Combined study of gamma p ->eta p and pi(-)p ->eta n in a chiral constituent quark approach

Within a chiral constituent quark model approach, η-meson production on the proton via electromagnetic and hadron probes is studied. With few parameters, the differential cross section and polarized beam asymmetry for γp → ηp and differential cross section for π − p → ηn processes are calculated and successfully compared with the data in the center-of-mass energy range from threshold up to 2 GeV. The five known resonances S11(1535), S11(1650), P13(1720),D13(1520), and F15(1680) are found to be dominant in the reaction mechanisms in both channels. Possible roles played by new resonances are also investigated; and in the photoproduction channel, significant contribution from S11 and D15 resonances, with masses around 1715 and 2090 MeV, respectively, are deduced. For the so-called missing resonances, no evidence is found within the investigated reactions. The helicity amplitudes and decay widths of N ∗ → πN, ηN are also presented and found to be consistent with the Particle Data Group values.

eta-production on the proton via electromagnetic and hadronic probes

The reactions pi(-)p -> eta n and gamma p -> eta p are investigated within a dynamical coupled-channels model of meson production reactions in the nucleon resonance region The meson-baryon channels included are pi N, pi Delta, sigma N, and rho N The direct eta-photoproduction process is studied within a formalism based on a chiral constituent quark model approach, complemented with a one-gluon-exchange mechanism, to take into account the breakdown of the SU(6)circle times O(3) symmetry In the models search, the following known nucleon resonances are embodied S-11(1535), S-11(1650), P-11(1440), P-11(1710), P-13(1720), D-13(1520), D-13(1700), D-15(1675), and F-15(1680). Data for the pi(-)p -> eta n reaction from threshold up to a total center-of-mass energy of W approximate to 2 GeV are satisfactorily reproduced For the photoproduction channel: two additional higher mass known resonances, P-13(1900) and F-15(2000), are also considered However, reproducing the data for gamma p -> eta p requires, within our approach, two new nucleon resonances, for which we extract, mass and width

Study of nucleon resonances in a chiral quark model via eta productions

In this report we investigate eta-meson productions oil the proton via electromagnetic and hadron probes in a chiral quark model approach. The observables, such as, differential cross section and beam asymmetry for the two productions are calculated and compared with the experiment. The five known resonances S-11(1535) S-11(1650); P-13(1720) D-13(1520), and F-15(1680) are found to be dominant in the reaction mech-anisms in both channels. Significant, contribution from a new S-11 resonances are deduced. For the so-called "missing resonances", no evidence is found within the investigated reactions. The partial wave amplitudes for pi(-)p -> eta n are also presented.

eta photoproduction on the proton in a chiral constituent quark approach via a one-gluon-exchange model

A formalism based on a chiral quark model (chi QM) approach complemented with a one-gluon-exchange model, to take into account the breakdown of the SU(6)circle times O(3) symmetry, is presented. The configuration mixing of wave functions for nucleon and resonances are derived. With few adjustable parameters, differential cross-section and polarized-beam asymmetry for the gamma p -> eta p process are calculated and successfully compared with the data in the center-of-mass energy range from threshold to 2 GeV. The known resonances S-11(1535), S-11(1650), P-13(1720), D-13(1520), and F-15(1680), as well as two new S-11 and D-15 resonances, are found to be dominant in the reaction mechanism. Moreover, connections among the scattering amplitudes of the chi QM approach and the helicity amplitudes, as well as decay widths of resonances, are established. Possible contributions from the so-called missing resonances are investigated and found to be negligible.

快重离子在聚苯乙烯中的辐照效应研究

本工作用兰州重离子加速器提供的2.1GeV的Kr离子分别在空气和真空条件下辐照了多层堆叠的聚苯乙烯薄膜样品，辐照剂量在5 * 10~(10)到3 * 10~(12)ions/cm~2之间，辐照温度在室温附近。辐照后对样品分别进行了傅立叶变换红外光谱和紫外可见光谱的测量，由此研究了快重离子辐照聚苯乙烯产生的物理和化学改性。实验结果表明，聚苯乙烯经Kr离子辐照后发生了降解，包括苯环在内的大部分官能团遭到破坏，相应特征峰的吸光度随辐照剂量和能损的增加而减小。与此同时，辐照还在1650-1750cm~(-1)之间和3300cm~(-1)处产生了新的吸收峰，其分别对应于C=O双键的分子振动和C≡C-H的C-H伸缩振动，表明辐照在聚苯乙烯中产生了炔基。实验发现产生炔基需要离子有足够高的电子能损值，在聚苯乙烯中该能损阈值约为1.0keV/nm。在材料经辐照发生降解的同时，样品的光吸收边界逐渐红移，并伴有透光率的下降。详细的测量显示，在紫外可见区材料吸光度的增加随剂量近似呈线性关系，随能损呈约二次方的指数关系。通过对2.1GeV的Kr离子和1.4GeV的Ar离子辐照结果的比较还发现，快重离子辐照产生的物理化学改性不仅与离子的能损有关，还与离子的速度有关。在同一能损条件下，速度越小，产生的效应就越大。文中用径向能量沉积密度和有效化学反应半径对上述结果进行分析讨论。

冻结数模型在中国东北多年冻土分区中的应用

基于1981—2000年间中国东北地区的气候要素和雪深数据,将冻结数模型应用于中国东北的多年冻土地区,研究了冻结数模型在东北多年冻土分区的可适用性.结果表明:中国东北地区的多年冻土以不连续多年冻土为主,其多年冻土区包括除岛状多年冻土以外的断续多年冻土(大块多年冻土)、岛状融区多年冻土(大块-岛状多年冻土)和山地多年冻土.对不同时期区划图进行比较,冻结数模型的模拟结果基本能够反映研究区当前多年冻土的分区状况.大兴安岭不连续多年冻土南界可向南延伸至阿尔山附近,其他山地多年冻土和小兴安岭伊春地区的多年冻土在模拟结果中也得到体现.

高山峡谷地区森林流域分布式降雨-径流模型的构建与验证

根据岷江上游杂谷脑河流域典型的高山峡谷地区主要水文特点,选择通用性较强的水文过程模式,构建高山峡谷地区森林流域分布式降雨-径流过程模型,避免过多复杂的区域性模型参数率定,保证模型在相似地区的可移植性;并选择杂谷脑水文站上游地区进行降雨-径流过程模拟,得到1999年和2000年模拟时段长度为1 000 h的两个径流过程,对模拟与实测的径流过程、累积径流量、洪峰流量与峰现时间等进行比较,其拟合效果较好.该模型结构简单,引入的经验参数较少,可推广应用到其它尺度流域.

沈阳福陵油松年轮宽度年表的建立

该文以沈阳福陵的油松为样本建立了油松年轮宽度年表(标准化年表、差值年表和自回归年表).分析表明:年表与冬季(上年11—2月)和初春(4—5月)低温的关系密切,其中与上年11月、1月的低温显著相关;年表与1、2月的降水量显著相关,还与1、9月的水汽压显著相关;上年10月—上年11月9、月、5—6月份的相对湿度对油松的影响突出;蒸发量对油松生长起显著的负效应,其中5月最明显,但1、2月的蒸发量与油松当年的年轮宽度正相关.油松年表的窄轮和窄化突变佐证了公元1650年以来的35次主要的旱灾年.油松年轮宽度年表和过去太阳活动、地磁的活动均存在共同的准周期变化.

物候模式识别在生态动力预报中的应用

以物候资料和数值天气预报模式输出图为基础,应用模式识别和数理逻辑判断的自动化技术,阐述制作生态动力预报的原理、方法和步骤.生态动力预报技术使传统的物候学在气象学和自动化技术支持下,扩展应用到生态预报业务领域,使物候预报从单站预报阶段发展到区域预报阶段,同时促进了农业气象预报方法从定性、统计阶段向动力预报阶段发展.该方法在农作物播种、长势、灌溉与施肥、病虫害防治等方面具有广阔的应用前景.

站在新的历史起点上推进生态文明建设

<正>生态文明的提出是历史的必然人类历史是一部人与自然关系发展的历史,它经历了一个从被动适应到主动适应的过程。在原始社会,即渔猎文明时期,人类只是被动地适应自然,对自然界没有实质性破坏和威胁,并处处受自然界的束缚,形成了原始的文明意识,此间历时百万年。随着农业的诞生,特别是铁器生产工具的出现,人们从被动适应自然过渡到主动适应自然,并出现了农业文明,此间历时万余年。在这一时期,人们为了自身的

湖北省近500年区域干湿序列重建及其比较分析

在历史旱涝记载资料可靠性检验的基础上,重建了湖北省3个区域近500年来的干湿气候变化序列,并比较分析了各区域干湿气候变化的趋势特征、准周期性及跃变现象。结果表明:在3个区域中,鄂东区1570~1770、1890~1950年两个时段偏湿,1470~1520、1790~1830年则偏干;鄂北区偏湿时期主要在1470~1530、1710~1750、1850~1910年三个时段,1470~1530、1770~1830年则偏干;鄂西南区有1550~1610、1650~1710、1830~1890、1930~1990