AVENTURINE GLAZES BY JOHN SHERMAN LATHROP THESIS FOR THE DEGREE OF BACHELOR OF SCIENCE IN CERAMIC ENGINEERING COLLEGE OF ENGINEERING UNIVERSITY OF ILLINOIS 1922 •-Mil Digitized by the Internet Archive in 2015 https://archive.org/detaiis/aventurineglazesOOIath INDEX Page I Introduction . . • . o 1-5 II Work Conducted by Previous Experimenters 6-7 A, Work done by U.S. Bureau of Mines 6 B. Work done by Nathan Bromberg 6-2> III Scope of Present Investigation S IV Method of Investigation S-9 V Burning 9 VI Method of Preparing Glazes 10 VII Materials Used 11 VIII Trial Pieces 11 IX Effect of Variations in Al20^, FegO^. . . • 11-2S Ao First Series 11-20 B. Second Series 21=-24- C. Third Series 24-27 D. General Conclusions from First Part 27-28 X Effect of Variations in Na20, K 2 O, CaO and PbO . . . 2S-3^ A, Conclusions from Second Part 28-3^ XI General Conclusions drawn from Experiments on Aventurine Glazes 34-35 INDEX TO FIGURES Page Fig, I Time -temperature Curve for Aventurine glazes Maturing at Cone 1 l4a Fig. II Area of Investigations of Variable Con- stituents of the Aventurine Glazes of Part 1 12a Fig. Ill Chart showing location of all Glazes on Tri-axial chart together with Dia- gramatic Presentation of Results .... 12b Fig, IV Time-temperature Curve for Aventurine Glazes burned at cone 3 24a Fig, V,VI,VII,VIII,IX Presentation of the R 0 components of each glaze together with the location of each glaze on Tri-axial diagrams for glazes varying in the R 0 components 29a-29e STUDIES IN AVENTURINE GLAZES, I Introduction Of all the types of glaaes, probably the most beautiful and yet the most difficult to produce are the crystalline glazes. There has been very little technical research done on this subject and undoubtedly if more work were done on the subject and more in- formation were available, crystalline glaaes could be produced and controlled as easily as other glazes. The glaze composition, the heat treatment of the glaze, and the body composition, are factors which have to be studied for each particular glaze. There are two typos of crystalline glazes^;- The first type, the macro-crystalline glazes, includes the aventurine glaze, some- times called "goldstone" or "tiger eye". In this type the crystals separate out of the molten matrix on cooling of a size readily vis- ible to the maked eye. The second type, the micro-crystalline glazes, includes some of the mott glazes. In this type, the entire mass crystallizes. For developing aventurine glazes, Stull recom- mends applying metallic oxides to the body and covering this with a boric acid glaze. When the glaze fuses and becomes fluid, it takes part of the metallic oxide into solution and, if enough of it is dissolved, the glaze becomes supersaturated and crystals se- parate out on cooling, p Mellor^ has given a good explanation of the formation of cyrstalline glazes by comparing the molten matrix with ordinary ^ R, To Stull "Notes on the Production of Crystalline Glazes". Trans, Am. Cer, Soc, Vol. VII, 190^ p,lS 6 J , W. Mellor "Crystallization in Pottery". Trans. Eng, Cer. Soc. Vol. IV, 1902 p .52 '* '.-k,*.- .-‘ ; V’*-' T ^/^^■-.‘t r#Oi<; o::' •■ : rt0#oiiJ» • >■ ' vTifr r.'Ji*.;,; ( AjS ^ , ' ■'-*’<■1, rXji 4 4:to:L* %Ki . 1 1 - '•• ' ' ; o- / r .. 1 {jn * ' — : r; ' • •■; } :a 4»>« . . fii‘4 ^ . . i&i • 1 1 . ' ' T (T- . i -' -1^' , . .#1^ ' •<<»>> '•- .?( ' C : . \ ..; : . V ■“ fe I ; . !•. .- e ‘ri.^'U, .. , • ■ ‘ • '-. I '.'/.Tr. ',; .-V . A' ••: • X t»S? , i' '■•• • ■- '. ‘ ,^v' V- .J. t,. 0'-^. 1 ^ r- J Y'i fi ’’■''I. ■••* ■'ic'iH' i .13 .'/’• •.;. ^ V f J .** T •' »*.' > ‘ 'S - > ' « « •• • » • 4 * A I ' k AiJ - 2 - solutions as follows: "The molecules of the solution resist crys- tallization and some crystallizing force is required to start crys- tallization." 0stwald3 states that it is only necessary to have one millionth part of a milligram in a solution of sodium chloride j to overcome the passive resistance of the molecules and start crys- tallization of the sodium chloride. Stull^ , in comparing the crystallizing tendencies of various oxides draws the following con- clusions! - I. The strongest crystallizing tendencies are given to glazes by those chemical elements of low atomic weight whose oxides go to make up the R 0, such as sodium, potassium, mag- nesium, calcium, manganese, iron zinc, etc. II. Those metals of high atomic weight, such as barium, lead, etc., seem to impart a glossy nature to silicates when used in sufficient quantities, which is unfavorable to crys- tallization. III. Those chemical elements of higher atomic weight whose I oxides make the acid portion of a glaze such as silicon, titan-J ium, phosphorus, etc., produce the best crystallizing agents, while those of lower atomic weight, as for example, boron, having an atomic weight of 11, impart a fluidity and brilli- ancy to a glaze which is detrimental to crystallization. IV. The introduction of an R20^materially assists crystalli- zation in some cases, while in others it is detrimental to it, 3 Zeit. Phys. Cehm. 1S97, 22, 2S9. Ibid 1. Vol. VI., p. Igg. •.r.r; -( \-j .. • ; w. iCl^y , „i.f J.ol ,i . : ti. CO •.iUa.x/.j,:*.-; i-w ^ '' ', : ± '.. : ^ '1 * : / . .> V. ,< . V \-i. ;>f::;:;-., n xli^o l. .1 .u . :■ ,',;.jf, ,'i i . '.-a ^ tt ' . iXXr'.' . 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Il -3“ ^The name "Aventurine" as applied to glazes, originated from its similarity to certain types of quartz and feldspar spangled with scales of mica, hematite or gothite, They give off fire-like reflections when held in a bright light and are known as aventurine | feldspar and aventurine quartz. ! i Wohler 6 produced glazes having a similar appearance in lS^ 9 o | Wartha? obtained an aventurine effect by first applying an engobe o iron or uranium oxide and then covering the same with a borax glaze . Aventurine gla.zes are produced by mixtures in which there is an excess of metallic oxides which go into solution. The glaze matrix becomes saturated with the metallic oxide, and on cooling, the solvent capacity of the glaze reaches a maximum, the glaze be- comes supersaturated, and the excess gradually separates out in thin, plate-like crystals. The metallic oxides generally used in aventurine glazes are those of iron, chromium, and sometimes copper C6 Mellor*^ states that aventurine glazes are more easily obtained on red tile than on white tile. This is probably due to the fact that the glaze dissolves some iron oxide from the body and aids in satur ating the glaze. Stull^ advises the use of vitrified bodies which have been biscuited at a temperature of two or three cones higher than that of the glaze. Zimmerl^states that it is necessary to have; IM^.^ a continu- ously oxidizing fire; 2 ^^, a gradually increasing temperature; ^ H. G. Schurecht — Journal Amer. Cer. Soc., Vol. 3# No. 12 6 Thomind, Ztg., 1^96, p. 219- December, 1920. 7 Ibid, 1^90 p. 170 . ^ Zeit. Phys. Chem. 1S97, 22, 2S9. 9 Ibid 1, W. H. Zimmer. ^^Crystallized Odagea". Trans .Am. Cer .Soc «Vol .14-1912 .| I f* " n iSi9B ;fcir. .i . . :: :i i-lJ ¥4llTU^Cf«19fflkJJ^ ' ' ‘ 1 • .:f:VM V . .. » it . ) r I ; ,. V !'.. r * i: i: ■> I t ' *• e^;. « :* ■! ; 1 :j. '-'-u ( [,j f,v, fUlAi. -- ( t . .'A ' J. * A , .MT.« Of i 3^ , a gradually decreasing tempeirature; and exclusion of Al20^ from the glaze# The rates of crystallization of the differ- ent glazes vary so much with the tempera^ture that the rate of cool- ing after burning must be regulated to suit the glaze. Correct cooling is of as much importance as is correct composition. The purpose of the slowly cooling fire is to give the crystals time to grow. Most writers are of the opinion that the "aventurine effect" is best produced by introducing iron in a suitable form into a properly constituted glaze. Mackler determined the effect of increasing the iron oxide content in glaz«s of the cone 09 type and found that when 35 parts of iron oxide were added to 100 parts of glaze, he obtained an aventurine effect, but the color of the glaze was too dark, due to the reduct ioh of the iron oxide to the ferrous condition. He, therefore, tried 20 per cent of finely ground metallic iron and obtained a transparent yellow glaze with many gold-like crystals. The glaze used by him corresponded to the following formulas- 0.25 KoO ) ) 2.25 SiOp 0.25 Na 0 ) 2 ) 0.75 BgO, 0.50 CaO ) PatrikjlB produced artificial crystals of hematite by melting a mixture of iron sulphate and sodiuun chloride and dissolving in water. Crystals 1 to 2 mm. in diameter were produced in this manner. These cyrstals are not easily dissolved in the glaze melt Thonind, Zeitg., IS96, p. 219. Ibid 11, 1 S^ 6 , p. 275. /), * , • f . i; ’ . I. T V' .oc • r V .vn • 3 “ .■> .1* / ffcL*;u . '. »■ ^ '• " ^ \ ^ M J 1 ; . •: ' l 1 \ J if t'*' '.} •; . “ I 11 • 5 »iJf '. Snr* . iiJ tfC.. i:,0 'iO ftl* . :i‘Jl7i w^8|^ ' » 0 * 1 . i'i'ulJ. Mi/i>< lo J fi K" (ti ■ vllc'cci, • - r » 0 .., , ... . V iS-t* ■ I ' . :-• 4 L ;• l£.'d- - i;M,..ir • , v;f> j ^ ' . -' tr»i 4 •, nr'Trli:- T ^ • v;- 7 f < Xr- , */ .. •"'1 .r.i, . -yi}i ^ Cl'O'. '. •• S * ' ’ ^ ", ilc '•♦’Itti , iVfOl H- C, '* ■ i,;.* ■ * i i'.c '■ - ot '>' ni i'xi'Or.'- • -V ^ * :'r«^ %.if3 *i ir t;£^ 3 fyir i. . r4L/i:r oc •4 •i I ‘ vt I. t. Iw ' V ■» 'v." ,i';\ ■ I". OJCW X *..., ; “ 5 “ and when introduced into a glaze appear as bright scales similar to aventurine glaaes. The following are two formulae for aventurine glazes 8Ub“ mitted by Parmelee^^ and reported as giving good golstone glazes:- Cone 2 glaze Fritt for cone 2 glaze 0.10 K «0 2 0.2 KpO ] 0,15 NapO! f 0.3 NapOJ 0 o 22 A 1 0 d ' 0,2 AlnO-i) 0.25 I 2 3 ) 2.30 SiOp 0,2 CaO ) 2.0 SiOp 0 .30 BpO-z ' ' 0.6 BpO-z ) 0.35 PbO ) '' 0,15 FeO ) 0.2 PbO ; 0.1 FeO 1 Batch Weights Batch weights for fritt Fritt 14-1 Feldspar 111 Whiting Borax 115 White load 65 Whiting 20 China clay 31 White lead 52 Flint 64 Flint 4 S Red iron oxide 6 Red Iron oxide S Cone 09 glaze Fritt for Cone 09 glaze 0.40 NagO) 0.5 NapO) ) 0.4 BpO,) 0.4 PbO ) ^ 2,0 SiOg ) 0.03 AlpO,) 0.46 PbO ) 2.1 SiOp 0.14 FeO ; 0.32 BpO^ ) d Batch Weights Batch weights for fritt Fritt 220 Borax 76 Red lead 32 Sodium carbonate 32 Red iron oxide 5 Red lead 91 Ball clay S Red iron oxide S Flint 24 - Flint 120 • 13 Professor C. W. Parmelee, Cer . Dept ., University of Illinois. ■ h , t ^ » • u J i *A '’I •J v' 1 C.T %-A — 0 u. v'( oortH : /Pk/ % •_ V .. Ml*. ^ !. i.H i «■. ij' . ] * i ^ ’«o0 j-,.-: • ^ , **P- w>< - jr '"■. :-i ■'i r i-x ': 1 ': - r I ^ f. ' ; 3 ..* r . i . . . I'xT r^ry I: T .‘fc s. i, J . ■’ .■■ ' '.T '( '•' v,*t itfZf ' fef c I- : i • . . -i (■' • vuX i.\\ \K ifX » •’ dtii.iV & '. \ t t6>- - 6 - II Discussion of Previous Investigations. l^In experiments conducted by the Bureau of Mines, the effect of varying iron oxide and silica was studied between the following limits in a cone 4 aventurine glaze: j 0.05 AlpO, ) 0,4- Na«0 ) ^ i ^ ) 0.25 BpO^z I 2A » 4,2 SiO„ 0.6 PbO ) ^ ^ 0.12-0. SI Fc 203) A, Summary of Work done by the U.S. Bureau of Mines 1. Within the foregoing experimental limits aventurine glazes were obtained with more than 0.4-1 Fc20j in glazes containing 2.4- Si02# and with more than 0.5S Feg 0^ in glazes containing 4-. 2 Si02 a 2, Glazes with 0.4-1 to 0*73 FepO^ vary in color from red to black according to kiln conditions, red being produced under oxi- dizing conditions and black under reducing conditions. 3* With reducing conditions the glazes high in iron become a dull black with a metallic lustre. By applying a thin coating of accone 02 lead glaze on the surface of such a glaze and firing in an oxidizing atmosphere, a maroon effect is obtained. 4-. Increasing the iron content increases the size and mmiber of crystals and also the refractoriness of the glazes. B. Work done by Nathan Bromberg on Thesis for B.S. Degree in Ceramic Engineering, University of Illinois, 1915* The purpose of this study was to develop aventurine glazes which would mature at cone 010 (950° C) , cone 1 (1150° C) and cone 5 (1230*^ C). The field to be investigated was determined on, iT — — - Ibid 5. [i f r ^ . irv * » : : and a rectangular diagram drawn so as to include all the variations desired. Bromberg’s General Conclusions. From the results of the foregoing studies, the following con- | ! elusions may be drawn: 5 1. The formation of crystals depends upon the slow cooling of the glaze. As each glaze has a different rate of crystal- lization at each temperature, the cooling curve for each glaze should be determined individually* 2. The amount of Fe^O^ necessary for the formation of aven- turine crystals depends upon the glaze and may vary from 0.25 to 0.6 molecules. 3. Increasing the Na^O content increases crystallization. 4. Aventurine crystals may be formed in the presence of .2 molecules of A1_0^. 5 . Aventurine crystals may be formed in the presence of CaO even when there is as much as 0.4 molecule present, 6* Decreasing the lead, increases crystallization and de- creases the gloss. Crystals were obtained in the presence of 0.5 molecule of PbO. 7 . These aventurine glazes did not seem restricted to any particular molecular or oxygen ratio, but came within the limits of good glazes. ' . 1 . ' ' 'I '\r I. * I A » * \ Ill Scope of Present Investigation. In the present investigation an attempt has been made to study the effect of variations in the alumina, ferric oxide, boric acid, and R 0 members in a cone 1 aventurino glaze. The correct heat treatmtnt for the proper development of the aventiirine effect was also studied as a means of control of the crystal growth. lected as a basis of the study. The investigation was divided into two parts. In the first part the effect of variations in the alum“ ina, boric acid, and ferric oxide content, and the effect of differ ent heat: treatments were studied. For the second part of the in- vestigation, the best aventurine glaze developed in the first part was used as a basis for the investigation of variations in the RO constituents of the glaze. The formula of the glaze under investigation with all the variables indicated is as follows: - were varied; the R 0 was kept constant at 1,0 Na 20 . The series was divided into three groups; the first group contained 0.05 nioles of Alumina; the second group contained 0.10 moles of Alumina; and the third group contained 0 .I 5 moles of Al^amina. Each group was IV Method of Investigation A good aventurine glaze maturing at cone 1 (1150^ C) was se~ 0,0 to 1.0 NagO) 0.0 to 1.0 K^O 0,0 to 1.0 CaO 0,0 to 1.0 PbO For the first part of the experiment only the ^ 2^3 i; f I t - 9 ' divided into a rectangular field with four horizontal members rep- resenting variations in 62 ©^ content from 1,25 moles to 2.0 moles, and five vertical members representing variations in the Fe^O^con- tent from 0*75 moles to 0*95 moles. V Burning All the trials were burned in glazed saggars in a down-draft coal-fired kiln, described in University of Illinois Bulletin, num- ber 20, Vol. XI, #44. The first burn was conducted following the time temperature curve of Fig. 1 so that there was a considerable temperature difference throughout the kiln. Cone pads were placed in each saggar so that the heat treatment of each trial could be noted. The effect of temperature variations was in this manner closely studied. The next biirn was conducted at cone 3 (1190° C) and the final burn was conducted at cone 1 with uniform heat treat- ment throughout the kiln as far as possible. In the second part of the work the variations were made in the R 0 members as already shown and the trials burned to cone 1, A representation of the field covered by four variables is difficult to place on paper but a visual representation of the field is of a pyramid with a triangular base. At the apex of the pyramid, 1.00 Na20 is located with 1.00 KgO, 1.00 CaO, and 1,00 PbO as the three corners of the base of the pyramid. To give a clearer conception of the field covered, I have drawn up a series of tri-axial diagrami representing horizontal planes parallel to the base of the pyramid which indicate clearly the variations in the R 0 members. These glazes were burned to cone 1 in glazed saggars as before and the effect of the variable RO members was noted and tabulated 4 f . Ix U t 'J X JliCl* -■ V X ..cil < i«UJ! f '( * .li Ik- i. i.xj^ iooi I H . , , r. ::. je «T^ ; - §i; X' 1 dii . - oc< ixir: n "t 1 ■>. i. LxitJJ- »fi-. UA ^ £tM r /. ‘ ■j 'j V*' - i. ^ 'ttZZ' ■ Mittal- .i! 1.' V. w-g iQj-r ) t 5t}»U •XxJi . ..iv'H V. !.>;.., / 0 ».->r '.I eii.i icf; ; ■ t .•* CA xliU '>* 1 t?! •'^ •: ly' ..< ff".' *;■•:.•■ L . I ' t f'j7 . C '.<■'■ i... »ti'- p.'.^ iiv-jT trtJ I • ^ U‘t ■ f • lil - r.1;f l.;i» i 'i Lii -W0 iLtI#diW>4‘“ 1. hi -T- , . .'.•■iv vr- ft.- .. ‘ •■ ^JCf^ iuJBi; .t: F :.' 1 :C' n< I ■ iyC‘x »t v. ixuJ.. .sr ,4'. it'-. i-OJiXi"; » •».• :• i , viit ! i:r34<'j\-', ,i < 'Mfhm », si OgJiM .;;■ r. /t;* .*:' • ,tj lets ■ '., s. bvi\> o . *- ',4.!.' -;'J it evftr! ^ 'it; v.'S, ! :< i- u''- Q(iv le iX"ir- r I fxi -f.7 ’) rxi? .1 ' j. ■ \,* : f.o • ' ;-Lua' >j.ff ^ |j '»■ .' ■ .'.•; ,\ao t.j ..V ■!:> vC*i-r;'; AS^Aoii-**: i d^flTW « 7 £1 - '• 4 ;? f. ^;.'ii.!(f rridW «r.T»^?'v r;: , rf' . r:-"'*:. ' ajb i *'- .’M' »i - 10 - VI Method of Preparing Glazes j For the first burn of the first part of the investigation and | for the second part, all the glaze materials were fritted as it ! takes a long time for the glaze to assimilate all the materials, ana better aventurine glazes are produced if all chemical action has c ceased before the final fusion of the glaze. For the second and third burns of the first part, O 0 O 5 moles of alumina were omitted from the fritt and added as raw clay in an endeavor to take advan- tage of the plasticity of the raw clay to aid in keeping the fritt in suspension. As most of the glaze is quite fluid before all of the more , re- fractory materials of the glaze are entirely dissolved, the method of drop-fritting the glaze was not employed. The materials were fritted in closed bottom crucibles to a quiet fusion and then poured into cold water for quenching. After quenching, the fritts were ground in porcelain ball mills with water till they readily passed a 100 mesh screen. To keep the fritt in suspension in water, the best method devised was to satur- ate the suspension with aqueous ammonia while still in the ball mill, Using this method no difficulty was experienced in suspending the fritt in water. In the first part of the investigation, the four corner fritts of groups I and III were prepared as described and all the inter- mediate glazes were prepared by molecular blending. This method of blending is described by Purdy and Fox in their work on fritted glazes. ^5 in the second part, the four corner fritts of the pyra- 15 R. C. Purdy and H. B. Fox "Fritted Glazes”. Trans. 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O' ' ^ /J * - .r*,^ ftrft (jooi oT ,rtt d«oc' *X)I A' toeOJBq tX2j>06t £Xlt totow lUlt tirtoo ot ox^ft ^;y|vo^ .tod^t'X' toocf «. totfjbw iti nolotaoqooi ol ttXtl 1 " l^'-; .XXXvT XIo4 *dJ ot Hito oXi/jtr mlnoaiWA m/ootip# dit^ aoioceqoo# -j- ^ . - •* y 'I ;6Jt ;|r&itxiieiqMf1i nX OeofioXi^ccxe aitv Yiri4ro|lliA on bcuitfe<|; t rv »” 3 (f^’ .t»#fw ni tilal Jdtitl te.ttoo*' tirc'-i odJ t«o|tit§lJOoyjBl eritf. lo tlvifq ml , -If Tfll X£a feflo Lbrfitofeoto on l>dti»SU |4 TTV f. *^- • V Cii’j" J U 9 J - -. J - ', f ( vx^i> ntfi jc nar^th L to B^Xuoet orfjf ,<^X«r uocf^osotf rfoxA :^o «oii»»ooX'®'tfi: ,» » I . I .OriOi XBOX’iJ^;;i: 4 »XlMlllXll Pi AtPlCT I I t • . ;• \ ■'■ ‘^,i'' V^; V . /. '. , '<:-rV.- '..,■ ■■ :.»■: *-y, , , (V^K **^•1" r ■ . ..;■ i f* ’ '*3*^ '/|| *N '1 y* *.f,'rffi_i . ' .1!' iljtn.i. .y< I (b ---1 <—* -■ >4 r-T rH ■rt v-i o a.) :o > SO c 4) ,q; H> CO > 4^ o ■rH CO fH a; o o rO rH O V 1 CO • o • 4-i CD V-t P'S CO o N O o a; 1 — 1 •. ;-H Vi M •H 1-H 'H M H> 0) C “H . C' Jjl 5h J-t .r4 - H o 0 ^.- Ti "H 0 rH CO ■ 0 ^1 •0 C- GO 1 1 1 H* 1 1 1 1 1 ^ CO 1 1 1 ! 1 1 1 1 1 r 1 ( U'C 1 1 1 uo u c 1 1 1 1 1 1 1-0 1 1 ! r 1 1 ij.*r •CO ! 1 1 CO I I 1 H i i CO 1 I 1 i 1 1 Oi 1 1 1 (H I CO 1 1 .0 1 1 <■1 1 1 1 1 rH 1 1 CO 0~^ ' W 1 1 !-'( r .1 1-q O' 0 0 0 CO / — > — 1 cq q i--1 i 1 . — i ‘-H H -H 1 { 1 — i 1 — i 1 — 1 ) — i .-) /H rH — ! IH ;-i iH rH H :H —i M r— 1 rH H H .H VH i “1 r-( H ‘H -4 M 1-H 1 — t i— 1 iH H .'H • 0 1 rH ,0 4 - OrH Cvl .0 'h I :0 1 ! :.0 1 1 . 0 1 1 0 . 0 ! 1 1 1 ■ ■> r 1 1 “ 1 .0 ! 1 •.0 1 1 t 1 sl' I 1 1 1 ! 1 i f "■1 ! 1 1 ! I 1 1 1 I .' 1 1 u 1 1 1 I 1 1 1 1 1 1 1 1 1 1 1 1 1 1 ! r4 1 1 ' ■) ! 1 -4 . <4 1 1 V : J 1 — 1 .0 .0 -o' ICC 1 — 1 ^ > CO .-4 .1 'i ■4 -A 4 U 0 0 0 0 fq OJ oq Q Pi I-H ;-H IH . H IH — 1 ;H H ' H ■H H hH n M r-t r-l *— t 1 H r*^ iH rH H 1 — 1 ! — ! '-H IH H r t — 1 IH H IH jD CO :rs O r H .0 rH I — I I — I rH ^vl v\2 CO I I i I I I I 1 I t . 0 <’ '-o o CO -0 CO CO tH . I I rH CO 0 - . 0 1.0 1 , n H H . — I I — I :-H ]-H ■ H I — I CO Q Ui rH - 2 O -0 i p:) rq -n O , :H i-H M H -I r-H H H ;— ( -H —I 1—1 :-H i-t I x> o rH CO 0 -c;-! lo rH iH I — I I — I rH rH I I I H CO 0-C-' 05 rH - 0 0 rH -0 O s5) CO ^ tj 1 i rq cq "0 rq O O O O O 'H -H :H H iH — I H H H H H M i H H -H - 13 - FRITT FORMULAE and COMBINING WEIGHTS lAl ia6 IDl 1 D 6 IIIAl IIIA6 Proportion Pa rt s Comb • Weight, 0,05 Clay — 52.0 — 11.10 0.625 Borax— 954-.0 — 126.00 0.375 Soda Ash—— — I59.O — 23.25 0.950 FepO^ 6OS.O — — 152.00 6,900 Flint — 1656. 0 — . 4 - 14.0 0 3W.0 7^5 0.05 Clay- — — 52.0 0.625 Borax 954.0 0.375 Soda Ash— 159.0 0.750 FepO^— — 4 S 0.0 6.900 Flint———— 1656.0 34^.0 11.10 126.00 23.25 120.00 414.00 0.05 Clay 52.0 — — 1.000 Bora,x — I52S.O — 0.950 FepO-z-^ — * — 6OS.O - — — — 6.900 Flint- 1656.0 3 S 44.0 11.10 202 .90 152.00 414.00 779.10 0.05 ’Clay — 52.0 11.10 1.000 Borax — I52S.O 202,00 0.750 FesOx 480.0 — 120.00 6.900 Flint' 1656.0 — — 414.00 3716.0 T^TTio 0.625 Borax 954.0 0,375 Soda Ash — 159.0 0.150 Clay— 155.0 0.950 FepO:: 6OS.O 6.700 Flint 1 608.0 3463 .0 126.00 23.25 33.30 152.00 402.00 73^^55 0,625 Borax — 954.0 0.375 Soda Ash I59.O 0.150 Clay— 155.0 0.750 Fe«0, 480,0 6.700 Flint — — 16O8.O 335^0 126.00 23.25 33.30 120 .00 402.00 704.55 • AI '■ J- “l4-“ Proportion Comb. IIIDl 1.00 Borax — ^ — — 0.15 Clay — 0.95 FcpO -7 — — — — — 6.70 Flint-——-— IIID6 1.00 Borax — — — - — »»»— 0.15 Clay — — — 0.75 FcpO -7 6.70 Flint——— Parts Weight . 152s .0 — 202.00 155.0 — 33.30 605.0 - 152.00 160s. 0 — te .00 3 ^ 99.0 7 ^ 9.30 1525.0 — — — 202,00 155.0 — — 33,30 450.0 120.00 l6g0.0 402.00 3771.0 757.30 -15- RESULTS OF GLOST BURN Cone 1. Glaze Cone Description of glaze 1 1 3 Over-fired, dull, copper colored. 2 OS Under-f ired, dull , yellow colored, crazed. 3 OS " , " , yellow-red color, " . IL OS ” , " , copper colored, crazed. 3 3 Over-f ired,bright jbrownish-black color. 6 OS Under-f ired, dull, yellow-red color, crazed, j 7 3 Over-fired,bright, mottled brown color. S 3 Over-fired, " ,dark maroon color. 9 3 " , " , Brownish-black color. 10 OS Under-f ired, dull ,brick-r ed color , 11 3 Bright, deep brown color, few aventurine spangles. 12 3 Bright , black, speckled aventurine separations. 13 3 Bright , brown-black. 14 3 Matt texture , reddish-brown color. 15 3 Ower-f ired, dull , copper color dappled with black.. 16 3 Matt texture,copper color , bubbled, heavy aventur- : ine separation. 17 3 Matt eggshell texture , dappled brown and copper color. IS 3 Matt texture, copper colored. 19 3 n tt n » ® 20 OS Dull, dirty yellow color, crazed. 21 ' 05 Bright , transparent , yellow, white bubbly separa- tions on the surface. 22 06 i 23 o6 n 24 o6 " deeper yellow color. 25 03 ” yellowish brown color. 26 5 Bright , yellowish brown color , bubbled, crazed. !- C' I X rf»( t •r r \ 0 ::; - 16 - Glaze Cone Description of Glaze 1 27 5 Bright , brownish-black color, mottled effect* 2S 05 Bright, yellow color* 29 05 Bright, brownish yellow color. 30 03 " , yellowish brown color, pinholed, j 31 02 Bright, dark brown with aventurine separations, pinholed. 32 02 Bright, mahogany color, little aventurine , crazed. 33 05 " ,dark yellow color, crazed. 3^^ 05 ", " , " , bubbled. 35 01 ", " » ^ > pinholed. 36 2 Bright, deep purple color , checkered in glaze ef- fect, very fine aventurine , pinholed, cracked. 37 02 Bright, black color with heavy separations of copper colored aggragates. 3S 02 The same with less metallic separations. 39 4 Bright , reddish-black color with white,bubbly separations , 40 01 Bright , yellow color , bubbled. 41 05 Bright , yellow color, red aventurine only on thin edges , crazed. 42 05 n 05 Bright , reddish-brown color, filled with very Minute aventurine separations , crazed. 44 01 The same with larger aventurine separations. ^5 2 Bright, brown color, heavy with aventurine separa-J t ions , beautiful red and gold aventurine spangles around the edges. 46 05 The same except that the color is darker. 1^7 05 The same. 4S 05 Bright , orange color, very heavy and minute aven- turine separations , crazed. 49 2 Bright, dark purple color with one patch of beautiful red and gold aventurine spangles. 50 01 Dull, the greater part of the piece red and full of true goldstone spangles. 51 05 True matt texture , purplish-pink color, evident- ly a micro-crystalline structure. A* * ^'- ■ tf Si. 4k > t ri " • '.;<7 .^0 . ... ^ . ' 1 . . _ • ■’ j '- • i , <11 ii;yc * 4 » ... t» . . • ■ ; ^ fti/ % «» ^0 '.' ' • • V. j, »a ll, \ £ 'V"'' Glaze Cone 52 0 $ 53 04 5^ 01 55 01 56 05 57 05 5S 05 59 01 60 04 -17“ Description of Glaze The same but with more of the appearance of aventurine spangles in the glaze. The same but lighter in color. Bright , yellowish-brown color with heavy aven- turine spangles around the edge and few inside^ crazed. Bright, yellow color, aventurine on edges, crazed. Bright, deep brownish-purple color with very minute and finely divided aventurine spangles, not crazed and a very attractive glaze. Matt texture but in other respects the same as glaze 5^ a- niuch lighter shade. The same except a blighter finish and darker color. Bright , yellow color , heavy aventurine on the edges and very few spangles inside , crazed. Bright , light yellow color and very few aven- turine spangles , crazed. The diagram below show the three groups of glazes with the different areas marked off on them. Group I 0.05 AlgO^ Group II 0,10 AlgO^ Group III 0.15 Al^O^ B C B No ffych- / ■GO y/es. of ?s 1 .2^ 1 .30 1 .13 2.00 2 3 ,-./o ^'9 111 i . .\.a ^ . [s I i • X « w ... .‘V i.r' -1. . ‘ I f « «■ i ( 1 ,L. I L -IS- Discussion of Results These results indicate that with this glaze composition, an alumina content of 0,15 equivalents produces better conditions for the development of aventurine glazes than does a lower alumina con- tent, The results also indicate that the higher alumina content produces more easily fusible glazes than do the lower alumina con- tents. This may seem contradictory to ordinary experience but the results point to this conclusion. The glazes with 0*05 equivalents of alumina showed no aven- turine tendencies at all. This may be due to the heat treatment which they received; all of these glazes were burned either too high or too low. However, some of the other glazes with a higher alumina content which were burned either excessively high or ex- cessively low showed brighter glazes and contained aventurine spangles. One glaze alone in this group showed tendencies towards the development of aventurine effects and that was the one highest in boric acid and highest in iron oxide. This glaze only showed the spangles under the electric light and was dull and unsatisfac- tory. The aeea of high iron oxide and mediiam boric acid content with low alumina gave bright brown or black colored glazes which lost their gloss on contact with the air. The group of glazes containing 0,10 equivalents of alumina developed all bright glazes. In this group only the glazes highest in iron oxide and highest in boric acid showed any separation of the iron from the glaze. In some of these glazes, the separation was thin, minutely divided aventurine spangles but in one glaze, number 37 j i't separated as large metallic separations which gave a ■ 1 0 ‘.;“. •■ ■ f • r^*‘ 1 ' T' , * i*f • 1 • V' • VA J ♦ » t.' , 0 . ,i, i . y •• u'v '.»>• 1.0 i.:nt ^ %« vijp‘ -'X, “ .i' 'i'; . ’ i 4 „’ • rrrrf: ,o» w,.ii ., r- : . t "..■.» V? il« V Ak ! i- '••-'f -Jjl.-'J '■*1 -.1 ‘ AiVtaujt/ . 1 1 cs.r ';.r, \ v f!ci j:.d i ■!■: ■ .K : \':.i r;t*i • u- SiDix* : '. iZ‘ ": Vli^g' .■ fcftSbtlC ,! t -->CJvjc» oc X'9»'Cr!'; iini.'ju'j.. *c k:, < : v i, pc . ■ .’,-bp e f? oc r..‘:; t.:' yoA; . ii;. -oj’’-o .- i:?; i.-r oei ‘i '11 i cc fu'-*' ■/’' ' ! . r .:>3 »A' ri.jj,i^*.rf f - ■'••■ ' ks- : I ' » -• - .« ;.-i •*• \l *i .biw Sfiu^^iiaJQU niSr ' ■>"=' I t ■■ i' iv. r,i*u'-' ?:/;'■ * r.o'lt, /f.ii.'i lo : . C’. -iv -v.-j-' .ir^. A 4 ^ V j: ^ / f . X 00 ; .• >. WQ A ^ t ifc 1 ! w * . . rt 0 "O fifeO*^ .,^ 'io ]i^ :,a -J i i: ■•*• • f *'•■ £'• .. ' i/.u O. X;^ ;^rI;U ;.?f .Ci n f' ^ c:c'.i; .•.•.".vcjeti Vi.' £>£(;x oi':: *; n I; ocoi£:i;-' Ins: . :..o .o li pit h -' r.Tiv yX.'i' .'ii' n i r : f>iiC ^ ly ?».( oit u ' . ‘■Is; ..;. *i'. <..c-Trl tdS \ ' &f V n.' V . iiSrtlvif: v£«Cun£je ^ c-^w MfC Ai f 1 - 19 - rather attractive glaze but not of the aventurine effect. The color range does not seem to be uniform except that the glazes high in iron oxide and low in boric acid and those low in iron oxide and high in boric acid were lighter colored than the others. The other colors were dark yellow, brown, black and purple. i The group containing O.I5 equivalents of alumina showed the greatest tendency to produce aventurines. All of these glazes ex- cept the ones high in iron oxide and low in boric acid and those high in boric acid and low in iron oxide showed more or less aven- turine spangles. These excep^tions produced yellow colored glazes while the others produced darker colors. The glazes lowest in iron oxide and lowest in boric acid showed the best aventurines, produc- ing large patches of the true red and gold goldstone effects. In this group the glazes highest in iron oxide and highest in boric acid had a tendency to produce matt textures. In all the groups the glazes highest in iron oxide and lowest in boric acid and those highest in boric acid and lowest in iron showed more of a tendency to craze than the others. One peculiar effect noticed is that in each group, the glaze with the highest iron oxide and highest boric acid content pro- duced a bright brownish-purple colored glaze which had a good, glossy finish and good texture. This color grew darker as the alumina content increased. The glaze of this composition in the O0I5 alumina group was the best colored and finished, being glossy and smooth with no pinholing or crazing. It was uniform in color and texture and was thick with very tiny, minute aventurine spangles I which did not show up well except xinder the electric light. The glaze developed well clear down to the edges of the piece. It dev- ^ v;: f.; ;; ^( 5 ! ^ '-'i :^; '::i u *io£6o ofci t . jlXo »o*i 1 fti ' ICJ, - ■ :, -'ir 'I 'tdj'i, •_• ui't:lr^tp?Tvc. 5 ^. :.'r'j.v ttrfT' - >1 /J \: •.■.*<■ .: . wi; * .• ^ »<3 • -'cnc * J. . , r.. t> . >Xrg§ - s'.f ill :i> i ; ' , •■ji.-ifLi onxv.;;^ . - j .- . «*■ 'c> ♦i^.iii. i -eljiro . -.‘OtVir . -J airij •\. xfei w:i ■’ .it. : • •' ' c/ XiSv* uvTi L Ti .>•» ■'' t •r.*' j - . -i * • J <-rr. . : v".^oij|a(|si tZ'C — v~ •'-L t ..... , :*■' ■• ■. ■; : I ’ o '. xXi‘ cl ■ '■ •: U;i :,i*i >:< . . • '.'i:. , i- &iircf Gx ♦ - rj .- .ru-ij .1 •- S _ ‘i’c;a L-j-r'^ru. jSkw ; 'j .' .'*j ; . ,• £1 Mjx .'j”'.,* i.'J. ?t :'.e--.!-jr: oc. . r:aC;- -■•i- i v, ^ ‘ M V'lt rfj t» t -- !».'• ^ ' I , , ,.. _ : irr«ji: 7 .:^ i bb^:rt Pfi’lt V - i : 4 Of? ifi’ f .-.-J (fi -'• -S fjfli*:-' % ■ . > V V iJlv .oifi., 'X rr 'LiJ- &iUI ':X'i if otiio . V "I'-’i.- . sty,.-., xf!W tircilrj o(;.G •tiidw c Vr-' . . •« - • • i” t :: t V • '* iJCrTf? x,:©sl01' trk «M - 20 - eloped at cone 05 and makes a very pleasing glaze. The heat distribution through the kiln was not uniform so the heat treatment of the glazes varies and it is hard to draw conclu- i ! sions as a result. | Some of the glazes were dipped too thick and others too thin. Most of the glazes showed improper blending of materials, j With these handicaps it is hard to draw any uniform conclusions from the results. The heat treatment given the kiln seems to have been poor and the cooling especially seems to have been too rapid for proper development of aventurine glazes. Conclusions. 1. 0.15 equivalents of alumina gives a better condition for the development of aventurines than a lower content. 2. A low iron oxide together with a low boric acid content in this glaze with highest alumina content produces the best goldstone effects. 3. High iron oxide content with high boric acid in the high alumina glaze tends to give matt textures. 4. High iron oxide with low boric acid and high boric acid with low iron gives yellow glazes with crazing tendencies, 5. Increasing alumina content gives more easily fusible glazes. 6. The best temperature to develop these aventurines is cone 1 or cone 2* 7. * A good bright, brownish purple glaze maturing at cone 05 is developed with 0.I5 alumina, 0.95 iron oxide and 2.00 boric acid in this base glaze. S. The glaze blending and heat treatment must be accurate carefuiiY aventurine. glazes. *.• QOXll ' :i V* • .:\.T.r ', UflV . i.if.ia- u il*. ,'L' I' -• ... ., .• ,. % '■ “ •• : 'j ••' .', 5 ;’^' “ ■ , ; • i.’ tti*: ■ " «. i-r:. : , •Mif." CC t1»» J?v , i ^']f -f C -iStiiin. t»A| •: :Uif ^af n- *. . ;n->T eiJS* » ' 9 ■ 1 : •- ..r-L Ui^H ’.■ ;*' ..101 p 6 vi *. t . .» t' jfe- >1 KW -rii.:. ¥rtlJluil‘ i- ia ■' ".i ’» * ?S»S. ^ 1 »’u A lt L . l»;i !m. '’ t it’, i. i r.'Zi r? :; •■ f . j. . yc : 1 V ii !firu - ». . A V.. . , i' :.J.i < .'- iX. ; ' ' '* . 1 »» t ’’“ ;■ . ^ ► ■ • ‘ w ‘K'IJL 4 *'■ I* — Lf. ^ . I •: •. i || .. • ‘ ■■ “J.L :.■... ■.. iw I I h t 'C- T! •• V f ■ / a ^ ' >J .■' "a -‘ 'J ) -• ’ „ }' . 4 i .'/fe’i I. •. .' '■4 ilcX.’kvc ■, • % I'jc * ■ ,'Ii'^ ■^ ' . L 5 - *«0 JMH 1 -^.1 . f. f: '*r.' I ... . y.i; .-< <*(® . .. .. 8, _js tl '7 ■ r. . .-, ■ *' . » • •^■JV 'J, t, . J; - 21 - Cone 3 (11900 C) Burn The glazes used in this series were the s^-me as those used for the first burn except that 0.05 moles of Alumina were left out of the fritt and added to the glaze later as raw clay in an attempt to take advantage of the plasticity of the raw clay to aid in hold- ing the fritt in suspension. The glazes were burned to cone 3 glazed saggars as before | and the results are tabulated below. j RESULTS OF GLOST BURN - Cone 3. Glaze Cone Description of glaze 1 2 Light brownish purple, large metallic separations J glossy. 2 1 Light brownish purple, minute aventurinr crystals j glossy. 3 1 N k 2 Light red color, good aventurine separation, dull • 5 3 Brown to black color, red aventurine separations on edges, dull. 6 1 P\irple color, minute aventurine crystals , glossy . 7 3 Golden color, heavy metallic separ actions, dull. 2 Purple to golden, heavy aventurine separations. glossy. 9 3 Golden, heavy aventurine separations, dull. 10 3 Dirty golden color, good aventiirine separations^on edges , dull . 11 4 Reddish gold color , entirely crystallized, dull , overburned. 12 4 H 13 4 tl : 14 4 It 1 15 3 Reddish-brown color, heavy aventurine separations. dull. - 16 3 Reddish-brown color , metallic separations ,dull . 17 3 " ,beautiful aventurine crystals on edges , bright -nTV. . ... i., r-'f ' \\X , ..•■»' r-\. : V:? nA e£SC J M ' -t . • JScivi ftiki: 1 r i c. C . \ fi- .' • '.P.- -;ai ;;: c: V t' ' ; ■ -r-'-T'" L. ■ • I-. I ■ "'V.ii', fj i :. ,*'y ;..'i v. r*j '■ . 'i • >. o "■ I .. v: . ‘J. .. _ i > r: - L.^,' > ‘ r.;* i J /■ :; . . ' ■ I ■ ‘ ' „ .J ,. S ;> 'i ' XTivy? - r<%V«-j Y Jj i , l‘ i V "J •" ft . i *1 <• 1 1 1 * ■' • ■ !. ■ '.! <**««>»• ; .i . ■ i I Glaze Cone -22- Description of elaze Ig 4 Reddish golden color, entirely crystallized, dull , 19 4 over “burned. 20 4 Red to black color, heavy aventurine separations. 21 03 dull. Light brownish purple color, no crystals , bright . 22 03 n 23 03 « 24 03 n 25 01 Black, few metallic separations, glossy. 26 3 Yellow, entirely crystallized, dull, overburned. 27 4 Muddy gray color , entirely crystallized, dull , over- 2g 4 b\irned. n 29 1 Reddish gold color , beautiful crystals , dull . 30 3 Mottled gold and black , metallic separation,dull . 31 3 Reddish color , entirely crystallized, dull, over- 32 02 burned. Muddy purple color , metallic separations, dull. 33 01 under-fired. Purple to golden, heavy aventurine separations. 3^ < 1 glossy. n 35 2 Mottled red and gold, heavy metallic separation. : 36 3 dull . Dirty golden color , entirely crystallized, dull. 37 02 overburned. Dark purple, golden aventurine crystals , glossy . 3S 3 Red to golden color, entirelycrystallized,dull. 39 3 overburned. n 40 2 Red to black metallic and aventurine separations. 1 4l 03 glossy. Dull reddish brown color, no crystals , semi-glossy , 42 02 Brownish purple, minute aventurine crystals, semi- : 1 glossy. Golden brown color, heavy minute crystals , glossy , 44 1 Brownish purple color, few minute crystals , glossy . Glaze Cone -23- Description of glaze ^5 1 Golden red color , beautiful aventurine crystals. 46 2 glossy. Dark gray color , aventurine separations , dull , over- 1^7 02 burned. Purple color, no crystals , glossy , under-fired. 4S 02 Purple gray, shows tendency to crystallize , glossy . 49 02 Purple, no crystals, glossy. 50 1 s Reddish purple, good aventurine crystals, glossy . 51 3 Golden black color , metallic separations , dull. 52 01 overburned. Grayish purple, few aventurine crystals , glossy . 53 01 Purple color, few aventurine separations , glossy . 5^ 1 Purple to golden red, heave avent\irine separations. 55 1 glossy. Purple to dark red, beautiful aventurine separa- 56 2 tions, glossy. Dull black, few aventurine separations , semi-glossy i 57 2 Dull black to golden, heavy aventurine separations! 5S 1 glossy . Purple to golden, heavy aventurine separations. 59 1 glossy. Purple to red-golden, heavy aventurine separations , 6o 2 glossy. Red, mottled metallic separations , dull . Discussion of Results of Cone 3 Burn. The conclusions drawn from the first burn are pretty well demon-' strated by this burn to be correct. Evidently cone 3 is too high a temperature for these glazes, as most of them are overbiirned. One point is brought out quite strongly by this burn and that is the ef- feet of alumina on the development of aventurine crystals. The glazes in Group I with only 0»05 moles of alumina are nearly all of ! them entirely crystallized, indicating that the glaze was quite fluid at cone 3 > thus allowing heavy crystal separations. The glaze in Group III, on the other hand, have not crystallized so f t *> ■ .A- f/b 1 4 fci i. , _ _ i. ' ^ ' • . J. I, i jt' w' Jl! i j '.' '. I t,. . .. ■ . ’.■•> •_ i T._ ■ \ ^ ^ ^ t (' \ \ 1 t ' • . V . If. f..' ■ 'i' ' ► ■•':»- J - ri : : 1 , ■. r * i '■ " *:•<" i x .- ’ -f t. ’ ■ ,-• I: ■ ' « 4 .'‘ t ■ / ■- t f ‘ j . V r-r t 'i.. I 7oVii ,■ . I : f ivT* *• . w 'll V iJ i, ' . - cwt' 0 ; I I i ■ . ( ♦V ■ . <, > ^ Oi J - »'CO I .V j fmwA 'U H I ::el r' Yi.;; ^ c.i* ii c : If.':;, v ’.i . ; ■.r'4.v »- il'.- 1 iXr.i J • -i'i iTU. ''.t fir* ; >■ . Wf!*i- ' - • f* .. .-Is c £*i : ; Lr / i.h \ - . i : 9^1:'^-. fac : )', e?tT . :r- ;*!»/•; -.j -r'iVi; I .* .. -*tk.v -.'3 r... I o i,l.v v.fi....-r*: rvniirti Z: "ic Cifllciv * .; s"il^ T ! i i 'gffi-;* "iX-fri, • ^jr‘.Ls: i'. . : yi * s. li I *;r. ; tl l£j ’•..‘Jii; L-t v„.c^ '■V •:;*■ / i- ' > . r ■ .. r *; V A 4 tXil- !- I & iMo . «•• e ' ^ ‘^inV wi .'Ci.'.;. ■..c ■ 4 jLtj. li v’'*'’-' yl^j er: 6-y : ;: <, • £' f 'iii 'iw ..Jt . : f IT c • i . > ‘ *! ■ \ j t •■ . t r,:-'-3 ... ..o ,v Iftifoi'j ;.X) ic atU . ao5 i i' . i ' :■ X .> (• i; j I j ex(T ; 'jw ru*“ V t; . (,^.2 ifvijj, cc/ . r'' ' ' ■ ' •■■■' »4?-..i,L3 ..... . . ■•;£;•' t;<:4 nl , '/i4'*0 X X. .’iT C3 . X X :■: : .<4 V C^J^i.X i 1i .T.'re) ■ ■ •■X -V*;, r.v'T.* cic. 4 , "-rfvia *( ’ 1 . : 'i. . il'i.J'rf o4»‘. i'J ;• » i"i» lv'> ■ H X t ■■ .tft w f ■ f vXi i’i-.'O t> w «' X^irftXXjl Glaze Cone 1 01 2 01 3 02 4 1 5 1 6 1 7 1 S 2 9 2 10 2 11 2 12 2 13 2 i4 2 15 2 l6 01 17 01 IS 1 19 2 20 1 21 03 22 03 23 24 1 25 1 26 1 -25- Results of Burn at Cone 1 (1150®C) Description of glaze Purple color, no crystals, glossy, crazed. j ” , few minute crystals, glossy , crazed. | ", " , dull, crazed. ! l I Golden red, almost entirely crystallized, dull. Reddish black, beautiful aventurine crystals, glossy. Brownish purple, heavy with minute golden crystali glossy. n Golden, entirely crystallized, dull. > f • Red-golden, entirely crystallized, dull. H n ft n M « * » • Golden, entirely crystallized, dull. n w n » > » Brownish-red, entirely crystallized, dull. Brownish-black, few metallic separations, glossy. Brown, few metallic separations, glossy. Brown-red, patches of good aventurine crystals, glossy. Brown-red, entirely crystallized, dull. Purple-black to golden, heavy with minute crystal^ glossy. Red, no crystals, not developed, dull. Light golden, almost entirely crystallized, dull. Gunmetal color, patches of good crystals, glossy. Red-p\irple, no crystals, glossy. — 26“* Glaze Cone Desdription of glaze 27 1 Red-purple, no crystals, glossy. 2& 1 Gray -purple, minute aventurine crystals, glossy. 29 2 Red-golden, entirely crystallized, glossy. I 30 1 Black, beautifully crystallized, glossy. j 31 1 1 Red-purple, no crystals, glossy, crazed. 32 1 n n n n f » » • I 33 1 Red-purple, few minute crystals, glossy, crazed. 3‘^ 1 Red-purple to golden aventurine, glossy. 35 1 Black, metallic separations, glossy. 36 1 Red-purple, no crystals, crazed, glossy. 37 1 Dark purple, no crystals, crazed, glossy. 3S 1 Gray -purple, minute crystals, glossy. 39 2 Golden, entirely crystallized, dull. 4o 1 Black, beautifully crystallized, glossy. 41 03 Dull brown, no crystals, dull, underfired. 42 1 Brown-purple, no crystals, glossy, crazed. 1 Purple, minute crystals, glossy. 44 1 Gold-purple, many minute crystals, glossy. ^5 1 Red beautiful aventurine crystals, glossy. 46 1 Purple, no crystals, crazed, glossy. ; 47 1 n It n « » » » • 1 4S 1 It n It n > i i • ’ 49 1 It II It It » > » • 50 1 Red-brown, heavily crystallized, matt texture. ' 51 1 Red, no crystals, glossy, crazed. 52 1 Mottled purple , no crystals, glossy. 53 1 Red-purple, no crystals, glossy, crazed* JCS: II Ci i > - '. ■• 'xo a - , ^ w - * . - • - : . \ fin c iOAid i '‘I -:s t , r >v'.x^ W ^1! 1 •• ^ t £ A ■ i S , . 1 '■ 4 r f ' . . . •-, f.;i JL i V ..idffjk J t-C t ^ V . '■ ' 1 i i? X' 'i .' n r :•. . cc 1 4 Z\1‘. ^ . •, V t ' ' -4 . , -•. -ii , „..• . i ' >. 4 “ ■ i ' '_ l‘ h ■t \ ' 1 '. i'- . . - * j_ . ^ ' *■ J. ' , 1 t ^ 4 « jT .■•. w ^ •; 'i • 4'. - , . , uX'.( CO • s • •- • 4 - ***y ^ ^ \ •m U‘ * , ' ^ ‘ 1 • - •.' '! ; • « r I . '^ ',. '.1 ■ ’ . ’ • 1 V 1 , A t . 4 , i "; ■ f, 4i^ oV*A ;j i " I ^ . •<»4 f i I 't t ^ t i : r 1. >1- V, t V t I • t ’< " ( M *' It I "i I » ' i •• ' ‘ . '• LfC- -•. i. - 27 - Glaze Cone Description of glaze Red-purple, no crystals, glossy, crazed, ” ,few minute crystals , glossy, crazed. 54 55 56 57 5S 59 60 1 Purple-red, no crystals, glossy, crazed 1 Red-p\irple, " , ", " 1 Purple, no crystals, glossy, crazed. 1 Red, no crystals, glossy, crazed. 1 1 1 n > n n n Discussion of Results of Third Burn (at Cone 1.) As in the previous burns, the higher alumina content gives a more viscous glaze and retards crystallization to a very marked degree. The temperature of this burn is evidently the proper mat- uring temperature for these glazes as most of them turned out glossy and smooth. The low iron and low boric acid glazes give the best aventur- ine crystals, and the most beautiful glazes. Increased iron con- tent seems to give the glaze more of a red color than the lower iron content , When these glases do not develop any aventurine effect they nevertheless produce beautiful mottled purple colored glazes. Conclusions from Third Burn (at cone 1) The conclusions drawn from this burn coincide with the conclu- sions of the two previous burns. General C o nclusions on Effect of Heat Treatment an d Variations in the content of Aliimlna, iron and boric acid . The general conclusions drawn from the foregoing work are; 1. Aventurine glazes with these variable compositions mature w t'V=^ ^0 ^ • . .' '^X i - 1 j, “ a {. '¥ C M ’ »* 4 « . X ' . -fctfK X : ' V. ' . 1x1 *i X '' ■*". ) t •f* , ) v<.; 1 . ■’ i;r,'iT To b-- ^ ; . V I.'..;; •'ll 43 ! 1! *: •■ ■■ ^ ■ f w . 1- i «iA 1 i - r oj; .;■ f . 1 V w L' - •1 c V ’a f '• (WOOctV |l » J Vl^W»t>iV0 CIS L'l- '.< ^C- w! cdT * i ‘>‘u-fc yo sS'Oia c,*. QesbXt ■, .bjfJ -wl 4 «oo«» ixijj: i.' ->i - v; i*v>-n ? to.. z »,w.^ .■ rfT. j» /<■ . ^9CM Ti: ,> ^ ^j^j. ^,. ; ',. - 'iv • •- • :■■ J :>e8 hlBit. ‘ . »>C jj ^r*'* '-- ‘,ic> T : V ; •< . i:,n bb worn '. --^^j « ■■■ • '’'ivl.-c ‘A *•■"■’ '1'. i. i! :'.^T - ; •. «.- ' * j ( <■ ; ut-O >'•<.•) ijiax’S in ;. .kC i": ’^T'C I ■■-ti /'•;'' ., ’• .• - 'lor . t •• J ■ ■■ ■ •' •: a . •' i':H:Xa4icc VtfT c.’i’ !• avolv—K. owj "tc u , > ' # » . i .0 . ^ . out,,.,,' ^\inCu.'X^‘i t -2S- at cone 1 • 2. Increasing alumina content retards crystallization, 3 . Best aventurine glazes were obtained with low iron and low borid acid content. 4 . Least crazing was found in areas of maximum crystalliza- tion. 5 . In areas where no crystallization takes place, beautiful mottled, glossy glazes are produced with a rsd“p\irple color 6. To produce the best results, the glaze materials must be entirely fritted together before being applied to the piece 7. Careful blending and careful firing and cooling must be regarded for the proper development of aventurine glazes, S. The best aventurine glaze produced has the following com- position; (0.15 AI2O3) 1.00 Na20 (1.25 B2O3 I 7.0 Si02 (0.75 Part II. In the second part of the investigation an attempt was made to determine the effects of variations in the R 0 group on the devel- opment of aventurine glazes and their maturing temperature. This was accomplished as outlined in the Method of Investigation. The tri-axial diagrams showing the R 0 composition of each glaze are given in diagrams V,VI ,VII ,VIII , and IX. The method of preparing the glazes and of blending is the same as given for Part I, Series I and the firing was carried out to t ( ( . 1.1 ,^•c •• ■ ■ • . . • ; -1 . r \ r .. .. . 7f i'r;l 'j .... . ; ■ ' ■ . . ; *■' I 'V-jCnz. >i i • f.3: . V''..'! T' f A X/t‘ «JW» ■■; • . • o . '■ V ■; 1'e rtt ii-Ir -29- cone 1» The glaze formula with the R 0 variations used in this work is as follows: - 0.0 to 1.00 Na 0 0.0 to 1.00 K26 0.0 to 1.00 CaO 0.0 to 1.00 PbO ) 0.15 Al-0,) ) 1,25 B 2 ^ 0 i ) 0-75 Fc20^) 7.0 SiOg The glaze compositions, batch weights, and RO components of each glaze are given in the following tables. Glaze composition and Batch Weights Glaze 1: 0,70 0-75 Glaze 362 1.00 0.15 6.70 1.25 0,75 Glaze 51 : 1.00 0.15 6.70 1.25 0,75 Glaze 56: 1.00 0.15 6.70 1.25 0.75 0.625 Borax — - — - — 1906.O — 0.375 Soda Ash-—- 31S.4 0.15 Clay- 309.6 Flint— — 3216. Oir Fe203‘ KpOOt- Clay^-" Flint- Comb • Weight . — -126,00 — 23.25 — 3^.20 — 402.00 120 .00 Whiting" Clay Flint— ®2®3 Fe203 — 6712.6 1104.0 309.6 3216.0 700.0 960.0 62^9.6 70^5 94.00 34.20 402.00 67.50 120.00 737.70 600.0 56.00 309.6 — - 3^.20 3216.0 — 402.00 700.0 — — S7.5O 960.0 — — 120.00 5935. 6 699.70 mte lead- Clay — Flint—" B2O3 — *3“^’ — Fe gU- 1035.0 309.6 3216.0 700.0 960.0 223.00 34.20 402.00 67.50 120.00 msTfu I f r\ I? I I \ > -30- RO Component 3 of Part II Glaze RO Components . 1 1,00 Na20 2 o.S Na20, 0.2 K20 ^ 0.6 Na20, 0.2 CaO 4 0.6 Na20, 0.2 PbO 5 0.6 Na20, 0.4 K20 5 0.6 Na20, 0.2 K20 , 0.2 CaO 7 0.6 Na20, 0.2 K20 , 0,2 PbO g — 0.6 Na20, 0.4 CaO ^ 0,6 Na20, 0.2 CaO , 0.2 PbO 10 — — — 0.6 Na20, 0.4 PbO 11 0.4 Na 20 , 0.6 K 20 12 — — 0.4 Na20, 0.4 K20 , 0,2 CaO 1 ^ — 0.4 Na20, 0.4 K20 , 0.2 PbO l4 0.4 Na20, 0.2 K20 , 0,4 CaO 15 0.4 Na20, 0.2 K20 , 0.2 CaO, 0,2 PbO 16 0.4 Na20, 0.2 K20 , 0.4 PbO 17 — 0.4 Na20, 0.6 CaO IS 0.4 Na20, 0.4 CaO , 0.2 PbO 19 0.4 Na20, 0.2 CaO , 0,4 PbO 20 0.4 Na20, 0.6 PbO 21 — 0.2 Na20, 0.6 K20 22 0.2 Na20, 0.6 K20, 0.2 CaO 23 0.2 Na20, 0.6 K20 , 0.2 PbO 24 — 0.2 Na20, 0.4 K 20 , 0.4 C aO 25 — 0.2 Na 20 , 0,4 K 20 , 0,2 CaO, 0.2 PbO 26 0.2 Na20, 0.4 K20 , 0.4 PbO 27 0.2 Na 20 , 0.2 K 20 , 0.6 CaO 28 0.2 Na20, 0.2 K20 , 0.4 CaO, 0.2 PbO 29 0.2 Na20, 0.2 K20 , 0.2 CaO , 0.4 PbO 30 — — — 0.2 Na20, 0.2 K20 , 0.6 PbO 31 0.2 Na20, 0.6 CaO 32 0.2 Na20, 0.6 CaO , 0.2 PbO Na20, 0.4 CaO , 0.4 PbO Na20, 0,2 CaO , 0.6 PbO 35 0.2 Na20, 0.6 PbO 36 1,0 K20 37 0.6 K20, 0,2 CaO 3 S ... 0.6 K20, 0,2 PbO 79 0.6 K20, 0.4 CaO 4o — . 0.6 K20, 0,2 CaO, 0.2 PbO 4 i — — — 0.6 K20, 0.4 PbO 42 0.4 K20, 0.6 CaO 43 ... 0.4 K20, 0,4 CaO, 0,2 PbO 44 — 0.4 K20, 0,2 CaO, 0.4 PbO 45 0.4 K20, 0.6 PbO 48 0.2 K20, 0.6 CaO 47 ... — .. 0.2 K20, 0,6 CaO, 0.2 PbO 4 g 0.2 K20, 0,4 CaO, 0.4 PbO 49 0.2 K20, 0.2 CaO, 0,6 PbO 50 — 0.2 K20, 0,6 PbO 4 - ■'' ( - 31 - 1 Glaze RO Components 51 — 1.0 CaO 52 O.S CaO, 0.2 PbO ] p ?3 0.6 8 aO, 0.4 PbO j p 0,4 CaO, 0.6 Pb0 1 55 0.2 CaO, O.S PbO ! 56 — 1 .0 PbO 1 II RESULTS OF GLOST BURN— VARIATIONS IN RO MEMBERS - Cone 1. j Glaze Cone Description of ^laze 1 1 Purple red with good aventurine crystals, glossy. 2 1 Black, good aventurine crystals, glossy. i 3 1 Deep brown, good crystallization, matt textiors. 4 1 Purple-brown, no crystals, glossy. 5 1 Reddish-black, good crystallization, matt texture! 6 1 Black, metallic separations, glossy. 7 1 Red-purple , no crystals, glossy. g 1 Purple, no crystals, semi-matt texture. 9 1 Brown-purple, no crystals, glossy. 10 1 n 11 2 Black, metallic and aventurine separations , glossy 1 12 1 Red-brown, minute aventurine crystals, glossy. 13 1 Brown-purple, no crystals, glossy. 14 1 Purple, no ccystals, glossy. 15 1 Red, no crystals, glossy. i 16 1 Red, no crystals, glossy. 17 1 Red-purple, no crystals, glossy. IS 1 19 1 Red-purple, few minute crystals, glossy. 20 1 Red, no crystals, glossy. 21 1 Red-gold, good aventurine, semi-matt. i '■I ■■t I / 1 j: V t r t. i -32- Glaze 22 23 24 25 26 27 2S 29 30 31 32 33 3^ 35 36 37 3S 39 40 41 42 ^3 44 ^5 46 47 45 Cone 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 01 2 1 1 1 1 1 1 1 1 Description of glaze Deep purple, good aventurine, glossy. Red-purple, no crystals, glossy. Deep brown-purple , few crystals, glossy. Deep gray-purple, few crystals, glossy. Red“purple, no crystals, glossy. Deep gray-purple, very minute crystals, glossy. " , no crystals, glossy, n tt ti » f * Red-purple, no crystals, glossy. Dull black, very few crystals, dull. Deep purple, very minute crystals, glossy. « « It » » • Red-purple, no crystals, glossy. Red-purple, no crystals, glossy. Deep brown, metallic and aventurine separations glossy . Gold-jpnrple , very minute crystals, glossy. Red-purple, no crystals, glossy. Red-brown, no crystals, matt texture. Black, no crystals, matt-texture. Deep brown, no crystals, semi-matt texture. Deep brown-purple, no crystals. Red-brown, no crystals, glossy. n n n > » • Red, no crystals, glossy. Black-purple, no crystals, semi-glossy. n « « » t • » . , , ,f '• ; tytr' • • , . ■. ,: ■ V /r I 1 t n ')i \ ? ri -33- Glaze Cone Description of glaze ^9 1 Black-purple, no crystals, semi-glossy. 50 1 Deep brown, no crystals, semi-glossy. 51 2 : Black, no crystals, dull, under-fired. 52 2 Brown, " » ^ * 53 1 Red-brown, no crystals, dull , under -fired. 5|f 1 « « n tt . » » » • 55 1 Red, no crystals, matt texture. 56 1 H ^ If It ^ ■.» » > * DisGUSBion of Results of Gloat Burn with Variable R 0 Soda seems to be the member of the R 0 group which most assists crystallization. The glazes centered around the soda vertex of the pyramid all showed crystallization to a marked extent but the amount of crystallization diminished toward the other vertices. Potash was the next agent most conducive to crystallization, which is in- dicated by the formation of crystals in the trials all the way from the soda to the potash vertex. Lime and lead both seem to hinder the formation of crystals, probably because of the high viscocity of the glazes containing these R 0 members. Lead and lime both made the glazes more refractory so that their maturing temperature is well above cone 1. Lime made the most refractory glaze of all. The only effects noticed on the color was that lead gave the glazes a reddish-purple tinge which became more pronounced as the lead vertex was approached, becoming quite red-purple at the lead vertex , - 34 - Conclusions on the Effect of Soda, Lime, Potash and Lead on Aventurine Glazes, From the above work, the follov/ing conclusions are deduced: 1, Soda aids the production of aventurine glazes more than any of the other R 0 member® employed, 2, Lime gives the most refractory glaze of all R 0 members employed, 3, Potash is the second best agent in the production of Aven- turine glazes and lead is next, 4, The color of the glazes is little effected by the R 0 members employed except by lead which gives a decided red- purple color to the glazes, 5» The influence of soda in the production of aventurine glazes in combination with other R 0 oxides is very strong, A little soda in the glaze makes a vast difference in the fusibility and the tendency to form crystals. XI General Conclusions, The general conclusions drawn from this study of aventurine glazes are;- lo For the production of aventurine glazes a slowly increas- ing and steadily oxidizing fire is necessary. The rate of cooling must be slow for the proper production of aventurine crystals . 2, An increase in SiOg requires an increase FegO^ to produce aventurine glazes, (Schurect) 3* An increase in the iron contentincreases the size and t t.A- »'i-.l'OJ> %o * L:. .J ■ • A 4 t V.' tH L i "• ‘ '>. vilTCO -^.CL ''i e\-i^ ^ -r: w •-..■■ ;. l; jc i a tt it^,. ' 0 a 'itrivo t;'..'. .Li.-, iv Il-Jsl ' ’ C €»^ 1 - ' V ■•' . 1 -''u;: ■ t ^'j 2 c©" -'o f. r^A‘’ - . L- f 1 : i, ft V' PV ci V is: V. u S »V 1 'tv \ii' '^'i.;Cv J*;-; U»'J .*4 'S - 1 ^ iP nvi-** '^y:r V ■■■^ -.r.'-i :.i " R 'i'-f!:' rf*t^ ,i :J :f^!ifi.nvco .'^ i .'i?^-A'; r'.r'.5r'3s‘f. 1 : rd.«V ; «• 5 \ 4tf, v:i .i •-•]::';MX • V 1 . *. ■ K •■ I" :1p'i C.J V-f;2rl'^' ' V .' i £,H L c: A 'A>;: ■ V v ♦ I v'; \ ) V» number of crystals and also the refractoriness of the gla^^e. (Schurecht) 4. An increase of Na^O increases crystallization. Bromberg incorporated this conclusion in his v/oric. (See page 7 of this thesis). The conclusion was verified in my own worJic on variations in the RO components. 3 . Aventurine glazes may be formed in the presence of .2 mole of Al^O^. (Bromberg, see page 7 of this thesis) 6 . Aventurine crystals may be formed in the presence of CaO even v>rhen there is as much as .4 mole present . (Bromberg, see page 7 of this thesis) 7. Decreasing the lead increases crystallization and decreases‘ the gloss. (Bromberg, see page 7 of this thesis) iviy work on vari- ations in the RO members verified his statement, 8 . Aventurine glazes are notrestricted to any pa-rticular molecular or oxygen ratio, but come within the limits of good glazes. (Bromberg, see page 7 of this thesis) 9 . A low iron oxide content (0.73 moles) together v/ith a low boric acid content ( 1.23 naoles.) with high alumina (Q.I 3 moles) and silica ( 7*00 moles) content produces the best goldstone effects. This is my own observation and agrees with the obser- vation of Schurecht. 10. Crazing occurs least in the areas of best crystallization. This is contrary to the behavior of most crystalline glazes but seems consistently true with aventurine s, 1 1 . From the observations of Bromberg and from the conclusions of my own work on the variations in the RO contents, the order of beneficial effect upon crystallization of the RO members studied is as follows: 1 . soda. 2 . Potash, 3 , Lead, 4 , Lime, * K V::VT” !/■•■ ' .:< ^■; -iig/^J.'-?.' •**r' ,d.wJb| tHi",!©' i.k^ oila ■ r ';- . ‘ ('-itv' ” •' ^ ’ , ' ■ . ,pT’ '' ' ij ^.y ‘ '•ifcu^V'S: .aoi^sdiXX*^BTl5»' %r^!k 'I'Jo . ■ ' ‘ ’ ' • - V- ■ - - ' :' ' ' V.' */- ■ \ ba%i ,^inXiv ti.i aJ: ''ia(y4Ai; aUU tv^tiiioq:%6otl.^ ■*• - ■• ft' . . , y.'i ,, , i.,Ji|i'^ 4Af< ai (Si?ili'ife.ir D4IA* isjlf wfoij]pv «;.4I.;;;,(;6Jbi*'5 i>, , i -. 7 ;. ■,'•>; '-■ .-. . ' %: ■ V ■ _ f, ,1 Is k. “■ fj-j 1^ AK* ' " ? ’> 1 »f * ^ ,iLtiXs^o«X^. xaX;.»ci|^id^ \ju OJ c^^i, .aJcj'lR fco^. to a.ri^iii^K:f iSiC?^ UH ,Oi^£^ , . ^^I5l|L " v«.X4‘S^^ t kl'-'W ’ ^ 60i(i ^ • ' . .j.i'>' ' ■' ■ '^' ‘4.4: ^.ceXoB tX.v; ♦mas-14 fita tWXrf' fgiSiOttai^-iM X-tteifiias B'Xm ■« 'il. ' ■t'l . ' _ I . •' y,« . fc N(&.r , 2 rfU *» t’ s (; X 4 “ten ^£iQ i ao© ( a^ loiff jO \ '♦ ) «, i ©i X ia if// « ii • ' , , -loitdo 'ii':.- 44^4»‘ £>5»T[5^-J i,no acyX3i8v^T&i»do isX 5 i£^^j^ .eXo»tto J i* 1-^1 , aoX 9vy *i' I Ai - *• . » V D { 1 1 Ar * io aa»l« swJ aX e’e tfixiU-ij .1 ■. eo« • wit ' fciU bi^;t-t.a-'j4!^K)i' '• ‘^' 1 -., - • J-- •- *' W ( "Jt .e'oai'X4.ift,aV'd ^X.-'ius.j^’eciir© ecj^aB _ ., unoimi0^ ‘4^t xr e^iTvisoW i r f * ^ '■{>/-' .. ’.". ' ’■' ifci I'j /''i©£«a9 .- “• — — ^^.>V.!L;. y*'- *•-' • » :• - *• ■*••' • <1 ’ ' .MU.. ‘ ' <■ i r^’JH ; ;it«a L£U^ia^1h r.’* f *-. m; «V';Sto.-r itg;a;a(jai.?n;ayj ujr 9g; :«j e ae&g^ ^ ■v-< . M ■' - Wi* »if • . . ...U/' '■ V' ' . 4 ^' '.. “ - 36 - In concluding this thesis 1 wish to express my thanks to Professor C. W. Parmelee of the Ceramic hngineeriQgdepartment of the University of Illinois f orchis aid^in directing my* work and his assistance in tne collection of material, I further wish to acknowlege my indebtedness to IJethan Bromberg and H. G, Schorecht for the valuable information they have produced in their wrrx on the subject of aventurine glazes, I also wish to thanx the Ceramic Engineering students of the class of 1^22 for the information they have given to me through their study of aventurine glazes and the report of their work which I was allowed to summarize.