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Bort

Bort, also spelled boart or , is a term in the diamond industry referring to low-quality, imperfectly crystallized fragments or polycrystalline aggregates that are unsuitable for use due to their , , color, flaws, or inclusions. These are typically opaque and , consisting of finely crystalline aggregates intergrown with non- carbon, which contributes to their lackluster appearance and difficulty in polishing. Unlike gem-quality diamonds, bort lacks the transparency and brilliance required for jewelry, distinguishing it from other natural diamond varieties such as (a related but denser ) or ballas. The term "bort" originates from the early , likely derived from "boort" or related to "gebrot" meaning fragment, reflecting its brittle and fragmented nature. Historically first documented in 1622, bort has been valued primarily for industrial purposes since at least , when it was recognized as a key source of and small fragments for commercial applications. Chemically identical to high-quality diamonds (pure carbon, formula C), bort's properties include extreme hardness (10 on the ) but reduced tensile strength due to its irregular structure, making it ideal for crushing into powder. In modern usage, bort constitutes a significant portion of —often over 80% of rough from certain mines—and is crushed for abrasives in cutting tools, , and other gemstones. While rarely faceted for jewelry due to polishing challenges, some exceptional pieces have been cut experimentally, though they remain niche. Major sources include and , where bort often occurs alongside more valuable in alluvial deposits.

Definition and Terminology

Etymology and Naming

The term "bort" derives from the "," referring to small, waste fragments produced during cutting, and is possibly linked to the "bort" or "bourt," meaning "bastard" or "inferior," reflecting its low quality relative to . This underscores the material's historical perception as substandard carbon crystals unsuitable for jewelry. The word first appeared in English in the early 17th century, with the earliest recorded use in , as documented in and trade texts describing processing. Spelling variants such as "boart" and "boort" emerged due to regional linguistic differences in the diamond trade centers of Antwerp and Amsterdam during the 16th and 17th centuries, where Flemish and Dutch influences shaped terminology in trading ledgers and polishing guild records. These variations appear interchangeably in historical documents from these hubs, which dominated European diamond sorting and cutting after the influx of rough stones from India and Brazil. In early trade nomenclature, "bort" specifically designated non-faceted, irregular pieces that were too flawed or misshapen for , setting it apart from high-clarity crystals destined for ornamental use. This distinction arose in the burgeoning Antwerp-Amsterdam markets of the 1600s, where bort was segregated for purposes rather than aesthetic value, aligning with its broader classification as an industrial variant.

Classification as Diamond Variant

Bort serves as an umbrella term in the diamond industry for non-gem-grade , encompassing shards, fragments, and flawed crystals that exhibit opacity or significant inclusions rendering them unsuitable for jewelry applications. These materials are distinguished from gem-quality by their lack of transparency and structural integrity, primarily due to internal flaws and irregular formations that prevent effective light transmission and polishing for aesthetic purposes. Classification of bort relies on criteria such as opacity, typically ranging from fully opaque to semi-opaque gray varieties due to inclusions and irregular . varies, often consisting of small fragments but including larger flawed unsuitable for gem use, and shapes commonly including irregular cubic or octahedral forms derived from broken . These attributes ensure bort's designation for rather than ornamental use, as the imperfections compromise brilliance and durability for faceting. Bort is distinct from related polycrystalline diamond varieties such as and ballas, which share non-gem-grade characteristics but have unique aggregate structures: as porous, black masses of intergrown microcrystals, and ballas as spherulitic clusters of diamond crystallites. These differences highlight bort's focus on low-quality, imperfectly crystallized fragments separate from such specialized forms.

Physical and Chemical Properties

Appearance and Morphology

Bort diamonds exhibit an opaque to translucent appearance, frequently displaying dark hues such as black, gray, or brown, which arise from abundant inclusions and impurities that scatter light and reduce clarity. These stones typically present irregular and rugged exteriors, manifesting as fragmented chips, elongated needles, or cleavage shards formed through natural breakage during geological processes. Unlike the transparent, well-faceted forms of gem diamonds, bort's rough, unpolished surfaces emphasize its industrial character. In terms of , bort encompasses a range of structural variations, from flawed single to dense polycrystalline aggregates that lack distinct external form. Common examples include twinned , distorted octahedral shapes, and fibrous aggregates resembling hailstone boart with concentric or radial patterns. Polycrystalline types, such as framesite or ballas-like forms, often appear as granular masses or spherocrystals, reflecting rapid growth conditions that prevent ideal crystallization. Microscopically, bort is characterized by prominent graphite inclusions and internal fractures, which become evident under 10x and further contribute to its opacity and structural heterogeneity. These features, including syngenetic graphite particles and mineral intergrowths, clearly differentiate bort from higher-clarity types by highlighting its flawed, aggregate nature.

Hardness, Density, and Impurities

Bort shares the exceptional of gem-quality , achieving a rating of 10 on the , the highest possible value. Despite this intrinsic , the effective toughness of bort is often reduced by internal fractures, cracks, and inclusions that make it prone to chipping during use. In industrial applications, Vickers measurements for bort typically range from 10,000 to 12,000 kg/mm², reflecting its suitability for tasks while highlighting variability due to structural imperfections. The of bort generally falls between 3.1 and 3.5 g/cm³, with values varying based on the extent of and inclusions present. This property is determined using the standard formula \rho = \frac{\text{mass}}{\text{volume}}, commonly assessed through specific gravity tests that compare the material's weight in air to its weight in . For instance, high-purity bort samples approach 3.5 g/cm³, while those with greater content exhibit lower densities closer to 3.1 g/cm³. As a primary allotrope of carbon, bort primarily consists of diamond microcrystals intergrown with non-diamond carbon (e.g., ), along with inclusions such as iron, , silicates, or sulfides that constitute up to 1-2% by weight, contributing to its opaque appearance and distinguishing it from clearer variants. These impurities significantly lower thermal conductivity to around 500-2000 W/m·K, in contrast to the 2200 W/m·K observed in pure , thereby affecting heat dissipation in high-performance applications.

Sources and Production

Natural Occurrence

Bort forms in the under extreme high-pressure and high-temperature conditions, typically 5 to 6 gigapascals (GPa) and 900 to 1,300 degrees , where carbon crystallizes into structure from fluids or melts within or eclogite rocks. These conditions mirror those for gem-quality diamonds, but bort typically exhibits more extensive defects, such as fractures, inclusions, and irregular , often resulting from rapid cooling during ascent or incorporation of impurities like , silicates, or metals during formation. The primary natural sources of bort are and pipes, which act as conduits transporting mantle-derived material to the surface through explosive volcanic eruptions. These pipes are predominantly located in ancient cratons, including South Africa's (e.g., Cullinan pipe), Russia's Siberian Craton (Yakutia region), and Australia's West Kimberley region (Argyle pipe). Significant quantities of bort are also obtained from secondary alluvial deposits, formed by and transportation from primary sources, particularly in where they occur in river gravels and terraces, and in parts of . In these deposits, bort constitutes the majority of output, comprising approximately 70 to 80 percent of all mined , far outnumbering gem-quality stones due to the prevalence of flawed crystals. Bort is commonly associated with mantle xenoliths, fragments of peridotite (such as harzburgite or lherzolite) or eclogite entrained in the kimberlite or lamproite magma, which provide the host environment for diamond crystallization. These xenoliths often contain the diamonds embedded or adhering to them, and overall, about 80 percent of diamonds recovered from such sources are classified as bort-grade due to their opacity, fragmentation, or abundance of inclusions. The impurities within these defects influence bort's density and hardness variations compared to clearer diamonds.

Extraction and Processing

Bort, the industrial-grade form of , is primarily extracted from pipes through open-pit or methods, depending on the depth and accessibility of the deposit. In open-pit operations, layers of are removed to expose the , which is then blasted and excavated using heavy machinery. , employed for deeper pipes, involves tunneling and to reach the body, followed by controlled blasting to fragment the rock. For secondary alluvial deposits, extraction typically involves open-cast methods such as riverbeds, excavating gravels, and panning or sluicing, followed by simple gravity separation and screening, commonly practiced in and other regions. These methods yield containing low concentrations of diamonds, typically less than 1 per , necessitating efficient separation techniques. Following extraction, the ore undergoes dense media separation (), a sink-float process that exploits the high density of (3.51–3.53 g/cm³). powders are milled and suspended in water to form a with a controlled of 2.9–3.5 g/cm³, typically adjusted around 3.0–3.2 g/cm³ for optimal diamond recovery. The ore is fed into hydrocyclones or separation tanks, where diamonds and other heavy minerals sink to the bottom (the "sink" fraction), while lighter materials float away. This gravity-based method concentrates the diamonds, reducing the volume of material for further processing by up to 90%. The concentrated sink fraction is then crushed in stages using jaw crushers and cone crushers to liberate diamonds from the host rock, followed by screening to classify particles into size fractions suitable for industrial use. For bort, which consists of irregular, non-gem-quality crystals, the relevant size range is typically 0.1–5 mm, encompassing crushing bort (fine fragments) and drilling bort (larger, rounded pieces). Cleaning occurs via immersion in acid baths, often a mixture of sulfuric and nitric acids or hydrofluoric acid, to dissolve silicates, graphitic carbon, and metallic impurities from the matrix without affecting the diamond lattice. This multi-step process achieves overall recovery efficiencies of approximately 90–98%, minimizing losses while preparing bort for industrial applications. Synthetic production of bort-like diamonds, which now dominates industrial supply, relies on the high-pressure high-temperature (HPHT) pioneered in the . Developed by in 1955, the process converts to in a belt press or multi-anvil apparatus, applying static pressures of about 5.5 GPa (equivalent to 55,000 atmospheres) and temperatures around 1400°C. A metal , such as an iron-nickel , facilitates the by dissolving carbon at the atomic level and precipitating it as diamond crystals upon cooling. These conditions produce polycrystalline aggregates or small, irregular crystals akin to natural bort, with growth runs lasting hours to days and yields optimized for abrasive-grade material. Post-synthesis, the diamonds are separated from the catalyst via acid leaching, similar to natural processing, ensuring purity for industrial handling.

Industrial Uses

Abrasives and Polishing

Bort, being unsuitable for gem purposes due to its irregular shape and inclusions, is primarily crushed into fine powders known as for use in abrasive applications. These grits typically range from 20 to 1200 , enabling effective material removal in various grinding and finishing processes. Common products incorporating bort grit include for surface preparation, grinding wheels for heavy stock removal on metals and ceramics, and compounds for achieving precise flatness in mechanical components. Global consumption of industrial diamonds, including natural bort, supports a vast abrasives market, with worldwide production exceeding 15.5 billion carats annually, predominantly synthetic but supplemented by natural sources like bort for specialized high- needs. In contexts, bort-derived powders are employed in finishing optical lenses, where they provide sharp cutting edges for removing subsurface damage, and in wafer processing, utilizing slurries to planarize surfaces to nanometer-level smoothness. This sharpness stems from bort's structure, which, despite impurities, maintains exceptional for efficient without excessive heat generation. A key advantage of bort in these applications is its cost-effectiveness compared to gem-quality , priced at approximately $3.50 to $50 per versus over $1,000 per for gems, making it ideal for large-scale use. For instance, in tools, bort grits are embedded in polishing pads to refine stone surfaces like or , and in , they facilitate mirror finishes on components, balancing affordability with durability.

Cutting and Drilling Tools

Bort diamonds, being irregular and low-clarity fragments of natural industrial-grade diamonds, are commonly embedded in the metal matrix segments of saw blades and wire saws to enable high-impact cutting through hard materials such as stone, concrete, and metals. These segments typically incorporate bort at concentrations of 20-50% by volume, which balances cutting efficiency and tool longevity by ensuring sufficient diamond exposure for abrasion while maintaining structural integrity of the bond. The bort particles, crushed and sized to specific meshes, provide the necessary sharpness for initial penetration and sustained wear resistance during prolonged operations. In drilling applications, bort is used in diamond-impregnated bits for and gas exploration, as well as operations, where it contributes to superior wear resistance against formations. These bits, featuring bort-enhanced diamond tables bonded to substrates, are capable of to depths exceeding 10 km in challenging environments, such as deep reservoirs. The bort's hardness ensures minimal cutter degradation, allowing for reliable performance in high-pressure, high-temperature conditions typical of such depths. Performance metrics for bort-equipped tools demonstrate significant advantages, with feed rates typically ranging from 0.5-2 m/min in rock sawing scenarios and rates of (ROP) of 10-50 m/h in . Compared to alternatives, these tools exhibit tool life extensions of up to 10 times, reducing downtime and operational costs in demanding applications. For instance, in geothermal projects, diamond-impregnated bits incorporating industrial diamonds like bort have achieved enhanced rates of in formations, as evidenced by field tests in high-temperature wells where they outperformed traditional roller-cone bits by maintaining integrity over extended runs.

History and Economic Role

Early Recognition and Use

Low-quality diamonds unsuitable for gem use were recognized in ancient around the 4th century BCE, where such stones were referenced in texts like the in the context of gem classification and valued for their hardness in and cutting applications rather than adornment. These early utilizations leveraged their properties to work harder materials, marking one of the earliest documented non-decorative applications of diamonds. European awareness of low-grade diamonds emerged in the 16th century amid Antwerp's rise as a global diamond trading hub, where they were distinguished from gem-quality material, facilitating their separate handling in polishing and export activities. This recognition supported Antwerp's dominance in diamond processing. Use expanded modestly in the 19th century, but supply constraints persisted until the 1860s discovery of diamond fields in , which dramatically increased global availability of both gem and industrial-grade stones, enabling broader adoption. A pivotal shift occurred in the late when manufacturers adopted for wire-drawing dies, utilizing its exceptional hardness to produce fine metal wires efficiently, transitioning the material from sporadic artisanal tools to essential industrial components. This underscored 's value in and foreshadowed its widespread utilitarian role.

Modern Production and Market

In the 2020s, global production of industrial diamonds, including bort, exceeds 15.5 billion carats annually, with synthetic diamonds accounting for over 99% of the total output. industrial diamond production has declined to approximately 39 million carats per year as of 2024 due to mine depletion, while synthetic production continues to grow steadily. Major producers of synthetic industrial diamonds include , the , and , which together supply nearly 99% of the world's total. For natural sources, leads with 41% of output, followed by at 20% and the at 18%. The industrial diamond market is valued at around USD 1.8 billion globally as of 2024, driven primarily by synthetic variants used in manufacturing. Trade occurs through major hubs such as Antwerp, Belgium, where the Antwerp World Diamond Centre facilitates the exchange of rough and industrial-grade stones, though much of the synthetic volume moves via direct industrial supply chains. Pricing for synthetic bort and grit varies by size, purity, and form, typically ranging from USD 0.01 to USD 0.10 per carat for standard industrial applications, reflecting their low-cost, high-volume nature. In the United States, average unit values for domestically produced synthetic industrial diamonds reached about USD 0.33 per carat in 2024. Industrial diamonds, particularly bort, constitute over 99% of all diamond usage worldwide, underpinning key sectors such as for (CVD) coatings in semiconductors and for high-precision components. Their economic significance lies in enabling efficient cutting, grinding, and drilling processes across , , and , with apparent global consumption dominated by synthetic sources. In 2024, natural production saw further declines due to mine closures in major producers like and , accelerating the shift to synthetic diamonds for their lower environmental impact. Since the , the industry has increasingly emphasized sustainable sourcing, including enhanced traceability for natural diamonds under frameworks like the Kimberley Process and a shift toward low-impact synthetic production to reduce environmental footprints from .