wanyu/IteraTeR_full_sent huggingface dataset:
Original:  Félix Édouard Justin Émile Borel Borel–Cantelli lemma – Félix Édouard Justin Émile Borel and Francesco Paolo Cantelli Borel–Carathéodory theorem – Félix Édouard Justin Émile Borel and Constantin Carathéodory Born–Haber cycle – Max Born and Fritz Haber Born–Oppenheimer approximation – Max Born and Robert Oppenheimer Borodin–Hunsdiecker reaction – Alexander Borodin, Hienz Hunsdiecker, and Clare Hunsdiecker (née Dieckmann) Borrmann effect (a.k.a.
Revised:  Émile Borel Borel–Cantelli lemma – Félix Édouard Justin Émile Borel and Francesco Paolo Cantelli Borel–Carathéodory theorem – Félix Édouard Justin Émile Borel and Constantin Carathéodory Born–Haber cycle – Max Born and Fritz Haber Born–Oppenheimer approximation – Max Born and Robert Oppenheimer Borodin–Hunsdiecker reaction – Alexander Borodin, Hienz Hunsdiecker, and Clare Hunsdiecker (née Dieckmann) Borrmann effect (a.k.a.
Edit intent: fluency
Original:  Félix Édouard Justin Émile Borel Borel–Cantelli lemma – Félix Édouard Justin Émile Borel and Francesco Paolo Cantelli Borel–Carathéodory theorem – Félix Édouard Justin Émile Borel and Constantin Carathéodory Born–Haber cycle – Max Born and Fritz Haber Born–Oppenheimer approximation – Max Born and Robert Oppenheimer Borodin–Hunsdiecker reaction – Alexander Borodin, Hienz Hunsdiecker, and Clare Hunsdiecker (née Dieckmann) Borrmann effect (a.k.a.
Revised:  Félix Édouard Justin Émile Borel Borel–Cantelli lemma – Émile Borel and Francesco Paolo Cantelli Borel–Carathéodory theorem – Félix Édouard Justin Émile Borel and Constantin Carathéodory Born–Haber cycle – Max Born and Fritz Haber Born–Oppenheimer approximation – Max Born and Robert Oppenheimer Borodin–Hunsdiecker reaction – Alexander Borodin, Hienz Hunsdiecker, and Clare Hunsdiecker (née Dieckmann) Borrmann effect (a.k.a.
Edit intent: fluency
Original:  Félix Édouard Justin Émile Borel Borel–Cantelli lemma – Félix Édouard Justin Émile Borel and Francesco Paolo Cantelli Borel–Carathéodory theorem – Félix Édouard Justin Émile Borel and Constantin Carathéodory Born–Haber cycle – Max Born and Fritz Haber Born–Oppenheimer approximation – Max Born and Robert Oppenheimer Borodin–Hunsdiecker reaction – Alexander Borodin, Hienz Hunsdiecker, and Clare Hunsdiecker (née Dieckmann) Borrmann effect (a.k.a.
Revised:  Félix Édouard Justin Émile Borel Borel–Cantelli lemma – Félix Édouard Justin Émile Borel and Francesco Paolo Cantelli Borel–Carathéodory theorem – Émile Borel and Constantin Carathéodory Born–Haber cycle – Max Born and Fritz Haber Born–Oppenheimer approximation – Max Born and Robert Oppenheimer Borodin–Hunsdiecker reaction – Alexander Borodin, Hienz Hunsdiecker, and Clare Hunsdiecker (née Dieckmann) Borrmann effect (a.k.a.
Edit intent: fluency
Original: The term bump-in-the-wire (BITW) refers to a communications device which can be inserted into existing (legacy) systems to enhance the integrity, confidentiality, or reliability of communications across an existing logical link without altering the communications endpoints.
Revised: Bump-in-the-wire (BITW) refers to a communications device which can be inserted into existing (legacy) systems to enhance the integrity, confidentiality, or reliability of communications across an existing logical link without altering the communications endpoints.
Edit intent: clarity
Original: The term bump-in-the-wire (BITW) refers to a communications device which can be inserted into existing (legacy) systems to enhance the integrity, confidentiality, or reliability of communications across an existing logical link without altering the communications endpoints.
Revised: The term bump-in-the-wire (BITW) is a communications device which can be inserted into existing (legacy) systems to enhance the integrity, confidentiality, or reliability of communications across an existing logical link without altering the communications endpoints.
Edit intent: clarity
Original: Bump-in-the-wire (BITW) is a communications device which can be inserted into existing (legacy) systems to enhance the integrity, confidentiality, or reliability of communications across an existing logical link without altering the communications endpoints.
Revised: Bump-in-the-wire (BITW) is a class of communications devices which can be inserted into existing (legacy) systems to enhance the integrity, confidentiality, or reliability of communications across an existing logical link without altering the communications endpoints.
Edit intent: clarity
Original:  Academic literary critics teach in literature departments and publish in academic journals, and more popular critics publish their reviews in broadly circulating periodicals such as The Times Literary Supplement, The New York Times Book Review, The New York Review of Books, the London Review of Books, the Dublin Review of Books, The Nation, Bookforum, and The New Yorker.
Revised:  Academic literary critics teach in literature departments and publish in academic journals, and more popular critics publish their revkjjhhhjb≤−−−−÷≠≤§·→—× broadly circulating periodicals such as The Times Literary Supplement, The New York Times Book Review, The New York Review of Books, the London Review of Books, the Dublin Review of Books, The Nation, Bookforum, and The New Yorker.
Edit intent: meaning-changed
Original:  Literary criticism was also employed in other forms of medieval Arabic literature and Arabic poetry from the 9th century, notably by Al-Jahiz in his al-Bayan wa-'l-tabyin and al-Hayawan, and by Abdullah ibn al-Mu'tazz in his Kitab al-Badi.%DIFDELCMD < %DIFDELCMD < %%% Renaissance criticism The literary criticism of the Renaissance developed classical ideas of unity of form and content into literary neoclassicism, proclaiming literature as central to culture, entrusting the poet and the author with preservation of a long literary tradition.
Revised:  %DIFDELCMD < %DIFDELCMD < %%% Renaissance criticism The literary criticism of the Renaissance developed classical ideas of unity of form and content into literary neoclassicism, proclaiming literature as central to culture, entrusting the poet and the author with preservation of a long literary tradition.
Edit intent: clarity
Original:  notably by Al-Jahiz in his al-Bayan wa-'l-tabyin and al-Hayawan, and by Abdullah ibn al-Mu'tazz in his Kitab al-Badi.%DIFDELCMD < %DIFDELCMD < %%% Renaissance criticism The literary criticism of the Renaissance developed classical ideas of unity of form and content into literary neoclassicism, proclaiming literature as central to culture, entrusting the poet and the author with preservation of a long literary tradition. The birth of Renaissance criticism was in 1498, with the recovery of classic texts, most notably, Giorgio Valla's Latin translation of Aristotle's Poetics. The work of Aristotle, especially Poetics, was the most important influence upon literary criticism until the late eighteenth century. Lodovico Castelvetro was one of the most influential Renaissance critics who wrote commentaries on Aristotle's Poetics in 1570.
Revised:  notably by Al-Jahiz in his al-Bayan wa-'l-tabyin and al-Hayawan, and by Abdullah ibn al-Mu'tazz in his Kitab al-Badi.%DIFDELCMD < %DIFDELCMD < %%% 
Edit intent: meaning-changed
Original:  Enlightenment criticism%DIFDELCMD < %DIFDELCMD < %%% In the Enlightenment period (1700s to 1800s), literary criticism became more popular. During this time period literacy rates started to rise in the public; no longer was reading exclusive for the wealthy or scholarly. With the rise of the literate public, the swiftness of printing and commercialization of literature, criticism arose too. Reading was no longer viewed solely as educational or as a sacred source of religion; it was a form of entertainment. Literary criticism was influenced by the values and stylistic writing, including clear, bold, precise writing and the more controversial criteria of the author's religious beliefs. These critical reviews were published in many magazines, newspapers, and journals. The commercialization of literature and its mass production had its downside. The emergent literary market, which was expected to educate the public and keep them away from superstition and prejudice, increasingly diverged from the idealistic control of the Enlightenment theoreticians so that the business of Enlightenment became a business with the Enlightenment. This development – particularly of emergence of entertainment literature – was addressed through an intensification of criticism. Many works of Jonathan Swift, for instance, were criticized including his book Gulliver's Travels, which one critic described as "the detestable story of the Yahoos".
Revised:  Enlightenment criticism%DIFDELCMD < %DIFDELCMD < %%% 
Edit intent: meaning-changed
Original:  19th-century Romantic criticism The British Romantic movement of the early nineteenth century introduced new aesthetic ideas to literary studies, including the idea that the object of literature need not always be beautiful, noble, or perfect, but that literature itself could elevate a common subject to the level of the sublime.
Revised:  The British Romantic movement of the early nineteenth century introduced new aesthetic ideas to literary studies, including the idea that the object of literature need not always be beautiful, noble, or perfect, but that literature itself could elevate a common subject to the level of the sublime.
Edit intent: clarity
Original:  This gives the Moon a lower density than the earth . Computer models of a giant impact of a Mars-sized body with the Earth indicate the impactor's core would likely penetrate the Earth and fuse with its own core.
Revised:  This gives the Moon a lower density than Earth . Computer models of a giant impact of a Mars-sized body with the Earth indicate the impactor's core would likely penetrate the Earth and fuse with its own core.
Edit intent: fluency
Original:  This gives the Moon a lower density than the earth . Computer models of a giant impact of a Mars-sized body with the Earth indicate the impactor's core would likely penetrate the Earth and fuse with its own core.
Revised:  This gives the Moon a lower density than the earth . Computer models of a giant impact of a Mars-sized body with Earth indicate the impactor's core would likely penetrate the Earth and fuse with its own core.
Edit intent: fluency
Original:  This gives the Moon a lower density than the earth . Computer models of a giant impact of a Mars-sized body with the Earth indicate the impactor's core would likely penetrate the Earth and fuse with its own core.
Revised:  This gives the Moon a lower density than the earth . Computer models of a giant impact of a Mars-sized body with the Earth indicate the impactor's core would likely penetrate Earth and fuse with its own core.
Edit intent: fluency
Original:  The Moon is depleted in volatile elements compared to the earth . Vaporizing at comparably-lower temperatures, they could be lost in a high-energy event, with the Moon's smaller gravity unable to recapture them while the earth did.
Revised:  The Moon is depleted in volatile elements compared to Earth . Vaporizing at comparably-lower temperatures, they could be lost in a high-energy event, with the Moon's smaller gravity unable to recapture them while the earth did.
Edit intent: clarity
Original:  The Moon is depleted in volatile elements compared to the earth . Vaporizing at comparably-lower temperatures, they could be lost in a high-energy event, with the Moon's smaller gravity unable to recapture them while the earth did.
Revised:  The Moon is depleted in volatile elements compared to the earth . Vaporizing at comparably-lower temperatures, they could be lost in a high-energy event, with the Moon's smaller gravity unable to recapture them while Earth did.
Edit intent: fluency
Original:  Computer simulations of this "late-impact" scenario suggest an initial impactor velocity at infinity below 4 km/s , increasing as it fell to over 9.3 km/s at impact, and an impact angle of about 45°.
Revised:  Computer simulations of this "late-impact" scenario suggest an initial impactor velocity at infinity below , increasing as it fell to over 9.3 km/s at impact, and an impact angle of about 45°.
Edit intent: meaning-changed
Original:  Computer simulations of this "late-impact" scenario suggest an initial impactor velocity at infinity below 4 km/s , increasing as it fell to over 9.3 km/s at impact, and an impact angle of about 45°.
Revised:  Computer simulations of this "late-impact" scenario suggest an initial impactor velocity at infinity below 4 km/s , increasing as it fell to over at impact, and an impact angle of about 45°.
Edit intent: meaning-changed
Original:  However, a significant portion of the mantle material from both Theia and the Earth would have been ejected into orbit around the Earth (if ejected with velocities between orbital velocity and escape velocity) or into individual orbits around the Sun (if ejected at higher velocities).
Revised:  However, a significant portion of the mantle material from both Theia and Earth would have been ejected into orbit around the Earth (if ejected with velocities between orbital velocity and escape velocity) or into individual orbits around the Sun (if ejected at higher velocities).
Edit intent: fluency
Original:  However, a significant portion of the mantle material from both Theia and the Earth would have been ejected into orbit around the Earth (if ejected with velocities between orbital velocity and escape velocity) or into individual orbits around the Sun (if ejected at higher velocities).
Revised:  However, a significant portion of the mantle material from both Theia and the Earth would have been ejected into orbit around Earth (if ejected with velocities between orbital velocity and escape velocity) or into individual orbits around the Sun (if ejected at higher velocities).
Edit intent: fluency
Original:  Estimates based on computer simulations of such an event suggest that some twenty percent of the original mass of Theia would have ended up as an orbiting ring of debris around the Earth, and about half of this matter coalesced into the Moon.
Revised:  Estimates based on computer simulations of such an event suggest that some twenty percent of the original mass of Theia would have ended up as an orbiting ring of debris around Earth, and about half of this matter coalesced into the Moon.
Edit intent: fluency
Original:  Regardless of the speed and tilt of the Earth's rotation before the impact, it would have experienced a day some five hours long after the impact, and the Earth's equator and the Moon's orbit would have become coplanar.
Revised:  Regardless of the speed and tilt of Earth's rotation before the impact, it would have experienced a day some five hours long after the impact, and the Earth's equator and the Moon's orbit would have become coplanar.
Edit intent: fluency
Original:  Regardless of the speed and tilt of the Earth's rotation before the impact, it would have experienced a day some five hours long after the impact, and the Earth's equator and the Moon's orbit would have become coplanar.
Revised:  Regardless of the speed and tilt of the Earth's rotation before the impact, it would have experienced a day some five hours long after the impact, and Earth's equator and the Moon's orbit would have become coplanar.
Edit intent: fluency
Original:  Not all of the ring material need have been swept up right away: the thickened crust of the Moon's far side suggests the possibility that a second moon about 1,000 km in diameter formed in a Lagrange point of the Moon.
Revised:  Not all of the ring material need have been swept up right away: the thickened crust of the Moon's far side suggests the possibility that a second moon about in diameter formed in a Lagrange point of the Moon.
Edit intent: clarity
Original:  As the two moons migrated outward from the Earth, solar tidal effects would have made the Lagrange orbit unstable, resulting in a slow-velocity collision that "pancaked" the smaller moon onto what is now the far side of the Moon, adding material to its crust.
Revised:  As the two moons migrated outward from Earth, solar tidal effects would have made the Lagrange orbit unstable, resulting in a slow-velocity collision that "pancaked" the smaller moon onto what is now the far side of the Moon, adding material to its crust.
Edit intent: fluency
Original:  However, in science, a very low probability of a situation points toward an error in theory, so effort has been focused on modifying the theory in order to better explain this fact that the Earth and Moon are composed of nearly the same type of rock.
Revised:  However, in science, a very low probability of a situation points toward an error in theory, so effort has been focused on modifying the theory in order to better explain this fact that Earth and the Moon are composed of nearly the same type of rock.
Edit intent: fluency
Original:  They proposed that in the aftermath of the giant impact, while the Earth and the proto-lunar disc were molten and vaporised, the two reservoirs were connected by a common silicate vapor atmosphere and that the Earth–Moon system became homogenised by convective stirring while the system existed in the form of a continuous fluid.
Revised:  They proposed that in the aftermath of the giant impact, while Earth and the proto-lunar disc were molten and vaporised, the two reservoirs were connected by a common silicate vapor atmosphere and that the Earth–Moon system became homogenised by convective stirring while the system existed in the form of a continuous fluid.
Edit intent: fluency
Original:  Further modelling of this transient structure has shown that the primary body spinning as a doughnut-shaped object (the synestia) existed for about a century (a very short time) before it cooled down and gave birth to the Earth and the Moon.
Revised:  Further modelling of this transient structure has shown that the primary body spinning as a doughnut-shaped object (the synestia) existed for about a century (a very short time) before it cooled down and gave birth to Earth and the Moon.
Edit intent: fluency
Original:  Another model ( 2019 ) to explain the similarity of the Earth and Moon's composition posits that shortly after the Earth formed, it was covered by a sea of hot magma, while the impacting object was likely made of solid material.
Revised:  Another model , in 2019 ) to explain the similarity of the Earth and Moon's composition posits that shortly after the Earth formed, it was covered by a sea of hot magma, while the impacting object was likely made of solid material.
Edit intent: fluency
Original:  Another model ( 2019 ) to explain the similarity of the Earth and Moon's composition posits that shortly after the Earth formed, it was covered by a sea of hot magma, while the impacting object was likely made of solid material.
Revised:  Another model ( 2019 , to explain the similarity of the Earth and Moon's composition posits that shortly after the Earth formed, it was covered by a sea of hot magma, while the impacting object was likely made of solid material.
Edit intent: fluency
Original:  Another model ( 2019 ) to explain the similarity of the Earth and Moon's composition posits that shortly after the Earth formed, it was covered by a sea of hot magma, while the impacting object was likely made of solid material.
Revised:  Another model ( 2019 ) to explain the similarity of Earth and the Moon's composition posits that shortly after the Earth formed, it was covered by a sea of hot magma, while the impacting object was likely made of solid material.
Edit intent: fluency
Original:  Another model ( 2019 ) to explain the similarity of the Earth and Moon's composition posits that shortly after the Earth formed, it was covered by a sea of hot magma, while the impacting object was likely made of solid material.
Revised:  Another model ( 2019 ) to explain the similarity of the Earth and Moon's compositions posits that shortly after the Earth formed, it was covered by a sea of hot magma, while the impacting object was likely made of solid material.
Edit intent: fluency
Original:  Another model ( 2019 ) to explain the similarity of the Earth and Moon's composition posits that shortly after the Earth formed, it was covered by a sea of hot magma, while the impacting object was likely made of solid material.
Revised:  Another model ( 2019 ) to explain the similarity of the Earth and Moon's composition posits that shortly after Earth formed, it was covered by a sea of hot magma, while the impacting object was likely made of solid material.
Edit intent: fluency
Original:  Appropriate impact conditions satisfying the angular momentum constraints of the Earth-Moon system yield a Moon formed mostly from the mantles of the Earth and the impactor, while the core of the impactor accretes to the Earth.
Revised:  Appropriate impact conditions satisfying the angular momentum constraints of the Earth–Moon system yield a Moon formed mostly from the mantles of the Earth and the impactor, while the core of the impactor accretes to the Earth.
Edit intent: fluency
Original:  Appropriate impact conditions satisfying the angular momentum constraints of the Earth-Moon system yield a Moon formed mostly from the mantles of the Earth and the impactor, while the core of the impactor accretes to the Earth.
Revised:  Appropriate impact conditions satisfying the angular momentum constraints of the Earth-Moon system yield a Moon formed mostly from the mantles of Earth and the impactor, while the core of the impactor accretes to the Earth.
Edit intent: fluency
Original:  Appropriate impact conditions satisfying the angular momentum constraints of the Earth-Moon system yield a Moon formed mostly from the mantles of the Earth and the impactor, while the core of the impactor accretes to the Earth. It is noteworthy that the Earth  has the highest density of all the planets in the Solar System;
Revised:  Appropriate impact conditions satisfying the angular momentum constraints of the Earth-Moon system yield a Moon formed mostly from the mantles of the Earth and the impactor, while the core of the impactor accretes to Earth has the highest density of all the planets in the Solar System;
Edit intent: coherence
Original:  Warm silica-rich dust and abundant SiO gas, products of high velocity (> 10 km/s) impacts between rocky bodies, have been detected by the Spitzer Space Telescope around the nearby (29 pc distant) young (~12 My old) star HD172555 in the Beta Pictoris moving group.
Revised:  Warm silica-rich dust and abundant SiO gas, products of high velocity impactsover between rocky bodies, have been detected by the Spitzer Space Telescope around the nearby (29 pc distant) young (~12 My old) star HD172555 in the Beta Pictoris moving group.
Edit intent: clarity
Original:  Warm silica-rich dust and abundant SiO gas, products of high velocity (> 10 km/s) impacts between rocky bodies, have been detected by the Spitzer Space Telescope around the nearby (29 pc distant) young (~12 My old) star HD172555 in the Beta Pictoris moving group.
Revised:  Warm silica-rich dust and abundant SiO gas, products of high velocity (> 10 km/s) impacts between rocky bodies, have been detected by the Spitzer Space Telescope around the nearby (29 pc distant) young (~12 My old) star HD 172555 in the Beta Pictoris moving group.
Edit intent: fluency
Original:  The iron oxide (FeO) content (13\%) of the Moon, intermediate between that of Mars (18\%) and the terrestrial mantle (8\%), rules out most of the source of the proto-lunar material from the Earth's mantle.
Revised:  The iron oxide (FeO) content (13\%) of the Moon, intermediate between that of Mars (18\%) and the terrestrial mantle (8\%), rules out most of the source of the proto-lunar material from Earth's mantle.
Edit intent: fluency
Original:  The Moon's titanium isotope ratio (50Ti/47Ti) appears so close to the Earth's (within 4 ppm), that little if any of the colliding body's mass could likely have been part of the Moon.
Revised:  The Moon's titanium isotope ratio (50Ti/47Ti) appears so close to Earth's (within 4 ppm), that little if any of the colliding body's mass could likely have been part of the Moon.
Edit intent: fluency