wanyu/IteraTeR_full_sent huggingface dataset:
Original:  The refined value of the WGS 84 gravitational constant (mass of Earth's atmosphere included) is GM = ×108 m3/s2 . The angular velocity of the Earth is defined to be ω = 72.92115×10−6 rad/s . This leads to several computed parameters such as the polar semi-minor axis b which equals a × (1 − f) = m , and the first eccentricity squared,  e2 = ×10−3.
Revised:  The refined value of the WGS 84 gravitational constant (mass of Earth's atmosphere included) is GM = ×108 m3/s2 . The angular velocity of the Earth is defined to be = 72.92115×10−6 rad/s . This leads to several computed parameters such as the polar semi-minor axis b which equals a × (1 − f) = m , and the first eccentricity squared, e2 = ×10−3.
Edit intent: clarity
Original:  The refined value of the WGS 84 gravitational constant (mass of Earth's atmosphere included) is GM = ×108 m3/s2 . The angular velocity of the Earth is defined to be ω = 72.92115×10−6 rad/s . This leads to several computed parameters such as the polar semi-minor axis b which equals a × (1 − f) = m , and the first eccentricity squared,  e2 = ×10−3.
Revised:  The refined value of the WGS 84 gravitational constant (mass of Earth's atmosphere included) is GM = ×108 m3/s2 . The angular velocity of the Earth is defined to be ω = . This leads to several computed parameters such as the polar semi-minor axis b which equals a × (1 − f) = m , and the first eccentricity squared, e2 = ×10−3.
Edit intent: clarity
Original:  The refined value of the WGS 84 gravitational constant (mass of Earth's atmosphere included) is GM = ×108 m3/s2 . The angular velocity of the Earth is defined to be ω = 72.92115×10−6 rad/s . This leads to several computed parameters such as the polar semi-minor axis b which equals a × (1 − f) = m , and the first eccentricity squared,  e2 = ×10−3.
Revised:  The refined value of the WGS 84 gravitational constant (mass of Earth's atmosphere included) is GM = ×108 m3/s2 . The angular velocity of the Earth is defined to be ω = 72.92115×10−6 rad/s . This leads to several computed parameters such as the polar semi-minor axis which equals = m , and the first eccentricity squared, e2 = ×10−3.
Edit intent: meaning-changed
Original:  The refined value of the WGS 84 gravitational constant (mass of Earth's atmosphere included) is GM = ×108 m3/s2 . The angular velocity of the Earth is defined to be ω = 72.92115×10−6 rad/s . This leads to several computed parameters such as the polar semi-minor axis b which equals a × (1 − f) = m , and the first eccentricity squared,  e2 = ×10−3.
Revised:  The refined value of the WGS 84 gravitational constant (mass of Earth's atmosphere included) is GM = ×108 m3/s2 . The angular velocity of the Earth is defined to be ω = 72.92115×10−6 rad/s . This leads to several computed parameters such as the polar semi-minor axis b which equals a × (1 − f) = , and the first eccentricity squared, e2 = ×10−3.
Edit intent: clarity
Original:  The refined value of the WGS 84 gravitational constant (mass of Earth's atmosphere included) is GM = ×108 m3/s2 . The angular velocity of the Earth is defined to be ω = 72.92115×10−6 rad/s . This leads to several computed parameters such as the polar semi-minor axis b which equals a × (1 − f) = m , and the first eccentricity squared,  e2 = ×10−3.
Revised:  The refined value of the WGS 84 gravitational constant (mass of Earth's atmosphere included) is GM = ×108 m3/s2 . The angular velocity of the Earth is defined to be ω = 72.92115×10−6 rad/s . This leads to several computed parameters such as the polar semi-minor axis b which equals a × (1 − f) = m , and the first eccentricity squared, math| e2 = ×10−3.
Edit intent: meaning-changed
Original:  The refined value of the WGS 84 gravitational constant (mass of Earth's atmosphere included) is GM = ×108 m3/s2 . The angular velocity of the Earth is defined to be ω = 72.92115×10−6 rad/s . This leads to several computed parameters such as the polar semi-minor axis b which equals a × (1 − f) = m , and the first eccentricity squared,  e2 = ×10−3.
Revised:  The refined value of the WGS 84 gravitational constant (mass of Earth's atmosphere included) is GM = ×108 m3/s2 . The angular velocity of the Earth is defined to be ω = 72.92115×10−6 rad/s . This leads to several computed parameters such as the polar semi-minor axis b which equals a × (1 − f) = m , and the first eccentricity squared, e2 = .
Edit intent: clarity
Original:  External links Geodesy for the Layman, Chapter VIII, "The World Geodetic System" NIMA Technical Report TR8350.2 Department of Defense World Geodetic System 1984, Its Definition and Relationships With Local Geodetic Systems,  Third Edition, National Geospatial-Intelligence Agency.
Revised:  External links Geodesy for the Layman, Chapter VIII, "The World Geodetic System" NIMA Technical Report TR8350.2 Department of Defense World Geodetic System 1984, Its Definition and Relationships With Local Geodetic Systems, '' Third Edition, National Geospatial-Intelligence Agency.
Edit intent: fluency
Original:  The deviations of the EGM96 geoid from the WGS 84 reference ellipsoid range from about −105 m to about +85 m . 1966 version Improvements to the global system included the Astrogeoid of Irene Fischer and the astronautic Mercury datum.
Revised:  The deviations of the EGM96 geoid from the WGS 84 reference ellipsoid range from about to about . 1966 version Improvements to the global system included the Astrogeoid of Irene Fischer and the astronautic Mercury datum.
Edit intent: meaning-changed
Original:  The defining parameters of the WGS 66 Ellipsoid were the flattening (1/298.25 determined from satellite data) and the semimajor axis ( 6,378,145 meters determined from a combination of Doppler satellite and astro-geodetic data).
Revised:  The defining parameters of the WGS 66 Ellipsoid were the flattening (1/298.25 determined from satellite data) and the semimajor axis ( determined from a combination of Doppler satellite and astro-geodetic data).
Edit intent: coherence
Original:  The adoption of an a-value 10 meters smaller than that for the WGS 66 Ellipsoid was based on several calculations and indicators including a combination of satellite and surface gravity data for position and gravitational field determinations.
Revised:  The adoption of an -value 10 meters smaller than that for the WGS 66 Ellipsoid was based on several calculations and indicators including a combination of satellite and surface gravity data for position and gravitational field determinations.
Edit intent: fluency
Original:  It is geocentric and globally consistent within ±1 m . Current geodetic realizations of the geocentric reference system family International Terrestrial Reference System (ITRS) maintained by the IERS are geocentric, and internally consistent, at the few-cm level, while still being metre-level consistent with WGS 84. Ellipsoid reference Semi-major axis a Semi-minor axis b Inverse flattening ( 1/ f) GRS 80 6 378 137.0 m ≈ 6 356 752.
Revised:  It is geocentric and globally consistent within . Current geodetic realizations of the geocentric reference system family International Terrestrial Reference System (ITRS) maintained by the IERS are geocentric, and internally consistent, at the few-cm level, while still being metre-level consistent with WGS 84. Ellipsoid reference Semi-major axis a Semi-minor axis b Inverse flattening ( 1/ f) GRS 80 6 378 137.0 m ≈ 6 356 752.
Edit intent: clarity
Original:  It is geocentric and globally consistent within ±1 m . Current geodetic realizations of the geocentric reference system family International Terrestrial Reference System (ITRS) maintained by the IERS are geocentric, and internally consistent, at the few-cm level, while still being metre-level consistent with WGS 84. Ellipsoid reference Semi-major axis a Semi-minor axis b Inverse flattening ( 1/ f) GRS 80 6 378 137.0 m ≈ 6 356 752.
Revised:  It is geocentric and globally consistent within ±1 m . Current geodetic realizations of the geocentric reference system family International Terrestrial Reference System (ITRS) maintained by the IERS are geocentric, and internally consistent, at the few-cm level, while still being metre-level consistent with WGS 84. Ellipsoid reference Semi-major axis Semi-minor axis b Inverse flattening ( 1/ f) GRS 80 6 378 137.0 m ≈ 6 356 752.
Edit intent: fluency
Original:  It is geocentric and globally consistent within ±1 m . Current geodetic realizations of the geocentric reference system family International Terrestrial Reference System (ITRS) maintained by the IERS are geocentric, and internally consistent, at the few-cm level, while still being metre-level consistent with WGS 84. Ellipsoid reference Semi-major axis a Semi-minor axis b Inverse flattening ( 1/ f) GRS 80 6 378 137.0 m ≈ 6 356 752.
Revised:  It is geocentric and globally consistent within ±1 m . Current geodetic realizations of the geocentric reference system family International Terrestrial Reference System (ITRS) maintained by the IERS are geocentric, and internally consistent, at the few-cm level, while still being metre-level consistent with WGS 84. Ellipsoid reference Semi-major axis a Semi-minor axis Inverse flattening 1/ f) GRS 80 6 378 137.0 m ≈ 6 356 752.
Edit intent: clarity
Original:  It is geocentric and globally consistent within ±1 m . Current geodetic realizations of the geocentric reference system family International Terrestrial Reference System (ITRS) maintained by the IERS are geocentric, and internally consistent, at the few-cm level, while still being metre-level consistent with WGS 84. Ellipsoid reference Semi-major axis a Semi-minor axis b Inverse flattening ( 1/ f) GRS 80 6 378 137.0 m ≈ 6 356 752.
Revised:  It is geocentric and globally consistent within ±1 m . Current geodetic realizations of the geocentric reference system family International Terrestrial Reference System (ITRS) maintained by the IERS are geocentric, and internally consistent, at the few-cm level, while still being metre-level consistent with WGS 84. Ellipsoid reference Semi-major axis a Semi-minor axis b Inverse flattening ( 1/ GRS 80 6 378 137.0 m ≈ 6 356 752.
Edit intent: clarity
Original:  It is geocentric and globally consistent within ±1 m . Current geodetic realizations of the geocentric reference system family International Terrestrial Reference System (ITRS) maintained by the IERS are geocentric, and internally consistent, at the few-cm level, while still being metre-level consistent with WGS 84. Ellipsoid reference Semi-major axis a Semi-minor axis b Inverse flattening ( 1/ f) GRS 80 6 378 137.0 m ≈ 6 356 752.
Revised:  It is geocentric and globally consistent within ±1 m . Current geodetic realizations of the geocentric reference system family International Terrestrial Reference System (ITRS) maintained by the IERS are geocentric, and internally consistent, at the few-cm level, while still being metre-level consistent with WGS 84. Ellipsoid reference Semi-major axis a Semi-minor axis b Inverse flattening ( 1/ f) GRS 80 ≈ 6 356 752.
Edit intent: meaning-changed
Original:  It is geocentric and globally consistent within ±1 m . Current geodetic realizations of the geocentric reference system family International Terrestrial Reference System (ITRS) maintained by the IERS are geocentric, and internally consistent, at the few-cm level, while still being metre-level consistent with WGS 84. Ellipsoid reference Semi-major axis a Semi-minor axis b Inverse flattening ( 1/ f) GRS 80 6 378 137.0 m ≈ 6 356 752.314 140 m 298.257 222 100 882 711...
Revised:  It is geocentric and globally consistent within ±1 m . Current geodetic realizations of the geocentric reference system family International Terrestrial Reference System (ITRS) maintained by the IERS are geocentric, and internally consistent, at the few-cm level, while still being metre-level consistent with WGS 84. Ellipsoid reference Semi-major axis a Semi-minor axis b Inverse flattening ( 1/ f) GRS 80 6 378 137.0 m ≈ ...
Edit intent: meaning-changed
Original: 15|Equatorial ( a ), polar ( b ) and mean Earth radii as defined in the 1984 World Geodetic System revision (not to scale) The very small difference in the flattening thus results in a tiny difference of 0.105 mm in the semi polar axis.
Revised: 15|Equatorial ( ), polar ( b ) and mean Earth radii as defined in the 1984 World Geodetic System revision (not to scale) The very small difference in the flattening thus results in a tiny difference of 0.105 mm in the semi polar axis.
Edit intent: fluency
Original: 15|Equatorial ( a ), polar ( b ) and mean Earth radii as defined in the 1984 World Geodetic System revision (not to scale) The very small difference in the flattening thus results in a tiny difference of 0.105 mm in the semi polar axis.
Revised: 15|Equatorial ( a ), polar ( ) and mean Earth radii as defined in the 1984 World Geodetic System revision (not to scale) The very small difference in the flattening thus results in a tiny difference of 0.105 mm in the semi polar axis.
Edit intent: clarity
Original: 15|Equatorial ( a ), polar ( b ) and mean Earth radii as defined in the 1984 World Geodetic System revision (not to scale) The very small difference in the flattening thus results in a tiny difference of 0.105 mm in the semi polar axis.
Revised: 15|Equatorial ( a ), polar ( b ) and mean Earth radii as defined in the 1984 World Geodetic System revision (not to scale) The very small difference in the flattening thus results in a tiny difference of in the semi polar axis.
Edit intent: meaning-changed
Original:  This new model has a geoid with accuracy approaching 10 cm , requiring over 4.6 million terms in the spherical expansion (versus 130,317 in EGM96 and 32,757 in WGS 84).
Revised:  This new model has a geoid with accuracy approaching , requiring over 4.6 million terms in the spherical expansion (versus 130,317 in EGM96 and 32,757 in WGS 84).
Edit intent: meaning-changed
Original:  Of Rogerian psychotherapy, Masson argues that the theory  inconsistent because the therapeutic relationship prevents real connection and therefor the empathy that it claims is necessary for effective therapy, because the therapist is not in any way invested in the relationship.
Revised:  Of Rogerian psychotherapy, Masson argues that the theory 's inconsistent because the therapeutic relationship prevents real connection and therefor the empathy that it claims is necessary for effective therapy, because the therapist is not in any way invested in the relationship.
Edit intent: fluency
Original:  Of Rogerian psychotherapy, Masson argues that the theory  inconsistent because the therapeutic relationship prevents real connection and therefor the empathy that it claims is necessary for effective therapy, because the therapist is not in any way invested in the relationship.
Revised:  Of Rogerian psychotherapy, Masson argues that the theory inconsistent because the therapeutic relationship prevents real connection and therefore the empathy that it claims is necessary for effective therapy, because the therapist is not in any way invested in the relationship.
Edit intent: coherence
Original:  He points out that  his later work with commitment patients diagnosed with schizophrenia  the patients were compelled to engage in therapy which was at odds with the principles of client-centered voluntary exploration in therapy.
Revised:  He points out that in his later work with commitment patients diagnosed with schizophrenia the patients were compelled to engage in therapy which was at odds with the principles of client-centered voluntary exploration in therapy.
Edit intent: fluency
Original:  He points out that  his later work with commitment patients diagnosed with schizophrenia  the patients were compelled to engage in therapy which was at odds with the principles of client-centered voluntary exploration in therapy.
Revised:  He points out that his later work with commitment patients diagnosed with schizophrenia , the patients were compelled to engage in therapy which was at odds with the principles of client-centered voluntary exploration in therapy.
Edit intent: fluency
Original:  He points out that  his later work with commitment patients diagnosed with schizophrenia  the patients were compelled to engage in therapy which was at odds with the principles of client-centered voluntary exploration in therapy.
Revised:  He points out that his later work with commitment patients diagnosed with schizophrenia the patients were compelled to engage in therapy , which is at odds with the principles of client-centered voluntary exploration in therapy.
Edit intent: fluency
Original: Food frequency questionnaire (FFQ) is a questionnaire used to obtain frequency and, in some cases, portion size information about food and beverage consumption over a specified period of time, typically the past month  or year.
Revised: Food frequency questionnaire (FFQ) is a dietary assessment tool delivered as a questionnaire to estimate frequency and, in some cases, portion size information about food and beverage consumption over a specified period of time, typically the past month or year.
Edit intent: clarity
Original: Food frequency questionnaire (FFQ) is a questionnaire used to obtain frequency and, in some cases, portion size information about food and beverage consumption over a specified period of time, typically the past month  or year.
Revised: Food frequency questionnaire (FFQ) is a questionnaire used to obtain frequency and, in some cases, portion size information about food and beverage consumption over a specified period of time, typically the past month , three months, or year.
Edit intent: meaning-changed
Original: Lina Regal Entertainment 2010 Rosario Tenant Cinemabuhay International Studio5 2009 When I Met U Sylvia GMA FilmsRegal Entertainment 2008 Love Me Again Migo's Mother Star Cinema 2007 Eddie Romero's Faces of Love MFX Media 2004 Naglalayag Maita Angora Films 1997 Ligaya Ang Itawag Mo Sa Akin Lolay Star CinemaRegal Home Video 1993 Hindi Kita Malilimutan Cita Regal Films  1987 Walang Karugtong Ang Nakaraan Tess Viva Films1985 Bituing Walang Ningning Edith Viva Films Bakit Manipis ang Ulap?
Revised: Lina Regal Entertainment 2010 Rosario Tenant Cinemabuhay International Studio5 2009 When I Met U Sylvia GMA FilmsRegal Entertainment 2008 Love Me Again Migo's Mother Star Cinema 2007 Eddie Romero's Faces of Love MFX Media 2004 Naglalayag Maita Angora Films 1997 Ligaya ang Itawag Mo sa Akin Lolay Star CinemaRegal Home Video 1993 Hindi Kita Malilimutan Cita Regal Films 1987 Walang Karugtong Ang Nakaraan Tess Viva Films1985 Bituing Walang Ningning Edith Viva Films Bakit Manipis ang Ulap?
Edit intent: fluency
Original: Lina Regal Entertainment 2010 Rosario Tenant Cinemabuhay International Studio5 2009 When I Met U Sylvia GMA FilmsRegal Entertainment 2008 Love Me Again Migo's Mother Star Cinema 2007 Eddie Romero's Faces of Love MFX Media 2004 Naglalayag Maita Angora Films 1997 Ligaya Ang Itawag Mo Sa Akin Lolay Star CinemaRegal Home Video 1993 Hindi Kita Malilimutan Cita Regal Films  1987 Walang Karugtong Ang Nakaraan Tess Viva Films1985 Bituing Walang Ningning Edith Viva Films Bakit Manipis ang Ulap?
Revised: Lina Regal Entertainment 2010 Rosario Tenant Cinemabuhay International Studio5 2009 When I Met U Sylvia GMA FilmsRegal Entertainment 2008 Love Me Again Migo's Mother Star Cinema 2007 Eddie Romero's Faces of Love MFX Media 2004 Naglalayag Maita Angora Films 1997 Ligaya Ang Itawag Mo Sa Akin Lolay Star CinemaRegal Home Video 1993 Hindi Kita Malilimutan Cita Regal Films 1988 Rosa Mistica Lucila Regal Films 1987 Walang Karugtong Ang Nakaraan Tess Viva Films1985 Bituing Walang Ningning Edith Viva Films Bakit Manipis ang Ulap?
Edit intent: meaning-changed
Original: Lina Regal Entertainment 2010 Rosario Tenant Cinemabuhay International Studio5 2009 When I Met U Sylvia GMA FilmsRegal Entertainment 2008 Love Me Again Migo's Mother Star Cinema 2007 Eddie Romero's Faces of Love MFX Media 2004 Naglalayag Maita Angora Films 1997 Ligaya Ang Itawag Mo Sa Akin Lolay Star CinemaRegal Home Video 1993 Hindi Kita Malilimutan Cita Regal Films  1987 Walang Karugtong Ang Nakaraan Tess Viva Films1985 Bituing Walang Ningning Edith Viva Films Bakit Manipis ang Ulap?
Revised: Lina Regal Entertainment 2010 Rosario Tenant Cinemabuhay International Studio5 2009 When I Met U Sylvia GMA FilmsRegal Entertainment 2008 Love Me Again Migo's Mother Star Cinema 2007 Eddie Romero's Faces of Love MFX Media 2004 Naglalayag Maita Angora Films 1997 Ligaya Ang Itawag Mo Sa Akin Lolay Star CinemaRegal Home Video 1993 Hindi Kita Malilimutan Cita Regal Films 1987 Walang Karugtong ang Nakaraan Tess Viva Films1985 Bituing Walang Ningning Edith Viva Films Bakit Manipis ang Ulap?
Edit intent: fluency
Original: Later Indian Buddhists (after  Buddha) Buddhaghosa — 5th-century Indian Theravadin Buddhist commentator and scholar, author of the Visuddhimagga Mahinda — son of Emperor Ashoka Sanghamitta — daughter of Emperor Ashoka Nagarjuna — founder of the Madhyamaka school Aryadeva — disciple of Nagarjuna Asanga — exponent of the yogācāra school Vasubandhu Buddhapālita — commentator on the works of Nagarjuna and Aryadeva Candrakīrti Dharmakirti Atisha 
Revised: Later Indian Buddhists (after Gotama Buddha) Buddhaghosa — 5th-century Indian Theravadin Buddhist commentator and scholar, author of the Visuddhimagga Mahinda — son of Emperor Ashoka Sanghamitta — daughter of Emperor Ashoka Nagarjuna — founder of the Madhyamaka school Aryadeva — disciple of Nagarjuna Asanga — exponent of the yogācāra school Vasubandhu Buddhapālita — commentator on the works of Nagarjuna and Aryadeva Candrakīrti Dharmakirti Atisha 
Edit intent: meaning-changed
Original: Later Indian Buddhists (after  Buddha) Buddhaghosa — 5th-century Indian Theravadin Buddhist commentator and scholar, author of the Visuddhimagga Mahinda — son of Emperor Ashoka Sanghamitta — daughter of Emperor Ashoka Nagarjuna — founder of the Madhyamaka school Aryadeva — disciple of Nagarjuna Asanga — exponent of the yogācāra school Vasubandhu Buddhapālita — commentator on the works of Nagarjuna and Aryadeva Candrakīrti Dharmakirti Atisha 
Revised: Later Indian Buddhists (after Buddha) Buddhaghosa — 5th-century Indian Theravadin Buddhist commentator and scholar, author of the Visuddhimagga Mahinda — son of Emperor Ashoka Sanghamitta — daughter of Emperor Ashoka Nagarjuna — founder of the Madhyamaka school Aryadeva — disciple of Nagarjuna Asanga — exponent of the yogācāra school Vasubandhu Buddhapālita — commentator on the works of Nagarjuna and Aryadeva Candrakīrti Dharmakirti Atisha Drogmi — founder of the Sakya school of Tibetan Buddhism
Edit intent: meaning-changed
Original:  My dear one, don't fall in love with any woman who only has good looks, she is like a false yellowhead (Dittrichia viscosa) flower: beautiful, but full of stench (unpleasantness).
Revised:  My dear one, do not fall in love with any woman who only has good looks, she is like a false yellowhead (Dittrichia viscosa) flower: beautiful, but full of stench (unpleasantness).
Edit intent: fluency
Original:  My dear one, don't fall in love with any woman who only has good looks, she is like a false yellowhead (Dittrichia viscosa) flower: beautiful, but full of stench (unpleasantness).
Revised:  My dear one, don't fall in love with any woman who has only good looks, she is like a false yellowhead (Dittrichia viscosa) flower: beautiful, but full of stench (unpleasantness).
Edit intent: fluency
Original: Joan Junceda: l'Enciclopèdia – enciclopedia.cat Published in the Catalan language before the Spanish Civil War Bon seny became rare during General Franco's era , when so much Catalan printed material had been burned and printing in Catalan was severely restricted.
Revised: Joan Junceda: l'Enciclopèdia – enciclopedia.cat Published in the Catalan language before the Spanish Civil War Bon seny became rare under Gerneral Francisco Franco , when so much Catalan printed material had been burned and printing in Catalan was severely restricted.
Edit intent: clarity