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Researchers have also investigated historical Chinese documents. Bian stone has been applied in Traditional Chinese Medicine for various soft tissue injuries, especially, cervical spondylosis , acute or chronic lower back pain , [4] as well as skin disorders , such as abscesses or boils, and regulating qi and blood circulation. Therapy usually begins with a traditional Chinese massage to open up the body's meridians, followed by a series of Bian stone treatments with pre-heated bian stone.


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This therapy can be coupled with other traditional Chinese medicine therapy, such as acupuncture, or cupping to achieve the optimal effect on cervical vertebra [5] disease. From Wikipedia, the free encyclopedia. Archived from the original on 4 June Retrieved 27 May Cheng, Xinnong.

Beijing: Foreign Language Press. Categories : Stone objects Traditional Chinese medicine.

The Atlantic Crossword

The longest-performing rock band of all time, the Rolling Stones have greatly influenced rock and roll throughout the decades. After five decades together, the Rolling Stones have amassed eight 1 singles and ten consecutive gold albums. However, the Rolling Stones eventually created their own sound by experimenting with instruments and writing rhythm and blues mixed with rock and roll. When the Beatles hit international stardom in , the Rolling Stones were right on their heels. While the Beatles became known as the good-boy band influencing pop rock , the Rolling Stones became known as the bad-boy band influencing blues-rock, hard rock, and grunge bands.

In the early s, Keith Richards and Mick Jagger were elementary-school classmates in Kent, England, until Jagger went to a different school. Nearly a decade later, their friendship was rekindled after a chance encounter at a train station in While Jagger was on his way to the London School of Economics where he was studying accounting, Richards was commuting to Sidcup Art College where he was studying graphic art.

Since Jagger had a couple of Chuck Berry and Muddy Waters records under his arm when they met, talk quickly turned to music. The two young men once again became friends, creating a partnership that has kept the Rolling Stones together for decades.


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The band embraced aspiring young musicians with an interest in this type of music, allowing them to perform in cameo appearances. Soon, Brian Jones decided to start his own band.

Materials and Methods

According to Richards, Jones named the band while on the phone trying to book a gig. This new sound, a renaissance of blues performed by young British musicians, had kids standing on the tables, rocking, dancing, and shouting to the sound of electric guitars with a provocative singer. Bill Wyman bass guitar, backing vocals joined in December , replacing Dick Taylor who went back to college.

Charlie Watts drums joined the following January, replacing Tony Chapman who left for another band. The Stones appeared on the TV show, Thank Your Lucky Stars , to perform the song while wearing matching houndstooth jackets to appease television producers. This was their first American hit that went to 48 on the American chart. The press turned an eye toward the Rolling Stones, a group of brash punks upsetting the status quo by playing black music to young white audiences.

The band decided the press was good for their popularity and thus purposely started shenanigans such as growing their hair and wearing casual, mod-style modified suits to receive more media attention. Becoming too big to perform in clubs by early , the Rolling Stones went on a British tour.

Influence of Urinary Stones on the Composition of a Hour Urine Sample | Clinical Chemistry

In June , the band rolled into America to perform concerts and to record at Chess Studios in Chicago as well as the Hollywood RCA Studios, where they captured the vibrant, earthy sound they desired due to better acoustics. Their American concert in San Bernardino, California, was well received by excited schoolboys and screaming schoolgirls, even without a major hit record in the States. The identified phases of the Villarlod molasse are coarse grains of quartz, feldspars, biotite, and clay mineral phases within a calcitic and dolomitic matrix Fig. Well-identified green spots of glauconite are observed on thin section Fig.

These dispersed particles provide the global green color to the stone and helps to identify the natural orientation of the minerals. The extracted clay fraction under XRD allows to identify the clay minerals as chlorite, glauconite, and smectite. SEM observations inform on the morphology of theses phyllosilicates. Smectite phases are observed at the surface of the other components Fig. Smectite and glauconite are well-known to have a huge swelling ability and to induce the free swelling of the stone under hydrothermal solicitation.


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    7. These clay minerals are chlorite, kaolinite, illite, as well as mixed layers of chlorite and smectite. Microstructural properties are characterized at the initial dry state.

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    Open porosity to mercury is measured at The first stone shows a pore access radius at 2. Thus, the two stones show specific microstructural organizations and distributions. Moreover, the identified clay minerals are different and their sensitivity to moisture is quite various. Their impact on swelling, alteration, and evolution of the mechanical behaviour with respect to moisture content is discussed in the next section.

    FESEM observation of the Villarlod molasse: rigid minerals as quartz and feldspars are included in the clay matrix, mainly constituted of smectite. FESEM observation of the stone: quartz, feldspars and chlorite phases are identified, as well as the bimodal porosity. The free swelling strains of the two stones are measured at various specific RH states, on cores perpendicular and parallel to the bedding plane Fig. A macroscopic reversibility of the swelling behaviour over cycles has already been described in Tiennot Another result is the lower strain values reached during the drying phase.

    The gradient of induced strains between two RH levels is higher during the drying phase. This swelling ability of the stones is related to the nature and distribution of the clay phases. The influence of such anisotropic swelling behaviour and of the values discrepancy between humidification and drying phases on the mechanical behaviour are presented and discussed in the section below.

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    Dimensional behaviour of Villarlod molasse in the directions perpendicular and parallel to the natural orientation of minerals during humidification and drying, with stabilization at specific RH levels. However, the evolution is quite different for the two stones.

    Indeed, both elastic moduli of Villarlod molasse are affected as soon as the RH increases Table 2. These results quantify the known evolution of Young moduli with the increase of moisture content. Moreover, they illustrate the differences in the elastic behaviour of the two stones and the fact that Villarlod molasse is affected even for low moisture content. This is related to the nature of the mineralogical phases. Indeed, molasse main clay phases, smectite and glauconite, are both very sensitive to moisture.

    It appears with these results that they are involved in the loss of elastic properties at very low moisture content. This can be related to the free swelling strains Fig. The recovering of this mechanical property is in close correlation with the elimination of water molecules from the network and the minerals sensitive to moisture. As the swelling strains in the two directions indicate the important gradient induced during drying, the slightly improved values of both moduli during drying seem relevant.

    Indeed, the first result shows the inversion of its anisotropy. This indicates that deformation of this sandstone phases are highly different—for instance, between quartz and clay phases—and requires a microcracking evolution. Initiation of a drying-induced microcracking is highlighted. Thus, clay phases nature and distribution influence the swelling and consequently the elastic behaviour of stones.

    Fracture behaviour and toughness are studied with respect to the natural anisotropy of the stones. Both stones show a quasi-brittle and brittle behaviour Figs. From the initial dry state, samples present different fracture behaviours. Toughness values reached in each configuration are lowest for the molasse than for the sandstone Tables 4 , 5. SCBt is lower, indicating that initiation occurs more easily along the isotropy transverse plane.

    Evolution of the stones toughness under various RH conditions is then studied. Villarlod molasse fracture behaviour using SCB method with respect to the stone natural orientation. The resistance to the initiation of crack is more affected by water vapour pressure when m reaches high values. This phenomenon has already been observed, and is due to the water condensation effect at the crack tip Atkinson However, the influence of moisture content and of the induced swelling on the mechanical behaviour of the two stones is different.

    SCBn and SCBt values measured during humidification indicate that an anisotropy of fracture toughness appears when the moisture content increases Fig. Thus, oriented swelling influences the toughness with respect to the orientation of the phases. Villarlod molasse toughness evolution is described in Table 4 and Fig.

    Under this high water vapour pressure and thus this high free swelling of the material, the ability of the stone to withstand crack propagation is the same perpendicular and parallel to the natural orientation of minerals and microcracks. The swelling of the sensitive minerals, especially smectite and glauconite, annihilates the initial anisotropy of the fracture behaviour of molasse Fig. It should also be noted that molasse m parameters reach higher values than the sandstone.

    This indicates that the increase of moisture content affects more significantly the first stone. This may also be explained by the mineralogical differences and by the swelling ability of each phase. Thus, the two stones show a different behaviour in close correlation with the nature and accessibility of the mineralogical phases and their swelling ability has a direct impact on the macroscopic mechanical behaviour. Toughness evolution of Villarlod molasse with water vapour pressure with respect to the stone natural orientation.

    Evolution of toughness during drying is then verified.