIAL DIAGNOSIS
There are two common presentations for individuals with an acute 
stone event: renal colic and painless gross hematuria. Renal colic 
is a misnomer because pain typically does not subside completely; 
rather, it varies in intensity. When a stone moves into the ureter, 
the discomfort often begins with a sudden onset of unilateral flank 
pain.
The intensity of the pain can increase rapidly, and there are no 
alleviating factors. This pain, which is accompanied often by nau­
sea and occasionally by vomiting, may radiate, depending on the 
location of the stone. If the stone lodges in the upper part of the 
ureter, pain may radiate anteriorly; if the stone is in the lower part 
of the ureter, pain can radiate to the ipsilateral testicle in men or 
the ipsilateral labium in women. Occasionally, a patient has gross 
hematuria without pain.
Other diagnoses may be confused with acute renal colic. If the 
stone is lodged at the right ureteropelvic junction, symptoms may 

mimic those of acute cholecystitis. If the stone blocks the ureter 
as it crosses over the right pelvic brim, symptoms may mimic 
acute appendicitis, whereas blockage at the left pelvic brim may be 
confused with acute diverticulitis. If the stone lodges in the ureter 
at the ureterovesical junction, the patient may experience urinary 
urgency and frequency. In female patients, the latter symptoms 
may lead to an incorrect diagnosis of bacterial cystitis; the urine 
will contain red and white blood cells, but the urine culture will be 
negative. An obstructing stone with proximal infection may present 
as acute pyelonephritis. A UTI in the setting of ureteral obstruc­
tion is a medical emergency that requires immediate restoration of 
drainage by placement of either a ureteral stent or a percutaneous 
nephrostomy tube. Other conditions to consider in the differential 
diagnosis include muscular or skeletal pain, herpes zoster, duodenal 
ulcer, abdominal aortic aneurysm, gynecologic conditions, ureteral 
stricture, and ureteral obstruction by materials other than a stone, 
such as a blood clot or sloughed papilla. Extraluminal processes 
can lead to ureteral compression and obstruction; however, because 
of the gradual onset, these conditions do not typically present with 
renal colic. 
DIAGNOSIS AND INTERVENTION
Serum chemistry findings are typically normal, but the white blood 
cell count may be elevated. Examination of the urine sediment will 
usually reveal red and white blood cells and occasionally crystals 
(Fig. 330-1). The absence of hematuria does not exclude a stone, 
particularly when urine flow is completely obstructed by a stone.
The diagnosis is often made on the basis of the history, physical 
examination, and urinalysis. Thus, it may not be necessary to wait 
for radiographic confirmation before treating the symptoms. The 
diagnosis is confirmed by an appropriate imaging study—preferably 
noncontrast helical computed tomography (CT), which is highly 
sensitive and allows visualization of uric acid stones (traditionally 
considered “radiolucent”) (Fig. 330-2). Helical CT detects stones 
as small as 1 mm that may be missed by other imaging modalities.
Typically, helical CT reveals a ureteral stone or evidence of recent 
passage (e.g., perinephric stranding or hydronephrosis), whereas 
a plain abdominal radiograph (kidney/ureter/bladder [KUB]) can 
miss a stone in the ureter or kidney, even if it is radiopaque, and 
does not provide information on obstruction. Abdominal ultra­
sound offers the advantage of avoiding radiation and provides 
information on hydronephrosis, but it is not as sensitive as CT and 
images only the kidney and possibly the proximal segment of the 
ureter; thus, most ureteral stones are not detectable by ultrasound.
Many patients who experience their first episode of colic seek 
emergent medical care. Randomized trials have demonstrated that 
parenterally administered nonsteroidal anti-inflammatory drugs 
(e.g., ketorolac) are just as effective as opioids in relieving symptoms 
and have fewer side effects. Excessive fluid administration has not 
been shown to be beneficial; therefore, the goal should be to main­
tain euvolemia. If the pain can be adequately controlled and the 
patient is able to take fluids orally, hospitalization can be avoided. 
Use of an alpha blocker may increase the rate of spontaneous stone 
passage.
Urologic intervention should be postponed unless there is evi­
dence of UTI, a low probability of spontaneous stone passage (e.g., 
a stone measuring ≥6 mm or an anatomic abnormality), or intrac­
table pain. A ureteral stent may be placed cystoscopically, but this 
procedure typically requires general anesthesia, and the stent can be 
quite uncomfortable, may cause gross hematuria, and may increase 
the risk of UTI.
If an intervention is indicated, the selection of the most appropri­
ate intervention is determined by the size, location, and composi­
tion of the stone; the urinary tract anatomy; and the experience 
of the urologist. Extracorporeal shockwave lithotripsy (ESWL), 
the least invasive option, uses shockwaves generated outside the 
body to fragment the stone, but is being used less frequently. An 
endourologic approach, now more frequently used than ESWL,

FIGURE 330-1  Urine sediment from a patient with calcium oxalate stones (left) and a patient with cystine stones (right). Calcium oxalate dihydrate crystals are bipyramidally 
shaped, and cystine crystals are hexagonal. (Left panel image courtesy of Dr. Mark Perazella, Yale School of Medicine. Right panel image courtesy Dr. John Lieske, Mayo 
Clinic.)
can remove a stone by basket extraction or laser fragmentation. For 
large upper-tract stones, percutaneous nephrostolithotomy has the 
highest likelihood of rendering the patient stone-free. Advances 
in urologic approaches and instruments have nearly eliminated 
the need for open surgical procedures such as ureterolithotomy or 
pyelolithotomy. 
EVALUATION FOR STONE PREVENTION
More than half of first-time stone formers will have a recurrence 
within 10 years. A careful evaluation is indicated to identify pre­
disposing factors, which can then be modified to reduce the risk 
of new stone formation or growth of existing renal stones. It is 
appropriate to proceed with an evaluation even after the first stone 
if the patient is interested because recurrences are common and 
are usually preventable with inexpensive lifestyle modifications or 
other treatments. 
HISTORY
A detailed history, obtained from the patient and from a thor­
ough review of medical records, should include the number and 
FIGURE 330-2  Coronal noncontrast CT image from a patient who presented with 
left-sided renal colic. An obstructing calculus, present in the distal left ureter 
at the level of S1, measures 10 mm in maximal dimension. There is severe left 
hydroureteronephrosis and associated left perinephric fat stranding. In addition, 
there is a nonobstructing 6-mm left renal calculus in the interpolar region. (Image 
courtesy of Dr. Stuart Silverman, Brigham and Women’s Hospital.)

CHAPTER 330
frequency of episodes (distinguishing stone passage from stone for­
mation) and previous imaging studies, interventions, evaluations, 
and treatments. Inquiries about the patient’s medical history should 
cover UTIs, gastric bypass surgery and other malabsorptive condi­
tions, gout, hypertension, and diabetes mellitus. A family history of 
stone disease may reveal a genetic predisposition. A complete list 
of current prescription and over-the-counter medications as well as 
vitamin and mineral supplements is essential. The review of systems 
should focus on identifying possible etiologic factors related to 
low urine volume (e.g., high insensible losses) and gastrointestinal 
malabsorption as well as on ascertaining how frequently the patient 
voids during the day and overnight.
Nephrolithiasis
A large body of compelling evidence has demonstrated the 
important role of diet in stone disease. Thus, the dietary history 
should encompass information on usual dietary habits (meals and 
snacks), calcium intake, consumption of high-oxalate foods (spin­
ach, rhubarb, potatoes), and fluid intake (including amount of spe­
cific beverages typically consumed). Amount and frequency of use 
of vitamin and mineral supplements should be carefully assessed. 
PHYSICAL EXAMINATION
The physical examination should assess weight, blood pressure, 
costovertebral angle tenderness, and lower-extremity edema as well 
as signs of other systemic conditions such as primary hyperpara­
thyroidism and gout. 
LABORATORY EVALUATION
If not recently measured, the following serum levels should be 
determined: electrolytes (to uncover hypokalemia or renal tubular 
acidosis), creatinine, calcium, phosphorus, and uric acid. The PTH 
level should be measured if indicated by elevated, high-normal, or 
low-normal serum and urine calcium concentrations. 25-Hydroxy 
vitamin D should be measured in concert with PTH to investigate 
the possible role of secondarily elevated PTH levels in the setting of 
vitamin D insufficiency.
The urinalysis, including examination of the sediment, can pro­
vide useful information. In individuals with asymptomatic residual 
renal stones, red and white blood cells are frequently present in 
urine. If there is concern about the possibility of an infection, a 
urine culture should be performed. The sediment may also reveal 
crystals (Fig. 330-1), which may help identify the stone type and 
also provide prognostic information as crystalluria is a strong risk 
factor for new stone formation.
The results from 24-h urine collections serve as the cornerstone 
on which therapeutic recommendations are based. Recommen­
dations on lifestyle modification should be deferred until urine

collection is complete. As a baseline assessment, patients should 
collect at least two 24-h urine samples while consuming their usual 
diet and usual volume of fluid. The following factors should be 
measured: total volume, calcium, oxalate, citrate, uric acid, sodium, 
potassium, phosphorus, magnesium, pH, and creatinine. When 
available, the calculated supersaturation is also informative. There 
is substantial day-to-day variability in the 24-h excretion of many 
relevant factors; therefore, obtaining values from two collections 
is important before committing a patient to long-term lifestyle 
changes or medication. The interpretation of the 24-h urine results 
should take into account that the collections are usually performed 
on a weekend day when the patient is staying at home; an individ­
ual’s habits may differ dramatically (beneficially or detrimentally) 
at work or outside the home. Specialized testing, such as calcium 
loading or restriction, is not recommended as it does not influence 
clinical recommendations.
Stone composition analysis is essential if a stone or fragment is 
available; patients should be encouraged to retrieve passed stones. 
The stone type cannot be determined with certainty from 24-h 
urine results, but pure uric acid stones can be identified by low 
Hounsfield units on CT. 
IMAGING
The “gold standard” diagnostic test is helical CT without contrast. 
If not already performed during an acute episode, a low-dose 
renal-limited noncontrast CT should be considered to establish 
definitively the baseline stone burden. A suboptimal imaging study 
may not detect a residual stone that, if subsequently passed, would 
be mistaken for a new stone. In this instance, the preventive medical 
regimen might be unnecessarily changed as the result of a preexist­
ing stone.
PART 9
Disorders of the Kidney and Urinary Tract
Recommendations for follow-up imaging should be tailored to 
the individual patient. While CT provides the best information, 
the radiation dose is higher than from other modalities; therefore, 
CT should be performed only if the results will lead to a change in 
clinical recommendations. Although less sensitive, renal ultrasound 
is typically used to minimize radiation exposure, with recognition 
of the limitations. 
PREVENTION OF NEW STONE FORMATION
Recommendations for preventing stone formation depend on the 
stone type and the results of metabolic evaluation. After remediable 
secondary causes of stone formation (e.g., primary hyperparathy­
roidism) are excluded, the focus should turn to modification of the 
urine composition to reduce the risk of new stone formation. The 
urinary constituents and calculated urine supersaturation are con­
tinuous variables, and the associated risk is continuous; thus, there 
are no definitive thresholds. Dichotomization into “normal” and 
“abnormal” can be misleading and should be avoided.
For all stone types, consistently diluted urine reduces the likeli­
hood of crystal formation. The urine volume should be at least 
2 L/d. Because of differences in insensible fluid losses and fluid 
intake from food sources, the required total fluid intake will vary 
from person to person. Rather than specify how much to drink, it 
is more helpful to educate patients about how much more they need 
to drink in light of their 24-h urine volume. For example, if the daily 
urine volume is 1.5 L, then the patient should be advised to drink 
consistently at least 0.5 L more per day in order to increase the urine 
volume to the goal of 2 L/d.
■
■RECOMMENDATIONS FOR SPECIFIC 

STONE TYPES
Calcium Oxalate 
Risk factors for calcium oxalate stones include 
higher urine calcium, higher urine oxalate, and lower urine citrate. 
This stone type is insensitive to urine pH in the physiologic range.
Individuals with higher urine calcium excretion tend to absorb a 
higher percentage of ingested calcium. Nevertheless, dietary calcium 
restriction is not beneficial and, in fact, is likely to be harmful (see 

“Dietary Risk Factors,” above). In a randomized trial in men with high 
urine calcium and recurrent calcium oxalate stones, a diet containing 
1200 mg of calcium and a low intake of sodium and animal protein 
significantly reduced subsequent stone formation compared with a 
low-calcium diet (400 mg/d). Excessive calcium intake (>1200 mg/d) 
should be avoided.
A thiazide diuretic, in doses higher than those used to treat hyper­
tension, can substantially lower urine calcium excretion. Several ran­
domized controlled trials, but not all, have demonstrated that thiazide 
diuretics can reduce calcium oxalate stone recurrence by ~50%. When 
a thiazide is prescribed, dietary sodium restriction is essential to obtain 
the desired reduction in urinary calcium excretion and minimize uri­
nary potassium losses. While bisphosphonates may reduce urine cal­
cium excretion in some individuals, there are only observational data 
to suggest whether this class of medication can reduce stone formation; 
therefore, bisphosphonates cannot be recommended solely for stone 
prevention at present, but they can be used to treat those individuals 
with low bone density.
A reduction in urine oxalate will, in turn, reduce the supersaturation 
of calcium oxalate. In patients with the common form of nephroli­
thiasis, avoiding high-dose vitamin C supplements is the only known 
strategy that reduces endogenous oxalate production. In patients with 
primary hyperoxaluria (type I), an siRNA-based therapy (lumasiran, 
nedosiran) can reduce oxalate generation in the liver.
Oxalate is a metabolic end product; therefore, any dietary oxalate 
that is absorbed will be excreted in the urine. Reducing absorption of 
exogenous oxalate involves two approaches. First, the avoidance of foods 
that contain high amounts of oxalate, such as spinach, rhubarb, almonds, 
and potatoes, is prudent. However, extreme oxalate restriction has not 
been demonstrated to reduce stone recurrence and could be harmful 
to overall health, given other health benefits of many foods that are 
erroneously considered to be high in oxalate. Second, the absorption of 
oxalate is reduced by higher calcium intake; therefore, individuals with 
higher-than-desired urinary oxalate should be counseled to consume 
adequate calcium. Oxalate absorption can be influenced by the intestinal 
microbiota, depending on the presence of oxalate-degrading bacteria. 
Currently, however, there are no available therapies to alter the micro­
biota that beneficially affect urinary oxalate excretion over the long term.
Citrate is a natural inhibitor of calcium oxalate and calcium phos­
phate stones. Increased consumption of foods rich in alkali (i.e., fruits 
and vegetables) can increase urine citrate. For patients with lower urine 
citrate in whom dietary modification does not adequately increase 
urine citrate, the addition of supplemental alkali (typically potassium 
citrate or bicarbonate) will lead to an increase in urinary citrate excre­
tion. Sodium salts, such as sodium bicarbonate, while successful in 
raising urine citrate, are typically avoided due to the adverse effects of 
sodium on urine calcium excretion.
Past reports suggested that higher levels of urine uric acid may 
increase the risk of calcium oxalate stones, but more recent studies 
do not support this association. However, allopurinol reduced stone 
recurrence in one randomized controlled trial in patients with calcium 
oxalate stones and high urine uric acid levels. The lack of association 
between urine uric acid level and calcium oxalate stones suggests that 
a different mechanism underlies the observed beneficial effect of allo­
purinol in this setting.
Additional dietary modifications may be beneficial in reducing 
stone recurrence. Restriction of nondairy animal protein (e.g., meat, 
chicken, seafood) is a reasonable approach and may result in higher 
excretion of citrate and lower excretion of calcium. In addition, reduc­
ing sodium intake to <2.5 g/d may decrease urinary excretion of cal­
cium. Sucrose and fructose intake should be minimized.
For adherence to a dietary pattern that is more manageable for 
patients than manipulating individual nutrients, the Mediterranean 
diet or the DASH (Dietary Approaches to Stop Hypertension) diet 
provides an appropriate and readily available option. Randomized tri­
als have conclusively shown the DASH diet to reduce blood pressure. 
At present, only data from observational studies are available, but these 
demonstrate a strong and consistent inverse association between these 
healthy dietary patterns and risk of stone formation.