Calcium carbonate is one of the most important minerals in the earth’s crust  . Calcium carbonate has different phases such as calcium carbonate hexahydrate, calcium carbonate monohydrate, vaterite, aragonite and calcite. These polymorphs have different crystal structure and appearance  . Under all known conditions, the vaterite is metastable and has a higher solubility than the other CaCO3 polymorphs  . The transformation of meta-stable vaterite took place through dissolution process, followed by the crystallization of calcite. It is proved that the additives play an important role on the crystal growth rate, and could prevent the transformation from vaterite to calcite whether organic additives or inorganic additives  -  . Calcium carbonate is mainly used as filler in many industries that depend on its properties such as phase, morphology and size     . Calcium carbonate nano particles were used in drug delivery and bone substitution    , whereas vaterite has many properties that make it suitable for preparation of drug delivery carriers  . Vaterite has been used for the removal of dyes    ; for adsorption of phosphate  ; and metallic ions (Cu2+ and Mn2+)  .
Gum Arabic (GA) is the oldest known of all the tree gum exudates  and the Sudan is considered as the largest producer of gum arabic. Talha and hashab are the most common types of gum arabic   . Gum Arabic is a polysaccharide compound that is found as a neutral to slightly acidic salt   , contains soluble fiber  , has a pH of approximately 4.5 - 5.5  , and is considered a comparatively weak polyelectrolyte  . Gum arabic is used in many applications as a thickener, stabilizer and emulsifier   . Gum arabic is utilized as a dispersant for carbon nanotubes  , α-Al2O3, TiO2, ZrO2  , and Fe3O4  . Copper  ; and some of the noble metals nano particle are prepared in the presence gum arabic   . In addition, gum arabic is used in preparation of calcite  , and magnetic nanoparticles  .
The current study aimed to study the effect of gum arabic on the spontaneous formation of vaterite and on its transformation to the most stable calcite at different initial concentrations of [Ca2+] and at different incubation temperature with molar ratio 1:2, constant flow rate and stirring.
Gum arabic of the hashab type was obtained from Al-Nasr Company in Sudan and used without further purification. Calcium chloride dehydrates and sodium carbonate was analytical grade and used as received. Aqueous solutions of the reactants were prepared using doubly deionized water. Solution of gum arabic was prepared by dissolving GA powder in deionized water about 30 g/100 ml water.
2.2. Calcium Carbonate Preparation
Two litre glass flasks were used for preparation of calcium carbonate. Mixing was completed with the help of an overhead mechanical stirrer. The stirring speed for all the reactions was maintained at 1200 rpm. Vaterite was prepared by addition sodium carbonate solution to calcium chloride solution with different initial concentrations, 0.1, 0.2 and 0.3 mole at ambient temperature. The addition doses of the gum arabic solution were 0, 2.5, 5.0 and 10.0 ml of GA solution (30%)/0.1 mole of CaCl2.
In order to study the stability of formed vaterite in the aqueous solution, the synthesized calcium carbonate retained in mother liquor for 24 h. In addition, the incubation temperature effect on the stability of formed vaterite by the freshly prepared vaterite sample was dispersed in distilled water and refluxed near to 95˚C for 2 h. The prepared CaCO3 was washed with water, dried and kept for investigation by using FT-IR, XRD, SEM, TEM and thermal analyses.
A JASCO Asia Portal-FT/IR-6300 Spectrometer using the KBr pellet method was used to record the FTIR spectra of the prepared samples. The sample was ground with dry KBr in a 1:100 mass ratio and pressed at 5 tons to form pellets. An XRD 7000 (Shimadzu Instruments, Japan) at a 2θ scan speed of 4˚ min−1, λ = 0.154 nm with Cu Kα as a radiation source was used for determination of the crystallinity of the prepared calcium carbonates. Field emission scanning electron microscopy, a JEOL JSM 6360 DLA, Japan, and a transmission electron microscope ((TEM; Hitachi, H-800) where used for determination of the morphology and size of the prepared samples. DSC (NETZSCH STA 409 C/CD instrument) was used for investigating the thermal behaviours of some selected samples. The samples are studied up to 1000˚C, using a rate of 10˚C/min in an He atmosphere. The molar content (%) of vaterite CaCO3 polymorphs was calculated as described in   .
3.1. Effect of Gum Arabic Concentration
Figure 1(a) illustrates the XRD patterns of the prepared CaCO3 in presence of different dose, 0, 2.5 ml, 5.0 ml and 10.0 ml from 30% GA solution per 0.1 mol of CaCl2. In case of the absence GA, the peaks at 29.4˚, 36.0˚, 39.4˚, 43.1˚, 47.4˚ and 48.5˚ 2θ are attributed to the formation of calcite  , while the peaks at 2θ values of 24.8˚, 27.0˚, 32.7˚, 43.8˚ and 55.7˚ are related to the vaterite  . This indicates that the precipitated calcium carbonate without GA is composed of a mixture of calcite and vaterite phases. The molar content of calcite and vaterite in this sample is 66% and 34%, respectively. On the other hand, the XRD patterns of calcium carbonate samples prepared in presence of different doses of gum arabic have the characteristic peaks of vaterite only as a dominant phase. The molar content of vaterite in presence of GA was increased with increasing of dose to 100%. This means that the addition of GA to the precipitation system prevented the transformation of vaterite to calcite. The FTIR spectra of the
Figure 1. Powder X-ray diffractograms (a) and FTIR spectra (b) of calcium carbonate precipitated at 0.0, 2.5, 5.0 and 10.0 ml of GA/0.1 mole of Ca2+ solutions, V (vaterite) and C (calcite).
prepared CaCO3 with different doses of gum arabic are shown in Figure 1(b). The bands at 876 and 712 cm−1 are related to calcite phase  , which appeared only in sample without GA. All samples, which are formed with different dose of GA, have absorption bands at 745, 875, and 1083 cm−1 with a splitted band at 1420/1490 cm−1 as indicating to a vaterite phase  . The intensity of vaterite bands was increased with concentration of gum up to 10 ml/0.1 mol of Ca2+  . Also, the relatively ratio of I746/I712 increases with increasing of GA indicates that the content of polycrystalline vaterite increased  .
Figures 2(a)-(c) show the SEM images of some selected samples. Figure 2(a) shows the SEM micrographs of the CaCO3 particles that obtained in absence of GA, it is clearly shown that the CaCO3 particles have a regular plate-like calcite structure and an average length of approximately 3.7 mm and 3.3 mm in width. The SEM images of CaCO3 particles (Figure 2(b)), which are prepared with 2.5 ml of GA/0.1 mole of calcium chloride, have a typical broccoli-like agglomerate of vaterite, which is composed of subunits while that formed with 5.0 ml of GA/0.1 mole composed of submits particles with only the spherical morphology of vaterite (Figure 2(c)). This means the fraction of spherical vaterite increased with the increase of the concentrations of GA  . The surface morphology (smooth or rough) and crystal interior depend on the moment the GA is interfering with the crystallization process and polyelectrolyte chain length  . The TEM image of sample prepared without GA (Figure 2(d)) shows that the crystals consisted of rhombohedral crystals 85 - 95 nm in length and 55 - 75 nm in width, and its surface appeared as a sponge-like structure with minor amount of spherical particles that related to vaterite. TEM images of the vaterite precipitated with 5 ml of GA/0.1 mole of calcium chloride sample showed the formation of mono-dispersed uniform spherical particles 15 to 30 nm in diameter.
As showing in Figure 3(a), the calcite DSC-TG curve, which formed without GA, appeared a very small shoulder at 77˚C that was related to removal of physical water, and the main endothermic peak at approximately 699˚C indicating calcination of calcium carbonate. The weight loss percentage associated with this peak was 39% and the calculated calcium carbonate content was approximately 90%. Also, Figure 3(b) illustrates the DSC-TG curves of sample prepared in presence of 5.0 ml GA/0.1 mole of Ca2+. The DSC curve of this sample reveals four endothermic peaks. The first peak, at 85˚C, may be related to removal of the physically water that adhered on the surface of the vaterite agglomerate  . The peaks at 125˚C, 165˚C are attributed to water formed in crystals inside the pores of vaterite  . These peaks are related to the approximately 5.0% loss in weight. An exothermic signal at 397.3˚C is related to converting vaterite to calcite. The last endothermic peak at 635˚C and simultaneous mass change about (39.83%) demonstrated the decomposition of calcium carbonate and release of carbon dioxide. The calcium carbonate content can be calculated from TG to be approximately 99.5%  .
3.2. Effect of the Initial Concentrations of Ca2+
The Figure 4(a) displays the XRD patterns for calcium carbonate samples prepared from calcium chloride solution have initial concentrations 0.1, 0.2 and 0.3 moles in the presence of 5 ml of GA/0.1 mole of Ca2+. As showing from Figure 4(a), All the samples have peaks at 24.8˚, 27.0˚, 32.7˚, 43.8˚ and 55.7˚ 2θ which
Figure 2. SEM images of calcium carbonate prepared with (a) 0.0 ml; (b) 2.5 ml; (c) 5.0 ml of GA/0.1 mole of Ca2+ and (d) TEM images of calcium carbonate prepared with 0.0 ml and 5.0 ml of GA/0.1 mole of Ca2+.
Figure 3. DSC-TG curves of calcium carbonate prepared without GA (a) and with 5.0 ml (b) of GA/0.1 mole of Ca2+, DSC curves (solid line) and TG (dotted line).
are related to the vaterite calcium carbonate. In addition to the intensity of characteristic peaks of vaterite was increased slightly with increasing of the initial concentrations. The molar content of vaterite, for all samples, is about 100%. The FTIR spectra of CaCO3 samples (Figure 4(b)), which were prepared with
Figure 4. Powder X-ray diffractograms (a) and FTIR spectra (b) of calcium carbonate precipitated with 5 ml of GA/0.1, 0.2 and 0.3 mole of Ca2+ solutions, V (vaterite) and C (calcite).
different initial concentrations of Ca2+, are pointed to the vaterite is the only one component in all samples at all concentration and also agreement with the results of X-ray diffraction analyses.
Figure 5(a) shows SEM images of calcium carbonate prepared from calcium chloride solution with initial concentration 1.0 mole in presence of 5 ml of
Figure 5. SEM images (a) and TEM images (b) of calcium carbonate prepared with 5 ml GA/1.0 mole of Ca2+, at room temp., for 24 hrs.
GA/0.1 mole of Ca2+. As it show calcium carbonate has aggregate particles as broccoli―or cauliflower―like aggregates and have diameter near about 15 to 30 nm. TEM images (Figure 5(b)) shows these aggregate particles composed from subunits have spherical shape with particles size changed from 30 - 40 nm.
Figure 6 shows the DSC-TG curves of the thermal behaviour of prepared calcium carbonate from calcium chloride solution with initial concentration 1.0 mole in presence of 5 ml of GA/0.1 mole of Ca2+. It shows six endothermic peaks at 110˚C, 117.4˚C, 169˚C, 388˚C, 429˚C, and 671˚C. As shown above, this sample is composed of vaterite. The releasing of surface and crystalline water of vaterite and gaylussite was observed from signals at 110˚C, 117.4˚C and 169˚C. The TG curve shows the weight loss associated in this step to be approximately 5.5%. The endothermic peaks at 388˚C and 429˚C indicated double hydrated crystal transformation from low temperature form into high temperature form. In this step, the mass reduction is related to ignition of GA and the loss of well-deep water in vaterite. The endothermic peak at 671˚C is associated with the decomposition of CaCO3, where the mass change at this peak was 33.0% and the concentration of calcium carbonate was approximately 75%  .
3.3. Stability of Vaterite
In order to study the effect of gum arabic on the stability of precipitated calcium carbonate, it was retained in the mother liquor for 24 hours. Figure 7(a) illustrates the XRD patterns of CaCO3 particles which were prepared from calcium chloride solution its concentration is 0.1 mol in the presence of different doses of
Figure 6. DSC-TG curves of calcium carbonate prepared with 5 ml GA/1.0 mole of Ca2+: DSC curves (solid line) and TG (dotted line).
Figure 7. Powder X-ray diffractograms (a) and FTIR spectra (b) of calcium carbonate precipitated at 0.0, 2.5, 5.0 and 10.0 ml of GA/0.1 mole of Ca2+ solutions prepared at room temp for 15 min. and 24 hrs, V (vaterite) and C (calcite).
GA solution. As show, the peaks at 29.4˚, 36.0˚, 39.4˚, 43.1˚, 47.4˚ and 48.5˚ 2θ are attributed to the formation of calcite which was appeared mainly in samples that retained in mother liquor. This is indicted to the converting the vaterite to calcite whereas the CaCO3 samples that prepared without GA turned to calcite completely after 24 h, with the molar content of calcite 34% but after 24 hours in the mother liquor has become 100%. The intensities of the characteristic peaks of calcite decreased with addition of GA. The calcite contents are 100, 34, 6, and 4% with GA dose 0, 2.5, 5.0 and 10.0 ml, respectively. On the other hand, FTIR spectra (Figure 7(b)) show the sample that incubated for 24 hr in absences of GA was completely converted to calcite (the bands at 875 and 712 cm−1). While in the presence of GA there are traces of calcite was appeared.
3.4. Effect of Incubation Temperature
Figure 8 displays the XRD patterns of calcium carbonated incubated at 95˚C for 120 min. Figure 8(a) shows the XRD patterns of sample prepared with different dose of GA and incubated at ambient temp and at 95˚C. It shows that the calcium carbonate prepared in the absence of gum arabic at room temperature contains a mixture of calcite (40%) and vaterite (60%) but when prepared at 95˚C, the aragonite phase appeared (30%), located at 2θ 26.19˚, 27.16˚, 37.8˚, 38.5˚ and 45.87˚  while calcite and vaterite content decreased to 48% and 22%, respectively. This is mainly due to transform of vaterite to calcite and to aragonite, where at elevated temperature which stabilized the aragonite phase  . With addition 2.5 ml of GA to precipitation solution, at room temperature, the vaterite phase became the main component (100%) of calcium carbonate to vaterite but at 95˚C the sample composed of 56% vaterite, 29% aragonite and 15% calcite. This is contributed to the dissolution and recrystallization of vaterite to aragonite and calcite. As the dose of GA increases, the dissolution and recrystallization process of vaterite prevented whereas the content of vaterite was slightly changed from 100% to 94% and 95% for 5 and 10 ml of GA, respectively. This confirms the ability of GA molecules to absorb and bind to the surface of vaterite calcium carbonate particles and prevent them from switching to other phases despite the high temperature of the medium that helps to transform process. Figure 8(b) illustrates the FTIR spectra of the calcium carbonate samples that incubated at ambient temperature and 95˚C. The characteristic bands of calcite and aragonite were appeared in samples without and with 2.5 ml of GA after fluxes at 95˚C for 2 hr but did not appear with increasing GA dose. These spectra are conformed on that the GA molecules adsorbed strongly on the surface of vaterite particles and prevent the dissolution and recrystallization process either to calcite or aragonite. However it is known that the thermal treatment or elevation incubation temperature help to forming the aragonite phase.
Figure 9(a) shows the XRD patterns of calcium carbonate precipitated with 5 ml GA/0.1, 0.2 and 0.3 mol of Ca2+ at 95˚C. It is shown that at low initial concentration aragonite phase only was formed that appears from the peaks located at 2θ 26.19˚, 27.16˚, 37.8˚, 38.5˚ and 45.87˚)  . While the vaterite phase formed with increasing concentration of Ca2+ with minor amount of calcite. This is undoubtedly due to the properties of gum arabic, which works to form the vaterite and prevent its transformation into calcite. The absorption bands at 700, 855, and 1083 cm−1 are related to aragonite (Figure 9(b)) that shows the formation of aragonite phase in the presence of 5 ml GA at the lowest concentration of Ca2+. While with initial concentration of Ca2+ increases only vaterite phase
Figure 8. Powder X-ray diffractograms (a) and FTIR spectra (b) of calcium carbonate precipitated at 0.0, 2.5, 5.0 and 10.0 ml of GA/0.1 mole of Ca2+ solutions prepared at room temp for 15 min. and 95˚C for 120 min., V (vaterite) and C (calcite).
formed. The SEM and TEM images of the aragonite prepared at 95˚C in presence 5 ml of GA/0.1 mol Ca2+ are displayed in Figure 10(a). The SEM images are shown only particles with needle morphology or the big spindles of aragonite that composed from nanoparticles about 75 - 150 nm. TEM images of aragonite show the individual needle-like shape that is composed of separate spindled continuous filaments or as a fingerprint.
Figure 9. Powder X-ray diffractograms (a) and FTIR spectra (b) of calcium carbonate precipitated at 95˚C for 120 min. with 5 ml GA/ 0.1, 0.2 and 0.3 mol Ca2+, V (vaterite) and C (calcite).
The DSC curve of aragonite (Figure 10(b)) clearly shows four endothermic peaks. The peaks at 120˚C and 200˚C are related to the evaporation of occluded water and decomposition of gum arabic  . According to the TG curves, the reduction in mass in this step was approximately 24%. Aragonite is a metastable phase of calcium carbonate and converted to calcite upon heating, as shown from the peak at 410˚C. This process is endothermic. The water appeared to be
Figure 10. SEM images and TEM images (a) DSC-TG curves: DSC curves (solid line) and TG (dotted line); (b) of calcium carbonate prepared with 5 ml GA/1.0 mole of Ca2+ at 95˚C for 120.
released uniformly during the transformation process and didn’t cause any distortion of the DSC curve  . The endothermic peak at 677˚C is related to the calcination of calcium carbonate. The mass change according to this peak was approximately 43.9%, which indicate that the concentration of calcium carbonate was approximately 99.5%.
The chemical composition of organic compounds plays an important role in the crystallization process and hence the form and type of product, whereas these additives change the properties of the solid-liquid interface during the crystallization and recrystallization process. The presence of −COOH, −OH and −NH2 are the main functional groups in gum arabic acquire it slightly acidic properties. The Wattle blossom model of gum arabic  indicates that it consists of arabinogalactan (GA), arabinogalactan protein (AGP), and glycoprotein (GP) (Figure 11(a)), this means GA has a hydrophilic and hydrophobic species. The pH value of the native gum arabic solution was 4.58, and its isoelectric point was 1.8. At this point, the carboxylic and amino groups carry negative and positive charges, respectively  . The carboxylic groups become fully protonated and less hydrophilic in acidic media at pH < pKa, whereas at pH > pKa, the carboxylic groups become ionized and have lower hydrophobicity. Thus, the GA molecule will compress and expand   , Figure 11(b). These conditions help to form strong bonding between calcium ions and gum arabic molecules as shown in Figure 11(c). Dror et al. was reported  , in aqueous systems of GA, which electrostatic repulsion does not play a controlling role in emulsion stabilization, but steric repulsion might be the main mechanism for particle stabilization. Amorphous calcium carbonate is formed once the carbonate ions are added to the calcium ions solution, which is directly converted to the hydrated calcium carbonate. These forms are converted into vaterite or aragonite according to the precipitation conditions and then turned into the most stable form of calcite. At the first period of the spontaneous process, the nuclei formed will act as seeds and will further grow to larger sizes before aggregation and forming secondary particles. The presence of GA resulted in the capture of calcium ions by fully ionized carboxylic groups to form a Ca2+-GA complexes, (GA(COO−) + Ca2+ ↔ GA(COO)Ca2+. These complexes are formed rapidly and make the surface of the aggregates the most active site for nucleation. It is well known that vaterite crystals predominately grow from supersaturated solution. The (0 0 1), (1 0 1), and (1 1 0) planes of vaterite are positively charged and contain exposed Ca ions; thus, complex adsorbs preferentially on these faces and block further growth to another axes and prevent vaterite transformation  . By further vaterite growing under GA complexes, pores of the spherical vaterite particles are filled, giving rise to the raspberry shapes by aggregation of several spheres. At high concentrations of GA, the vaterite is the most formed phase. Whereas, the GA molecules becomes more incorporated into calcium carbonate crystal facets and a
Figure 11. Scheme of reaction of GA with calcium ion and precipitation of calcium carbonate, (a) behaviour of GA in aqueous solution; (b) effect of change of pH on the terminal functional groups of GA; (c) combination of calcium ion with GA molecules and formation of GA-Ca+ complex; (d) absorption of GA on the surface of vaterite.
multilayer formed at the surface of the particle by intermolecular hydrogen bonding between adsorbed and free GA molecules. In addition, the physical presence of the adsorbed GA molecules changes the surface charge density. Therefore, GA molecules will only bridge near the closest point of interaction between particles as a bolaform molecule, but do not help to form large aggregates with only an enhancement of steric stabilization of the small primary particles and which prevents their aggregation leading to smaller secondary particles. In addition, at high concentrations of GA, the molecules may start self-associating in solution and therefore shift the equilibrium established between the free and adsorbed GA molecules. The low concentration of calcium and carbonate increases the content of the samples prepared from vaterite phases with the concentration of gum arabic, due to the strength of gum arabic bonding with calcium carbonate particles, which hinders their conversion to calcite despite the conditions. As the concentration of reactive materials increases, the sample content of the vaterite increased and reduced the calcite content that related to increase the supersaturation conditions  . Actually, the stability of CaCO3 polymorphic phases mainly depends on the properties of additives and their own solubility in aqueous solution  . The stability of these phases’ solids decreases in the following order: ACC < vaterite < aragonite < calcite. Whereas the bulk lattice energies of calcite over aragonite is due to its higher entropy content at elevated temperatures rather than its bulk lattice energy, which favors aragonite  . Therefore, the stability of polymorph and morphology of CaCO3 minerals are directed by both thermodynamic and kinetic factors  . When the prepared vaterite retained in mother liquor there are traces of calcite phase (about 6%) were formed due to dissolution and recrystallization process of vaterite. This explains the hiding power and strong bond between vaterite surface and GA molecules, whereas the GA formed a multilayer at the surface of the particle by intermolecular hydrogen bonding between adsorbed and free GA molecules   . At elevated incubation temperature, the GA contaminated CaCO3 particles exhibit strong resistance towards aggregation into flocs and are stable to recrystallization process in water   . This stabilization effect is achieved when the amount of GA is sufficient to cover the surface of all formed particles and formed the GA shell. So the uncoated particles will then undergo dissolution and recrystallization and formed traces of calcite. The formation of aragonite at concentration 0.1 mol of Ca2+ may related to decrease the supersaturation conditions that enhanced by elevated temperature  .
The effects of gum arabic on the formation and morphology of calcium carbonate were investigated. Different analytical techniques were used to study the mineral and chemical composition, microstructure and thermal behaviour of prepared calcium carbonate. Based on the obtained results, we can provide the following. GA has ability to directing of calcium carbonate to formation vaterite. Increasing the GA dose enhances the molar content of vaterite. Vaterite aggregates as broccoli―or cauliflower was formed at low dose of GA and full spherical particles at high dose. The increasing of initial concentration of Ca2+ has slightly effect on the vaterite content. GA improved the stability of vaterite under aqueous solutions up to 24 hrs and elevated temperature. SEM and TEM analysis were shown that all the prepared vaterite calcium carbonate composed from nano sized particles. GA as biomaterial can be use for preparation of bio-vaterite calcium carbonate.
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