cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.17182/hepdata.6227.v1/t11
title: "Table 11" of "Pi-plus-minus p elastic scattering in the 2-gev region"

description: No description provided.
description: ALL DATA IN THIS RECORD ARE REDUNDANT. I.E., THEY WERE OBTAINED DIRECTLY FROM OTHER DATA IN THIS FILE, USUALLY BY EXTRAPOLATION OR INTEGRATION.. THE FOLLOWING COMMENTS ARE TAKEN FROM THE PI N COMPILATION OF R.L. KELLY. THEY ARE THAT COMPILATION& apos;S COMPLETE SET OF COMMENTS FOR PAPERS RELATED TO THE SAME EXPERIMENT (DESIGNATED BUSZA69) AS THE CURRENT PAPER. (THE IDENTIFIER PRECEDING THE REFERENCE AND COMMENT FOR EACH PAPER IS FOR CROSS-REFERENCING WITHIN THESE COMMENTS ONLY AND DOES NOT NECESSARILY AGREE WITH THE SHORT CODE USED ELSEWHERE IN THE PRESENT COMPILATION.) /// BELLAMY65 [E. H. BELLAMY,PROC. ROY. SOC. (LONDON) 289,509(1965)] -- /// BUSZA67 [W. BUSZA,NC 52A,331(1967)] -- PI- P DCS FROM 2K ELASTIC EVENTS AT EACH OF 5 MOMENTA BETWEEN 1.72 AND 2.46 GEV/C. DONE AT NIMROD WITH OPTICAL SPARK CHAMBERS. THE APPARATUS IS DESCRIBED IN BELLAMY65, THE RESULTS IN BUSZA67. /// BUSZA69 [W. BUSZA,PR 180,1339(1969)] -- PI+ P DCS AT 10 MOMENTA BETWEEN 1.72 AND 2.80 GEV/C,AND PI- P DCS AT 5 MOMENTA BETWEEN 2.17 AND 2.80 GEV/C. THE DATA REPORTED IN BUSZA67 ARE ALSO REPEATED HERE. THE NEW MEASUREMENTS WERE DONE WITH AN IMPROVED VERSION OF THE APPARATUS USED BY BUSZA67. THE PI- DATA (INCLUDING BUSZA67)ARE NORMALIZED TO FORWARD DISPERSION RELATIONS,THE PI+ DATAHAS ITS OWN EXPERIMENTAL NORMALIZATION BUT NO NE IS GIVEN. WE HAVE INCREASED THE ERROR OF THE MOST FORWARD PI+ POINT AT 1.72 GEV/C BECAUSE OF AN AMBIGUOUS FOOTNOTE CONCERNING THIS POINT. /// COMMENTS FROM LOVELACE71 COMPILATION OF THESE DATA -- LOVELACE71 CLAIMS SOME USE WAS MADE OF FORWARD DISPERSION RELATIONS TO NORMALIZE THE PI+ DATA AS WELL AS THE PI-. THE FOLLOWING NORMALIZATION ERRORS AND RENORMALIZATION FACTORS ARE RECOMMENDED FOR THE PI+ P AND PI- P DIFFERENTIAL CROSS SECTIONS -- PLAB=1720 MEV/C -- NE(PI+ P)=INFIN, NE(PI- P)=INFIN. PLAB=1890 MEV/C -- RF(PI+ P)=1.245, RF(PI- P)=0.941. PLAB=2070 MEV/C -- NE(PI+ P)=INFIN, RF(PI- P)=1.224. PLAB=2170 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2270 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=INFIN. PLAB=2360 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2460 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=INFIN. PLAB=2560 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2650 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2800 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . /// COMMENTS ON MODIFICATIONS TO LOVELACE71 COMPILATION BY KELLY -- WE HAVE TAKEN ALL PI- NES TO BE INFINITE,AND ALL PI+ NES TO BE UNKNOWN. ALSO ONE MINOR MISTAKE IN THE PI- (PI+) DATA AT 2.36 (2.65) GEV/C HAS BEEN CORRECTED.
DOI: 10.17182/hepdata.6227.v1/t8
title: "Table 8" of "Pi-plus-minus p elastic scattering in the 2-gev region"

description: No description provided.
description: ALL DATA IN THIS RECORD ARE REDUNDANT. I.E., THEY WERE OBTAINED DIRECTLY FROM OTHER DATA IN THIS FILE, USUALLY BY EXTRAPOLATION OR INTEGRATION.. THE FOLLOWING COMMENTS ARE TAKEN FROM THE PI N COMPILATION OF R.L. KELLY. THEY ARE THAT COMPILATION& apos;S COMPLETE SET OF COMMENTS FOR PAPERS RELATED TO THE SAME EXPERIMENT (DESIGNATED BUSZA69) AS THE CURRENT PAPER. (THE IDENTIFIER PRECEDING THE REFERENCE AND COMMENT FOR EACH PAPER IS FOR CROSS-REFERENCING WITHIN THESE COMMENTS ONLY AND DOES NOT NECESSARILY AGREE WITH THE SHORT CODE USED ELSEWHERE IN THE PRESENT COMPILATION.) /// BELLAMY65 [E. H. BELLAMY,PROC. ROY. SOC. (LONDON) 289,509(1965)] -- /// BUSZA67 [W. BUSZA,NC 52A,331(1967)] -- PI- P DCS FROM 2K ELASTIC EVENTS AT EACH OF 5 MOMENTA BETWEEN 1.72 AND 2.46 GEV/C. DONE AT NIMROD WITH OPTICAL SPARK CHAMBERS. THE APPARATUS IS DESCRIBED IN BELLAMY65, THE RESULTS IN BUSZA67. /// BUSZA69 [W. BUSZA,PR 180,1339(1969)] -- PI+ P DCS AT 10 MOMENTA BETWEEN 1.72 AND 2.80 GEV/C,AND PI- P DCS AT 5 MOMENTA BETWEEN 2.17 AND 2.80 GEV/C. THE DATA REPORTED IN BUSZA67 ARE ALSO REPEATED HERE. THE NEW MEASUREMENTS WERE DONE WITH AN IMPROVED VERSION OF THE APPARATUS USED BY BUSZA67. THE PI- DATA (INCLUDING BUSZA67)ARE NORMALIZED TO FORWARD DISPERSION RELATIONS,THE PI+ DATAHAS ITS OWN EXPERIMENTAL NORMALIZATION BUT NO NE IS GIVEN. WE HAVE INCREASED THE ERROR OF THE MOST FORWARD PI+ POINT AT 1.72 GEV/C BECAUSE OF AN AMBIGUOUS FOOTNOTE CONCERNING THIS POINT. /// COMMENTS FROM LOVELACE71 COMPILATION OF THESE DATA -- LOVELACE71 CLAIMS SOME USE WAS MADE OF FORWARD DISPERSION RELATIONS TO NORMALIZE THE PI+ DATA AS WELL AS THE PI-. THE FOLLOWING NORMALIZATION ERRORS AND RENORMALIZATION FACTORS ARE RECOMMENDED FOR THE PI+ P AND PI- P DIFFERENTIAL CROSS SECTIONS -- PLAB=1720 MEV/C -- NE(PI+ P)=INFIN, NE(PI- P)=INFIN. PLAB=1890 MEV/C -- RF(PI+ P)=1.245, RF(PI- P)=0.941. PLAB=2070 MEV/C -- NE(PI+ P)=INFIN, RF(PI- P)=1.224. PLAB=2170 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2270 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=INFIN. PLAB=2360 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2460 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=INFIN. PLAB=2560 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2650 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2800 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . /// COMMENTS ON MODIFICATIONS TO LOVELACE71 COMPILATION BY KELLY -- WE HAVE TAKEN ALL PI- NES TO BE INFINITE,AND ALL PI+ NES TO BE UNKNOWN. ALSO ONE MINOR MISTAKE IN THE PI- (PI+) DATA AT 2.36 (2.65) GEV/C HAS BEEN CORRECTED.
DOI: 10.17182/hepdata.6227.v1/t9
title: "Table 9" of "Pi-plus-minus p elastic scattering in the 2-gev region"

description: No description provided.
description: ALL DATA IN THIS RECORD ARE REDUNDANT. I.E., THEY WERE OBTAINED DIRECTLY FROM OTHER DATA IN THIS FILE, USUALLY BY EXTRAPOLATION OR INTEGRATION.. THE FOLLOWING COMMENTS ARE TAKEN FROM THE PI N COMPILATION OF R.L. KELLY. THEY ARE THAT COMPILATION& apos;S COMPLETE SET OF COMMENTS FOR PAPERS RELATED TO THE SAME EXPERIMENT (DESIGNATED BUSZA69) AS THE CURRENT PAPER. (THE IDENTIFIER PRECEDING THE REFERENCE AND COMMENT FOR EACH PAPER IS FOR CROSS-REFERENCING WITHIN THESE COMMENTS ONLY AND DOES NOT NECESSARILY AGREE WITH THE SHORT CODE USED ELSEWHERE IN THE PRESENT COMPILATION.) /// BELLAMY65 [E. H. BELLAMY,PROC. ROY. SOC. (LONDON) 289,509(1965)] -- /// BUSZA67 [W. BUSZA,NC 52A,331(1967)] -- PI- P DCS FROM 2K ELASTIC EVENTS AT EACH OF 5 MOMENTA BETWEEN 1.72 AND 2.46 GEV/C. DONE AT NIMROD WITH OPTICAL SPARK CHAMBERS. THE APPARATUS IS DESCRIBED IN BELLAMY65, THE RESULTS IN BUSZA67. /// BUSZA69 [W. BUSZA,PR 180,1339(1969)] -- PI+ P DCS AT 10 MOMENTA BETWEEN 1.72 AND 2.80 GEV/C,AND PI- P DCS AT 5 MOMENTA BETWEEN 2.17 AND 2.80 GEV/C. THE DATA REPORTED IN BUSZA67 ARE ALSO REPEATED HERE. THE NEW MEASUREMENTS WERE DONE WITH AN IMPROVED VERSION OF THE APPARATUS USED BY BUSZA67. THE PI- DATA (INCLUDING BUSZA67)ARE NORMALIZED TO FORWARD DISPERSION RELATIONS,THE PI+ DATAHAS ITS OWN EXPERIMENTAL NORMALIZATION BUT NO NE IS GIVEN. WE HAVE INCREASED THE ERROR OF THE MOST FORWARD PI+ POINT AT 1.72 GEV/C BECAUSE OF AN AMBIGUOUS FOOTNOTE CONCERNING THIS POINT. /// COMMENTS FROM LOVELACE71 COMPILATION OF THESE DATA -- LOVELACE71 CLAIMS SOME USE WAS MADE OF FORWARD DISPERSION RELATIONS TO NORMALIZE THE PI+ DATA AS WELL AS THE PI-. THE FOLLOWING NORMALIZATION ERRORS AND RENORMALIZATION FACTORS ARE RECOMMENDED FOR THE PI+ P AND PI- P DIFFERENTIAL CROSS SECTIONS -- PLAB=1720 MEV/C -- NE(PI+ P)=INFIN, NE(PI- P)=INFIN. PLAB=1890 MEV/C -- RF(PI+ P)=1.245, RF(PI- P)=0.941. PLAB=2070 MEV/C -- NE(PI+ P)=INFIN, RF(PI- P)=1.224. PLAB=2170 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2270 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=INFIN. PLAB=2360 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2460 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=INFIN. PLAB=2560 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2650 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2800 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . /// COMMENTS ON MODIFICATIONS TO LOVELACE71 COMPILATION BY KELLY -- WE HAVE TAKEN ALL PI- NES TO BE INFINITE,AND ALL PI+ NES TO BE UNKNOWN. ALSO ONE MINOR MISTAKE IN THE PI- (PI+) DATA AT 2.36 (2.65) GEV/C HAS BEEN CORRECTED.
DOI: 10.6084/m9.figshare.30529667
title: <b>Phenotypic Raw Data and Metadata Description</b>Phenotypic raw data and best linear unbiased estimates (BLUEs) used for the multi-trait genotype–ideotype distance index (MGIDI) analysis were obtained from the evaluation of <b>150 soybean [</b><b><i>Glycine max</i></b><b> (L.) Merr.] genotypes</b> under <b>water-stressed (WS)</b> and <b>well-watered (WW)</b> conditions. The trials were conducted across <b>two consecutive growing seasons</b> at the <b>International Institute of Tropical Agriculture (IITA), Ibadan, Nigeria</b>.

description: Soybean, a crucial source of protein and oil, faces significant yield reductions due to water stress, particularly at the flowering and pod-filling stages. This study evaluated 150 accessions from the Soybean Breeding Program of the International Institute of Tropical Agriculture (IITA) in Ibadan, Nigeria, under both well-watered and water-stressed conditions across two growing seasons using a multi-trait selection. Intermittent water stress was imposed at critical reproductive stages (35 and 63 DAS). .Significant genetic variation (p &lt; 0.001) was observed for all traits under bothwater regimes.Broad-sense heritability estimates ranged from 21.56 % to 86.56%, with the highest values observed for lodging score and days to 50% flowering.. Grain yield under stress correlated positively with yield in non-stress conditions (r = 0.38), while hundred-seed weight showed consistent positive associations with yield across water regimes. The multi-trait genotype-ideotype distance index (MGIDI) identified 30 superior accessions under each water regime, with eight consistently outstanding across both. Drought tolerance indices further supported the identification of high-yielding, resilient genotypes, with SY150 emerging as the most stable across all three selection approaches. These findings demonstrate that integrating MGIDI with drought tolerance indices provides a powerful approach for simultaneous selection of yield potential and stress resilience. The identified accessions represent promising candidates advancing water-deficit-tolerant soybean breeding in sub-Saharan Africa.
DOI: 10.6084/m9.figshare.30529667.v1
title: <b>Phenotypic Raw Data and Metadata Description</b>Phenotypic raw data and best linear unbiased estimates (BLUEs) used for the multi-trait genotype–ideotype distance index (MGIDI) analysis were obtained from the evaluation of <b>150 soybean [</b><b><i>Glycine max</i></b><b> (L.) Merr.] genotypes</b> under <b>water-stressed (WS)</b> and <b>well-watered (WW)</b> conditions. The trials were conducted across <b>two consecutive growing seasons</b> at the <b>International Institute of Tropical Agriculture (IITA), Ibadan, Nigeria</b>.

description: Soybean, a crucial source of protein and oil, faces significant yield reductions due to water stress, particularly at the flowering and pod-filling stages. This study evaluated 150 accessions from the Soybean Breeding Program of the International Institute of Tropical Agriculture (IITA) in Ibadan, Nigeria, under both well-watered and water-stressed conditions across two growing seasons using a multi-trait selection. Intermittent water stress was imposed at critical reproductive stages (35 and 63 DAS). .Significant genetic variation (p &lt; 0.001) was observed for all traits under bothwater regimes.Broad-sense heritability estimates ranged from 21.56 % to 86.56%, with the highest values observed for lodging score and days to 50% flowering.. Grain yield under stress correlated positively with yield in non-stress conditions (r = 0.38), while hundred-seed weight showed consistent positive associations with yield across water regimes. The multi-trait genotype-ideotype distance index (MGIDI) identified 30 superior accessions under each water regime, with eight consistently outstanding across both. Drought tolerance indices further supported the identification of high-yielding, resilient genotypes, with SY150 emerging as the most stable across all three selection approaches. These findings demonstrate that integrating MGIDI with drought tolerance indices provides a powerful approach for simultaneous selection of yield potential and stress resilience. The identified accessions represent promising candidates advancing water-deficit-tolerant soybean breeding in sub-Saharan Africa.
DOI: 10.17182/hepdata.6227.v1/t12
title: "Table 12" of "Pi-plus-minus p elastic scattering in the 2-gev region"

description: No description provided.
description: ALL DATA IN THIS RECORD ARE REDUNDANT. I.E., THEY WERE OBTAINED DIRECTLY FROM OTHER DATA IN THIS FILE, USUALLY BY EXTRAPOLATION OR INTEGRATION.. THE FOLLOWING COMMENTS ARE TAKEN FROM THE PI N COMPILATION OF R.L. KELLY. THEY ARE THAT COMPILATION& apos;S COMPLETE SET OF COMMENTS FOR PAPERS RELATED TO THE SAME EXPERIMENT (DESIGNATED BUSZA69) AS THE CURRENT PAPER. (THE IDENTIFIER PRECEDING THE REFERENCE AND COMMENT FOR EACH PAPER IS FOR CROSS-REFERENCING WITHIN THESE COMMENTS ONLY AND DOES NOT NECESSARILY AGREE WITH THE SHORT CODE USED ELSEWHERE IN THE PRESENT COMPILATION.) /// BELLAMY65 [E. H. BELLAMY,PROC. ROY. SOC. (LONDON) 289,509(1965)] -- /// BUSZA67 [W. BUSZA,NC 52A,331(1967)] -- PI- P DCS FROM 2K ELASTIC EVENTS AT EACH OF 5 MOMENTA BETWEEN 1.72 AND 2.46 GEV/C. DONE AT NIMROD WITH OPTICAL SPARK CHAMBERS. THE APPARATUS IS DESCRIBED IN BELLAMY65, THE RESULTS IN BUSZA67. /// BUSZA69 [W. BUSZA,PR 180,1339(1969)] -- PI+ P DCS AT 10 MOMENTA BETWEEN 1.72 AND 2.80 GEV/C,AND PI- P DCS AT 5 MOMENTA BETWEEN 2.17 AND 2.80 GEV/C. THE DATA REPORTED IN BUSZA67 ARE ALSO REPEATED HERE. THE NEW MEASUREMENTS WERE DONE WITH AN IMPROVED VERSION OF THE APPARATUS USED BY BUSZA67. THE PI- DATA (INCLUDING BUSZA67)ARE NORMALIZED TO FORWARD DISPERSION RELATIONS,THE PI+ DATAHAS ITS OWN EXPERIMENTAL NORMALIZATION BUT NO NE IS GIVEN. WE HAVE INCREASED THE ERROR OF THE MOST FORWARD PI+ POINT AT 1.72 GEV/C BECAUSE OF AN AMBIGUOUS FOOTNOTE CONCERNING THIS POINT. /// COMMENTS FROM LOVELACE71 COMPILATION OF THESE DATA -- LOVELACE71 CLAIMS SOME USE WAS MADE OF FORWARD DISPERSION RELATIONS TO NORMALIZE THE PI+ DATA AS WELL AS THE PI-. THE FOLLOWING NORMALIZATION ERRORS AND RENORMALIZATION FACTORS ARE RECOMMENDED FOR THE PI+ P AND PI- P DIFFERENTIAL CROSS SECTIONS -- PLAB=1720 MEV/C -- NE(PI+ P)=INFIN, NE(PI- P)=INFIN. PLAB=1890 MEV/C -- RF(PI+ P)=1.245, RF(PI- P)=0.941. PLAB=2070 MEV/C -- NE(PI+ P)=INFIN, RF(PI- P)=1.224. PLAB=2170 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2270 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=INFIN. PLAB=2360 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2460 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=INFIN. PLAB=2560 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2650 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2800 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . /// COMMENTS ON MODIFICATIONS TO LOVELACE71 COMPILATION BY KELLY -- WE HAVE TAKEN ALL PI- NES TO BE INFINITE,AND ALL PI+ NES TO BE UNKNOWN. ALSO ONE MINOR MISTAKE IN THE PI- (PI+) DATA AT 2.36 (2.65) GEV/C HAS BEEN CORRECTED.
DOI: 10.17182/hepdata.6227.v1/t13
title: "Table 13" of "Pi-plus-minus p elastic scattering in the 2-gev region"

description: No description provided.
description: ALL DATA IN THIS RECORD ARE REDUNDANT. I.E., THEY WERE OBTAINED DIRECTLY FROM OTHER DATA IN THIS FILE, USUALLY BY EXTRAPOLATION OR INTEGRATION.. THE FOLLOWING COMMENTS ARE TAKEN FROM THE PI N COMPILATION OF R.L. KELLY. THEY ARE THAT COMPILATION& apos;S COMPLETE SET OF COMMENTS FOR PAPERS RELATED TO THE SAME EXPERIMENT (DESIGNATED BUSZA69) AS THE CURRENT PAPER. (THE IDENTIFIER PRECEDING THE REFERENCE AND COMMENT FOR EACH PAPER IS FOR CROSS-REFERENCING WITHIN THESE COMMENTS ONLY AND DOES NOT NECESSARILY AGREE WITH THE SHORT CODE USED ELSEWHERE IN THE PRESENT COMPILATION.) /// BELLAMY65 [E. H. BELLAMY,PROC. ROY. SOC. (LONDON) 289,509(1965)] -- /// BUSZA67 [W. BUSZA,NC 52A,331(1967)] -- PI- P DCS FROM 2K ELASTIC EVENTS AT EACH OF 5 MOMENTA BETWEEN 1.72 AND 2.46 GEV/C. DONE AT NIMROD WITH OPTICAL SPARK CHAMBERS. THE APPARATUS IS DESCRIBED IN BELLAMY65, THE RESULTS IN BUSZA67. /// BUSZA69 [W. BUSZA,PR 180,1339(1969)] -- PI+ P DCS AT 10 MOMENTA BETWEEN 1.72 AND 2.80 GEV/C,AND PI- P DCS AT 5 MOMENTA BETWEEN 2.17 AND 2.80 GEV/C. THE DATA REPORTED IN BUSZA67 ARE ALSO REPEATED HERE. THE NEW MEASUREMENTS WERE DONE WITH AN IMPROVED VERSION OF THE APPARATUS USED BY BUSZA67. THE PI- DATA (INCLUDING BUSZA67)ARE NORMALIZED TO FORWARD DISPERSION RELATIONS,THE PI+ DATAHAS ITS OWN EXPERIMENTAL NORMALIZATION BUT NO NE IS GIVEN. WE HAVE INCREASED THE ERROR OF THE MOST FORWARD PI+ POINT AT 1.72 GEV/C BECAUSE OF AN AMBIGUOUS FOOTNOTE CONCERNING THIS POINT. /// COMMENTS FROM LOVELACE71 COMPILATION OF THESE DATA -- LOVELACE71 CLAIMS SOME USE WAS MADE OF FORWARD DISPERSION RELATIONS TO NORMALIZE THE PI+ DATA AS WELL AS THE PI-. THE FOLLOWING NORMALIZATION ERRORS AND RENORMALIZATION FACTORS ARE RECOMMENDED FOR THE PI+ P AND PI- P DIFFERENTIAL CROSS SECTIONS -- PLAB=1720 MEV/C -- NE(PI+ P)=INFIN, NE(PI- P)=INFIN. PLAB=1890 MEV/C -- RF(PI+ P)=1.245, RF(PI- P)=0.941. PLAB=2070 MEV/C -- NE(PI+ P)=INFIN, RF(PI- P)=1.224. PLAB=2170 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2270 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=INFIN. PLAB=2360 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2460 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=INFIN. PLAB=2560 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2650 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2800 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . /// COMMENTS ON MODIFICATIONS TO LOVELACE71 COMPILATION BY KELLY -- WE HAVE TAKEN ALL PI- NES TO BE INFINITE,AND ALL PI+ NES TO BE UNKNOWN. ALSO ONE MINOR MISTAKE IN THE PI- (PI+) DATA AT 2.36 (2.65) GEV/C HAS BEEN CORRECTED.
DOI: 10.17182/hepdata.6227.v1/t14
title: "Table 14" of "Pi-plus-minus p elastic scattering in the 2-gev region"

description: No description provided.
description: ALL DATA IN THIS RECORD ARE REDUNDANT. I.E., THEY WERE OBTAINED DIRECTLY FROM OTHER DATA IN THIS FILE, USUALLY BY EXTRAPOLATION OR INTEGRATION.. THE FOLLOWING COMMENTS ARE TAKEN FROM THE PI N COMPILATION OF R.L. KELLY. THEY ARE THAT COMPILATION& apos;S COMPLETE SET OF COMMENTS FOR PAPERS RELATED TO THE SAME EXPERIMENT (DESIGNATED BUSZA69) AS THE CURRENT PAPER. (THE IDENTIFIER PRECEDING THE REFERENCE AND COMMENT FOR EACH PAPER IS FOR CROSS-REFERENCING WITHIN THESE COMMENTS ONLY AND DOES NOT NECESSARILY AGREE WITH THE SHORT CODE USED ELSEWHERE IN THE PRESENT COMPILATION.) /// BELLAMY65 [E. H. BELLAMY,PROC. ROY. SOC. (LONDON) 289,509(1965)] -- /// BUSZA67 [W. BUSZA,NC 52A,331(1967)] -- PI- P DCS FROM 2K ELASTIC EVENTS AT EACH OF 5 MOMENTA BETWEEN 1.72 AND 2.46 GEV/C. DONE AT NIMROD WITH OPTICAL SPARK CHAMBERS. THE APPARATUS IS DESCRIBED IN BELLAMY65, THE RESULTS IN BUSZA67. /// BUSZA69 [W. BUSZA,PR 180,1339(1969)] -- PI+ P DCS AT 10 MOMENTA BETWEEN 1.72 AND 2.80 GEV/C,AND PI- P DCS AT 5 MOMENTA BETWEEN 2.17 AND 2.80 GEV/C. THE DATA REPORTED IN BUSZA67 ARE ALSO REPEATED HERE. THE NEW MEASUREMENTS WERE DONE WITH AN IMPROVED VERSION OF THE APPARATUS USED BY BUSZA67. THE PI- DATA (INCLUDING BUSZA67)ARE NORMALIZED TO FORWARD DISPERSION RELATIONS,THE PI+ DATAHAS ITS OWN EXPERIMENTAL NORMALIZATION BUT NO NE IS GIVEN. WE HAVE INCREASED THE ERROR OF THE MOST FORWARD PI+ POINT AT 1.72 GEV/C BECAUSE OF AN AMBIGUOUS FOOTNOTE CONCERNING THIS POINT. /// COMMENTS FROM LOVELACE71 COMPILATION OF THESE DATA -- LOVELACE71 CLAIMS SOME USE WAS MADE OF FORWARD DISPERSION RELATIONS TO NORMALIZE THE PI+ DATA AS WELL AS THE PI-. THE FOLLOWING NORMALIZATION ERRORS AND RENORMALIZATION FACTORS ARE RECOMMENDED FOR THE PI+ P AND PI- P DIFFERENTIAL CROSS SECTIONS -- PLAB=1720 MEV/C -- NE(PI+ P)=INFIN, NE(PI- P)=INFIN. PLAB=1890 MEV/C -- RF(PI+ P)=1.245, RF(PI- P)=0.941. PLAB=2070 MEV/C -- NE(PI+ P)=INFIN, RF(PI- P)=1.224. PLAB=2170 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2270 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=INFIN. PLAB=2360 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2460 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=INFIN. PLAB=2560 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2650 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2800 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . /// COMMENTS ON MODIFICATIONS TO LOVELACE71 COMPILATION BY KELLY -- WE HAVE TAKEN ALL PI- NES TO BE INFINITE,AND ALL PI+ NES TO BE UNKNOWN. ALSO ONE MINOR MISTAKE IN THE PI- (PI+) DATA AT 2.36 (2.65) GEV/C HAS BEEN CORRECTED.
DOI: 10.17182/hepdata.6227.v1/t15
title: "Table 15" of "Pi-plus-minus p elastic scattering in the 2-gev region"

description: No description provided.
description: ALL DATA IN THIS RECORD ARE REDUNDANT. I.E., THEY WERE OBTAINED DIRECTLY FROM OTHER DATA IN THIS FILE, USUALLY BY EXTRAPOLATION OR INTEGRATION.. THE FOLLOWING COMMENTS ARE TAKEN FROM THE PI N COMPILATION OF R.L. KELLY. THEY ARE THAT COMPILATION& apos;S COMPLETE SET OF COMMENTS FOR PAPERS RELATED TO THE SAME EXPERIMENT (DESIGNATED BUSZA69) AS THE CURRENT PAPER. (THE IDENTIFIER PRECEDING THE REFERENCE AND COMMENT FOR EACH PAPER IS FOR CROSS-REFERENCING WITHIN THESE COMMENTS ONLY AND DOES NOT NECESSARILY AGREE WITH THE SHORT CODE USED ELSEWHERE IN THE PRESENT COMPILATION.) /// BELLAMY65 [E. H. BELLAMY,PROC. ROY. SOC. (LONDON) 289,509(1965)] -- /// BUSZA67 [W. BUSZA,NC 52A,331(1967)] -- PI- P DCS FROM 2K ELASTIC EVENTS AT EACH OF 5 MOMENTA BETWEEN 1.72 AND 2.46 GEV/C. DONE AT NIMROD WITH OPTICAL SPARK CHAMBERS. THE APPARATUS IS DESCRIBED IN BELLAMY65, THE RESULTS IN BUSZA67. /// BUSZA69 [W. BUSZA,PR 180,1339(1969)] -- PI+ P DCS AT 10 MOMENTA BETWEEN 1.72 AND 2.80 GEV/C,AND PI- P DCS AT 5 MOMENTA BETWEEN 2.17 AND 2.80 GEV/C. THE DATA REPORTED IN BUSZA67 ARE ALSO REPEATED HERE. THE NEW MEASUREMENTS WERE DONE WITH AN IMPROVED VERSION OF THE APPARATUS USED BY BUSZA67. THE PI- DATA (INCLUDING BUSZA67)ARE NORMALIZED TO FORWARD DISPERSION RELATIONS,THE PI+ DATAHAS ITS OWN EXPERIMENTAL NORMALIZATION BUT NO NE IS GIVEN. WE HAVE INCREASED THE ERROR OF THE MOST FORWARD PI+ POINT AT 1.72 GEV/C BECAUSE OF AN AMBIGUOUS FOOTNOTE CONCERNING THIS POINT. /// COMMENTS FROM LOVELACE71 COMPILATION OF THESE DATA -- LOVELACE71 CLAIMS SOME USE WAS MADE OF FORWARD DISPERSION RELATIONS TO NORMALIZE THE PI+ DATA AS WELL AS THE PI-. THE FOLLOWING NORMALIZATION ERRORS AND RENORMALIZATION FACTORS ARE RECOMMENDED FOR THE PI+ P AND PI- P DIFFERENTIAL CROSS SECTIONS -- PLAB=1720 MEV/C -- NE(PI+ P)=INFIN, NE(PI- P)=INFIN. PLAB=1890 MEV/C -- RF(PI+ P)=1.245, RF(PI- P)=0.941. PLAB=2070 MEV/C -- NE(PI+ P)=INFIN, RF(PI- P)=1.224. PLAB=2170 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2270 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=INFIN. PLAB=2360 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2460 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=INFIN. PLAB=2560 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2650 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . PLAB=2800 MEV/C -- NE(PI+ P)=0.1 , NE(PI- P)=0.1 . /// COMMENTS ON MODIFICATIONS TO LOVELACE71 COMPILATION BY KELLY -- WE HAVE TAKEN ALL PI- NES TO BE INFINITE,AND ALL PI+ NES TO BE UNKNOWN. ALSO ONE MINOR MISTAKE IN THE PI- (PI+) DATA AT 2.36 (2.65) GEV/C HAS BEEN CORRECTED.