Medical Journals

Do Anatomic Factors Pose a Significant Risk in the Formation of Lower Pole Stones?

Authors:
  • Manikandan Ramaswamy
  • Gall Zara
  • Gunendran Thiruendran
  • Neilson Donald
  • Adeyoju Adebanji

From: Department of Urology, Stepping Hill Hospital, Stockport, Cheshire, United Kingdom. armanikan2000@gmail.com

Urology

  • Publish Date: Apr 2007
  • ISSN: 1527-9995
  • Volume: 69
  • Issue: 4
  • Pages: 620-4
  • Medium: Internet
  • Language: English
  • Citation (JAMA): Manikandan Ramaswamy, Gall Zara, Gunendran Thiruendran, et al. Do Anatomic Factors Pose a Significant Risk in the Formation of Lower Pole Stones?. Urology Apr 2007;69:620-4

Abstract

OBJECTIVES: To determine whether various anatomic factors predispose to a lower pole stone on one side compared with the other. METHODS: We analyzed the intravenous urography pictures of 40 consecutive patients presenting with a single lower pole stone. Measurements were taken of the infundibulopelvic angle (IPA), ureteroinfundibular angle, infundibular width, pelvicaliceal height, infundibular length, and pelvicaliceal angle of the affected and normal kidney. The IPA was measured according to the methods of Sampaio, Bagley, and Elbahnasy. A comparison was made to determine whether any of these measurements predisposed one side to form stones. RESULTS: The mean age was 47 years (range 20 to 80). The mean stone size was 9.2 mm (range 5 to 20). The mean IPA was 94.82 degrees (Sampaio), 56.17 degrees (Bagley), 60.40 degrees (Elbahnasy), and 49.15 degrees (Sampaio) on the affected kidney and 95.97 degrees (P = 0.66), 57.47 degrees (P = 0.57), 65.9 degrees (P = 0.04), and 54 degrees (P = 0.07) on the normal side. A statistically significant difference was found only when we measured the IPA as described by Elbahnasy. The mean infundibular width was 4.4 mm on both sides (P = 0.99). The caliceopelvic height was 21.6 mm on the affected side and 22.6 mm on the normal side (P = 0.30). The infundibular length was 28.6 mm and 27.4 mm (P = 0.16) and the caliceopelvic angle was 48 degrees and 47.6 degrees (P = 0.8) on the affected and normal kidneys, respectively CONCLUSIONS: Lower pole anatomy as a risk factor for stones depends on the type of measurement used. A consensus should be reached to define how exactly the IPA should be measured. Other anatomic factors were not significantly different between the affected and normal side in our study.

Mesh Headings (Keywords): Adult, Aged, Aged, 80 and over, Humans, Kidney, Kidney Calculi, Middle Aged, Retrospective Studies, Risk Factors


Check for Full Text / PubMed Unique Identifier (PMID): 17445636


This abstract is part of PubMed, a service of the U.S. National Library of Medicine. PubMed includes more than 17 million citations from MEDLINE and other life science journals for biomedical articles. See Copyright and Disclaimers.

Linked medical terms appearing on this page are added by Healia to help readers find more information and are not part of the original PubMed document.

The data herein was last updated on July 8th, 2008 and may not reflect the most current and accurate data available from NLM.


Advertisements

About | Privacy Policy | Business Solutions | Advertise | Contact | Add Healia to your site

©2012. Healia / Meredith Corporation  

Use of this site constitutes acceptance of our Terms of Service and Privacy Policy. All content on this Web site, including medical opinion and any other health-related information, is for informational purposes only and should not be used for a specific diagnosis or individual treatment plan for any situation. Use of this site and the information contained herein does not create a doctor-patient relationship. Always seek the direct advice of your doctor in connection with any questions or issues you may have regarding your own health or the health of others.