Canine and Feline Urolithiasis Updates and Challenges India F
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Precipitation of Phosphate Minerals from Effluent of Anaerobically Digested Swine Manure Alex Y
University of South Florida Scholar Commons Graduate Theses and Dissertations Graduate School January 2012 Precipitation of Phosphate Minerals from Effluent of Anaerobically Digested Swine Manure Alex Y. Lin University of South Florida, [email protected] Follow this and additional works at: http://scholarcommons.usf.edu/etd Part of the Chemical Engineering Commons, Environmental Engineering Commons, and the Environmental Sciences Commons Scholar Commons Citation Lin, Alex Y., "Precipitation of Phosphate Minerals from Effluent of Anaerobically Digested Swine Manure" (2012). Graduate Theses and Dissertations. http://scholarcommons.usf.edu/etd/4359 This Thesis is brought to you for free and open access by the Graduate School at Scholar Commons. It has been accepted for inclusion in Graduate Theses and Dissertations by an authorized administrator of Scholar Commons. For more information, please contact [email protected]. Precipitation of Phosphate Minerals from Effluent of Anaerobically Digested Swine Manure by Alex Yuan-li Lin A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science Department of Civil and Environmental Engineering College of Engineering University of South Florida Co-Major Professor: Sarina Ergas, Ph.D. Co-Major Professor: Jeffrey Cunningham, Ph.D. Maya Trotz, Ph.D. Date of Approval: November 9, 2012 Keywords: struvite, wastewater, confined animal feeding operation (CAFO), fertilizer, synthetic Copyright © 2012, Alex Yuan-li Lin DEDICATION I dedicate this thesis to all those that have supported me along the way whether directly or indirectly. I would like to thank members of Intervarsity on the USF campus, members of Community Life Church, and my family for their support and encouragement in many ways. -
DESCRIPTIVE HUMAN PATHOLOGICAL MINERALOGY 1179 but Still Occursregularly
Amerkan Mincraloght, Volume 59, pages I177-1182, 1974 DescriptiveHuman Pathological Mineralogy Rrcneno I. Gmsox P.O. Box I O79, Dauis,C alilornia 95 6 I 6 Absfract Crystallographic, petrographic, and X-ray powder difiraction analysis of approximately 15,000 samples showed that the most common mineral constituents of human pathological concretions are calcium oxalates (whewellite and weddellite), calcium phosphates (apatite, brushite, and whitlockite), and magnesium phosphates (struvite and newberyite). Less are monetite, hannayite, calcite, aragonite, vaterite, halite, gypsum, and hexahydrite."o-rnon of the variables determining which minerals precipitate, the effects of different pH values on deposi- tional conditions are most apparent, and are shown by occurrences and relationships among many of the minerals studied. A pH-sensitive series has been identified among magnesium phosphatesin concretions. Introduction The study was carried out over a period of three The importanceof mineralogyin the field of medi- years.Composition was confirmedby X-ray powder cine lies in the applicationof mineralogicalmethods diffraction and polarizing microscopy;sequence was to study pathologicalmineral depositsin the human arrived at from considerationsof microscopic tex- body. Urology benefitsgreatly becauseconcretions tural and crystallographicrelationships. More than of mineral matter (calculi) are common in the 14,500samples were derivedfrom the urinary sys- urinary system.The value of mineralogicalanalysis tem of kidneys,ureters, bladder, and urethra; the of urinary material was first describedby prien and remaining samples are not statistically significant Frondel (1947). Mineralogistsmay be unawareof and arediscussed only briefly. the variability and nature of such compounds be- Calcium cause reports are usually published in medical Oxalates journals. This investigationreports the mineralogy Whewellite, CaCzOE.H2O,and weddellite, CaCz- and possiblepathological significanceof these min- O4'2H2O,are very uncommonin the mineralworld. -
Portosystemic Shunts
Portosystemic Shunts ABOUT THE DIAGNOSIS Radiographic techniques using special dyes administered during Portosystemic shunts are defects of the blood’s circulation through surgery are needed to locate the portosystemic shunts in other the liver. They cause symptoms of poor growth and neurologic pets. dysfunction, and the best form of treatment for portosystemic LIVING WITH THE DIAGNOSIS shunts that have been present since birth (the majority) is usually via surgery. Successful surgical treatment of congenital portosystemic shunts Portosystemic shunts result from abnormal blood vessels that can lead to the pet living a normal life. Without surgery, some dogs connect the portal system of the liver with the veins of the rest of can be managed with medication alone for months to years, while the body. The portal system is a division of the blood circulation in others, the medication is not sufficient to control the problem. that collects blood from the intestines and carries it to the liver, Cats are less likely to have their symptoms controlled by medica- where toxins and nutrients are removed before it enters the general tion alone. circulation. Normally, intestinal bacteria produce toxic substances, When portosystemic shunts first arise later in life (acquired such as ammonia, that are absorbed into the blood and then portosystemic shunts), they do so as a result of chronic liver dis- detoxified in the liver. When this blood bypasses the liver through ease such as cirrhosis. In such cases, surgical closure of the a portosystemic shunt, these toxins that are normally removed by shunts is not performed, and the priority rests on treatment of the the liver are allowed to circulate in the bloodstream. -
Pre and Postnatal Diagnosis of Congenital Portosystemic Shunt: Impact of Interventional Therapy
International Journal of Pediatrics and Adolescent Medicine 7 (2020) 127e131 HOSTED BY Contents lists available at ScienceDirect International Journal of Pediatrics and Adolescent Medicine journal homepage: http://www.elsevier.com/locate/ijpam Original research article Pre and postnatal diagnosis of congenital portosystemic shunt: Impact of interventional therapy * Shireen Mreish a, , Mohamed A. Hamdan b a Pediatrics, Tawam Hospital, Affiliated with Johns Hopkins, Al Ain, United Arab Emirates b Pediatric Cardiology, KidsHeart Medical Center, Dubai, United Arab Emirates article info abstract Article history: Introduction: Congenital portosystemic shunts (CPSS) are rare vascular malformations that can lead to Received 25 November 2018 severe complications. With advanced imaging techniques, diagnosis is becoming more feasible occurring Accepted 25 February 2019 in fetal life. Different approaches have been adopted to manage these cases, with an increased utilization Available online 15 March 2019 of interventional therapy recently. This cohort aims to describe the course of children diagnosed with CPSS and the impact of interventional therapy on the outcome. Methods: Retrospective chart review was done for all patients who were diagnosed with CPSS in our institution between January 2006 and December 2015. Results: Six patients were diagnosed with CPSS. During this period, 8,680 mothers carrying 9548 fetuses underwent fetal ultrasound examinations. Three patients were diagnosed antenatally at a median [IQ] gestational age of 33 [26e33] weeks, and three patients were diagnosed postnatally at 0, 2, and 43 months, respectively. At a median follow-up of 87 [74e110] months, 5 patients are alive; 4 of whom had received transcatheter closure for different indications, and one who had spontaneous resolution of her CPSS. -
1 Raman Spectroscopy of Newberyite, Hannayite and Struvite. Ray L. Frost
Raman spectroscopy of newberyite, hannayite and struvite. Ray L. Frost• a, Matt L. Weier a, Wayde N. Martens, a Dermot A. Henry b, and Stuart J. Mills b,c a Inorganic Materials Research Program, School of Physical and Chemical Sciences, Queensland University of Technology, GPO Box 2434, Brisbane Queensland 4001, Australia. b Geosciences, Museum Victoria, PO Box 666E, Melbourne, Victoria 3001, Australia. c CSIRO Minerals, Box 312, Clayton South, Victoria 3169, Australia. This is the authors’ version of a paper that was later published as: Frost, Ray, Weier, Matt , Martens, Wayde, Henry, Dermot & Mills, Stuart (2005) Raman spectroscopy of newberyite, hannayite and struvite. Spectrochimica Acta 62(1):pp. 181-188. Copyright 2005 Elsevier Abstract The phosphate minerals hannayite, newberyite and struvite have been studied by Raman spectroscopy using a thermal stage. Hannayite and newberyite are -1 characterised by an intense band at around 980 cm assigned to the ν1 symmetric stretching vibration of the HPO4 units. In contrast the symmetric stretching mode is -1 observed at 942 cm for struvite. The Raman spectra are characterised by multiple ν3 antisymmetric stretching bands and ν2 and ν4 bending modes indicating strong distortion of the HPO4 and PO4 units. Hannayite and newberyite are defined by bands -1 at 3382 and 3350 cm attributed to HOPO3 vibrations and hannayite and struvite by + bands at 2990, 2973 and 2874 assigned to NH4 bands. Raman spectroscopy has proven most useful for the analysis of these ‘cave’ minerals where complex paragenetic relationships exist between the minerals. Keywords: hannayite, newberryite, struvite, phosphate, Raman spectroscopy Introduction Interest in struvite formation also comes from the formation in urinary tracts and kidneys [1-6]. -
Portosystemic Shunts in Dogs
Portosystemic Shunts in Dogs 803-808-7387 www.gracepets.com What is a liver shunt? The portal vein is a large vein that collects blood from the systemic circulation and carries it into the liver, where toxins and other byproducts are removed. A liver shunt occurs when an abnormal connection persists or forms between the portal vein or one of its branches, and another vein, allowing blood to bypass or shunt around the liver. In the majority of cases, a liver shunt is caused by a birth defect called a congenital portosystemic shunt. In some cases, multiple small shunts form because of severe liver disease such as cirrhosis. These are referred to as acquired portosystemic shunts. How does a congenital portosystemic shunt develop? All mammalian fetuses have a large shunt (ductus venosus) that carries blood quickly through the fetal liver to the heart. A congenital portosystemic shunt develops if: 1. The ductus venosus fails to collapse at birth and remains intact and open after the fetus no longer needs it. 2. A blood vessel outside the liver develops abnormally and remains open after the ductus venosus closes. What are the clinical signs of a liver shunt? The most common clinical signs include “stunted” growth, poor muscle development, abnormal behaviors such as disorientation, staring into space, circling or head pressing, and seizures. Less common symptoms include drinking or urinating too much, vomiting and diarrhea. Pets may be diagnosed when they take a long time recovering from anesthesia or if clinical signs occur after eating high protein meals. Some pets do not show signs until they are older, when they develop urinary problems such as recurrent kidney or bladder infections or stones. -
Bladder Stones in Dogs & Cats By: Dr
Navarro Small Animal Clinic 5009 Country Club Dr. Victoria, TX 77904 361-573-2491 www.navarrosmallanimalclinic.com Bladder Stones in Dogs & Cats By: Dr. Shana Bohac Dogs, like people, can develop a variety of bladder stones. These stones are rock-like structures that are formed by minerals. Some stones form in alkaline urine, whereas others form when the urine is more acidic. Bladder stones are very common in dogs, particularly small breed dogs. The most common signs that a dog or cat has bladder stones include blood in the urine, and straining to urinate. Blood is seen due to the stones bouncing around and hitting the bladder wall. This can irritate and damage the tissue and can cause cystitis (inflammation of the bladder). Straining to urinate occurs because of the inflammation and irritation of the bladder walls or urethra or muscle spasms. The stone itself can actually obstruct the flow of urine if it blocks the urethra. Small stones can get stuck in the urethra and cause a complete obstruction. This can be life threatening if the obstruction is not relieved since the bladder can rupture as more urine is produced with nowhere to go. Bladder stones form because of changes in the urine pH. Normal dog urine is slightly acidic and contains waste products such as dissolved minerals and enzymes such as urease. Urease breaks down excess ammonia in urine. An overload of ammonia in urine can cause bladder inflammation and thickening known as cystitis. There are a variety of stones that can form in the bladder, some that form in acidic urine, while others form in alkaline urine. -
Current Insights Into the Mechanisms and Management of Infection Stones
Current insights into the mechanisms and management of infection stones Authors: Erika J. Espinosa-Ortiz, Brian H. Eisner, Dirk Lange, and Robin Gerlach The final publication is available at Springer via https://dx.doi.org/10.1038/s41585-018-0120-z. Espinosa-Ortiz, Erika J., Brian H. Eisner, Dirk Lange, and Robin Gerlach, “Current insights into the mechanisms and management of infection stones,” Nature Reviews Urology, November 2018, 16: 35-53. doi: 10.1038/s41585-018-0120-z. Made available through Montana State University’s ScholarWorks scholarworks.montana.edu Current insights into the mechanisms and management of infection stones Erika J. Espinosa-Ortiz1,2, Brian H. Eisner3, Dirk Lange4* and Robin Gerlach 1,2* Abstract | Infection stones are complex aggregates of crystals amalgamated in an organic matrix that are strictly associated with urinary tract infections. The management of patients who form infection stones is challenging owing to the complexity of the calculi and high recurrence rates. The formation of infection stones is a multifactorial process that can be driven by urine chemistry , the urine microenvironment, the presence of modulator substances in urine, associations with bacteria, and the development of biofilms. Despite decades of investigation, the mechanisms of infection stone formation are still poorly understood. A mechanistic understanding of the formation and growth of infection stones — including the role of organics in the stone matrix, microorganisms, and biofilms in stone formation and their effect on stone characteristics — and the medical implications of these insights might be crucial for the development of improved treatments. Tools and approaches used in various disciplines (for example, engineering, chemistry , mineralogy , and microbiology) can be applied to further understand the microorganism–mineral interactions that lead to infection stone formation. -
Struvite Urolithiasis in Dogs
Glendale Animal Hospital 623-934-7243 www.familyvet.com Struvite Urolithiasis in Dogs (Struvite Stones in the Urinary Tract of Dogs) Basics OVERVIEW • ”Urolithiasis” is the medical term for the presence of stones (known as “uroliths”) in the urinary tract • The most common minerals found in the stones (uroliths) are used to name the particular stone; in this type of stone, struvite makes up the composition of the stone, and thus the name “struvite urolithiasis”; struvite is magnesium ammonium phosphate • The urinary tract consists of the kidneys, the ureters (the tubes running from the kidneys to the bladder), the urinary bladder (that collects urine and stores it until the pet urinates), and the urethra (the tube from the bladder to the outside, through which urine flows out of the body) • Struvite urolithiasis is the formation of crystalline stones (uroliths) composed of magnesium ammonium phosphate, or struvite, in the urinary tract GENETICS • The high incidence of struvite stones (uroliths) in some breeds of dogs (such as the miniature schnauzer) suggests a familial (runs in certain families or lines of animals) tendency; it is hypothesized that susceptible miniature schnauzers inherit some abnormality of local host defenses of the urinary tract that increases their likelihood to develop urinary tract infection (UTI) • Sterile struvite uroliths were found in a family of English cocker spaniels SIGNALMENT/DESCRIPTION OF PET Species • Dogs Breed Predilections • Miniature schnauzer, shih tzu, bichon frise, miniature poodle, cocker spaniel, -
Optical Properties of Common Rock-Forming Minerals
AppendixA __________ Optical Properties of Common Rock-Forming Minerals 325 Optical Properties of Common Rock-Forming Minerals J. B. Lyons, S. A. Morse, and R. E. Stoiber Distinguishing Characteristics Chemical XI. System and Indices Birefringence "Characteristically parallel, but Mineral Composition Best Cleavage Sign,2V and Relief and Color see Fig. 13-3. A. High Positive Relief Zircon ZrSiO. Tet. (+) 111=1.940 High biref. Small euhedral grains show (.055) parallel" extinction; may cause pleochroic haloes if enclosed in other minerals Sphene CaTiSiOs Mon. (110) (+) 30-50 13=1.895 High biref. Wedge-shaped grains; may (Titanite) to 1.935 (0.108-.135) show (110) cleavage or (100) Often or (221) parting; ZI\c=51 0; brownish in very high relief; r>v extreme. color CtJI\) 0) Gamet AsB2(SiO.la where Iso. High Grandite often Very pale pink commonest A = R2+ and B = RS + 1.7-1.9 weakly color; inclusions common. birefracting. Indices vary widely with composition. Crystals often euhedraL Uvarovite green, very rare. Staurolite H2FeAI.Si2O'2 Orth. (010) (+) 2V = 87 13=1.750 Low biref. Pleochroic colorless to golden (approximately) (.012) yellow; one good cleavage; twins cruciform or oblique; metamorphic. Olivine Series Mg2SiO. Orth. (+) 2V=85 13=1.651 High biref. Colorless (Fo) to yellow or pale to to (.035) brown (Fa); high relief. Fe2SiO. Orth. (-) 2V=47 13=1.865 High biref. Shagreen (mottled) surface; (.051) often cracked and altered to %II - serpentine. Poor (010) and (100) cleavages. Extinction par- ~ ~ alleL" l~4~ Tourmaline Na(Mg,Fe,Mn,Li,Alk Hex. (-) 111=1.636 Mod. biref. -
Transjugular Intrahepatic Portosystemic Stent-Shunt In
Guidelines Transjugular intrahepatic portosystemic stent-shunt in Gut: first published as 10.1136/gutjnl-2019-320221 on 29 February 2020. Downloaded from the management of portal hypertension Dhiraj Tripathi ,1,2,3 Adrian J Stanley ,4 Peter C Hayes ,5 Simon Travis,6 Matthew J Armstrong ,1,2,3 Emmanuel A Tsochatzis ,7 Ian A Rowe ,8 Nicholas Roslund,9 Hamish Ireland ,10 Mandy Lomax,11 Joanne A Leithead,12 Homoyon Mehrzad,13 Richard J Aspinall ,14 Joanne McDonagh,1 David Patch7 For numbered affiliations see ABSTRact ► In secondary prevention of oesophageal end of article. These guidelines on transjugular intrahepatic variceal bleeding, TIPSS can be considered portosystemic stent- shunt (TIPSS) in the management where patients rebleed despite combination of Correspondence to of portal hypertension have been commissioned by the VBL +NSBB taking into account the severity Dr Dhiraj Tripathi, Liver Unit, University Hospitals Birmingham Clinical Services and Standards Committee (CSSC) of of rebleeding and other complications of portal NHS Foundation Trust, the British Society of Gastroenterology (BSG) under the hypertension, with careful patient selection Birmingham B15 2TH, UK; auspices of the Liver Section of the BSG. The guidelines to minimise hepatic encephalopathy (weak d. tripathi@ bham. ac. uk are new and have been produced in collaboration with recommendation, moderate- quality evidence). Received 2 November 2019 the British Society of Interventional Radiology (BSIR) Further large controlled trials are required to Revised 20 January 2020 and British Association of the Study of the Liver (BASL). investigate the role of TIPSS as first- line therapy Accepted 22 January 2020 The guidelines development group comprises elected in secondary prevention (strong recommenda- members of the BSG Liver Section, representation tion, low quality of evidence). -
Tavistockite and Bialite Discredited
MINERALOGICAL MAGAZINE, MARCH 1969, VOL. 37, NO. 285 Tavistockite and bialite discredited P. G. EMBREY AND E. E. FEJER Department of Mineralogy, British Museum (Natural History) SUMMARY. Specimens of tavistockite fall into two groups: true tavistockite from the George and Charlotte mine, Tavistock, Devon, and wavellite from the Stenna Gwyn mine, St. Austell, Cornwall. Both were sold as tavistockite by the discoverer, Richard TaIling. Tavistockite proper is a fluorapatite, as shown by optical and X-ray examination, and the alumina and water in the original analysis are certainly derived from kaolinite with which the apatite is intimately associated. The published optical properties attributed to tavistockite were determined by E. S. Larsen on Stenna Gwyn material, and are those of wavellite. Re-examination of a portion of Buttgenbach's type bialite, which he related to tavistockite on optical grounds, shows it to be wavellite. TAVISTOCKITE has been a doubtful species from the time it was first described in 1865 by A. H. Church! as 'Hydrated Calcium-aluminic Phosphate (?)'. Its apparent validity has been established by successive appearances in all the standard works on systematic mineralogy, starting with J. D. Dana's renaming as tavistockite in 1868.2 The present study is perhaps as much historical as mineralogical, since Church's original material cannot be traced and other specimens present a confused picture both in naming and in locality. We have studied seventeen specimens (see table) that are or have at one time been labelled tavistockite, and find that they fall into two distinct groups that may readily be characterized by the mineral assemblages present.