共查询到19条相似文献,搜索用时 812 毫秒
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在亚纯函数值分布论中,有重要的杨乐不等式。本文基于Nevanlinna理论将杨乐不等式中计数函数的常数推广为多项式函数。 相似文献
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在亚纯函数值分布论中,有重要的杨乐不等式.本文基于Nevanlinna理论将杨乐不等式中计数函数的常数推广为多项式函数. 相似文献
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唐林勇 《西南师范大学学报(自然科学版)》2002,27(1):10-12
基于Nevanlinna理论对杨乐不等式进行推广,把原不等式中的计算函数的常数易为超越小整函数,得到了另一个形式的杨乐不等式。 相似文献
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在亚纯函数值分布论中,有一类重要的精密的杨乐不等式.为求得亚纯函数相对于多项式函数的值分布,基于Nevanlinna理论和函数论分析的方法将杨乐不等式中计数函数的常数推广为多项式函数,并得到了相应的亏量和的上界,结果显示亚纯函数相对于多项式的值分布的不等式也是精密的. 相似文献
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定义并研究了代数体函数的对应加法,结合杨乐、孙道椿的研究亚纯函数的方法,将仪洪勋联系重值的亚纯函数唯一性定理推广到了多值的代数体函数. 相似文献
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研究了两个不可约代数体函数相等的条件,并结合杨乐,Lahiri研究亚纯函数重值的方法将仪鸿勋关于亚纯函数唯一性定理的几个结论推广到多值的代数体函数。 相似文献
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研究了亚纯函数族的正规性,在改进顾永兴、杨乐、方明亮等人的相关结果的基础上获得了亚纯函数族的几个正规定则.在涉及例外函数a(z)其中a(z)≠0的条件下,主要证明了定理1和定理2. 相似文献
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C.C.Swisher Ⅲ 《科学通报(英文版)》2002,47(2)
We report new 40Ar/39Ar dating results obtained from total fusion and incremental-heating analyses of sanidine and biotite from three tuffs found interbedded within the fossil-bearing deposits of Liaoning, northeast China. The first is a new sample of the Bed 6 Sihetun tuff from the Yixian Formation, previously dated by our team as middle Early Cretaceous, and recently considered by Lo et al., partially reset due to metamorphism from a nearby basaltic sill. The second is the Yixian Bed 9 tuff from Hengdaozi considered by Lo et al. to be unaffected by metamorphism and whose age, based on total fusion 40Ar/39Ar dating of biotite, argues for a Jurassic age for the Yixian Formation.The third tuff is a previously undated tuff from the upper part of the underlying Tuchengzi Formation. Single crystal total fusion 40Ar/39Ar analyses of the Sihetun sanidine showed homogeneous radiogenic Ar, Ca/K ratios, excellent reproducibility and gave a mean age of 125.0 ± 0.18 (1SD) ±0.04 (SE) Ma. Single sanidine crystal total fusion 40Ar/39Aranalyses of the Hengdaozi tuff gave a mean age of 125.0 +0.19 (1SD) ± 0.04 (SE) Ma, which is indistinguishable from the Sihetun tuff. The Tuchengzi Formation tuff gave a mean age of 139.4 ± 0.19 (1SD) ± 0.05 (SE) Ma. Detailed laser incremental-heating analyses of biotite from Sihetun, Hengdaozi, and Tuchengzi tuffs show disturbed Ar release patterns and evidence of trapped argon components. We conclude from these analyses that the total fusion dates on biotite by Lo et al. are erroneously old and isotopic dating of both biotite and sanidine from tuffs of the Yixian Formation point to a middle Early Cretaceous age. The upper part of the Tuchengzi Formation can be referred to the Early Cretaceous.`` 相似文献
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代数体函数的唯一性定理 总被引:7,自引:3,他引:4
定义了代数体函数的加法及乘法,并证明了运算后的结果仍是代数体函数. 并应用新定义的加法,将联系重值的唯一性定理推广到多值的代数体函数. 相似文献
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微分多项式具有重值的亚纯函数的奇异方向 总被引:1,自引:0,他引:1
李纯红 《西华师范大学学报(哲学社会科学版)》1993,14(1):7-15
给出了一类亚纯函数在涉及微分多项式具有重值情况下的正规定则与奇异方向,分别推广了杨乐、顾永兴、陈怀惠、柏盛桄和作者的结果. 相似文献
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C. C. Swisher Xiaolin Wang Zhonghe Zhou Yuanqing Wang Fan Jin Jiangyong Zhang Xing Xu Fucheng Zhang Yuan Wang 《科学通报(英文版)》2002,47(2):136-139
We report new 40Ar÷39Ar dating results obtained from total fusion and incremental-heating analyses of sanidine and biotite from three tuffs found
interbedded within the fossil-bearing deposits of Liaoning, northeast China. The first is a new sample of the Bed 6 Sihetun
tuff from the Yixian Formation, previously dated by our team as middle Early Cretaceous, and recently considered by Lo et
al., partially reset due to metamorphism from a nearby basaltic sill. The second is the Yixian Bed 9 tuff from Hengdaozi considered
by Lo et al. to be unaffected by metamorphism and whose age, based on total fusion 40Ar÷39Ar dating of biotite, argues for a Jurassic age for the Yixian Formation. The third tuff is a previously undated tuff from
the upper part of the underlying Tuchengzi Formation. Single crystal total fusion 40Ar÷39Ar analyses of the Sihetun sanidine showed homogeneous radiogenic Ar, Ca÷K ratios, excellent reproducibility and gave a mean
age of 125.0±0.18 (1SD)±0.04 (SE) Ma. Single sanidine crystal total fusion 40Ar÷39Ar analyses of the Hengdaozi tuff gave a mean age of 125.0±0.19 (1SD)±0.04 (SE) Ma, which is indistinguishable from the Sihetun
tuff. The Tuchengzi Formation tuff gave a mean age of 139.4±0.19 (1SD)±0.05 (SE) Ma. Detailed laser incremental-heating analyses
of biotite from Sihetun, Hengdaozi, and Tuchengzi tuffs show disturbed Ar release patterns and evidence of trapped argon components.
We conclude from these analyses that the total fusion dates on biotite by Lo et al. are erroneously old and isotopic dating
of both biotite and sanidine from tuffs of the Yixian Formation point to a middle Early Cretaceous age. The upper part of
the Tuchengzi Formation can be referred to the Early Cretaceous. 相似文献
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水分胁迫下亚麻种子萌发的生理响应 总被引:3,自引:0,他引:3
为了解水分胁迫对亚麻种子萌发的影响以及为亚麻抗旱栽培技术和育种方法提供理论依据,以亚麻076、075、陇亚8号的种子为试验材料,分别用不同质量分数(0%、10%、15%、20%、25%、30%)的聚乙二醇(PEG-6000)处理,研究水分胁迫对亚麻种子的萌发的影响。结果显示:随着PEG质量分数的增加,亚麻种子的发芽势、发芽率下降,其中陇亚8号下降幅度最大。亚麻种子在PEG质量分数增加时,电导率呈现了低高低的趋势,其中076的电导率的变化较明显。适宜质量分数的PEG胁迫可以提高种子的活力指数,而较高质量分数的PEG则降低种子的活力指数。试验可知,这3个品种的种子在抗旱性上有明显的差异,076抗旱性强,075较抗旱,陇亚8号不抗旱。 相似文献
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C. C. Swisher III WANG Xiaolin ZHOU Zhonghe WANG Yuanqing JIN Fan ZHANG Jiangyong XU Xing ZHANG Fucheng WANG Yuan 《科学通报(英文版)》2002,47(2):135-138
We report new 40Ar/39Ar dating results obtained from total fusion and incremental-heating analyses of sanidine and biotite from three tuffs found interbedded within the fossil-bearing deposits of Liaoning, northeast China. The first is a new sample of the Bed 6 Sihetun tuff from the Yixian Formation, previously dated by our team as middle Early Cretaceous, and recently considered by Lo et al., partially reset due to metamorphism from a nearby basaltic sill. The second is the Yixian Bed 9 tuff from Hengdaozi considered by Lo et al. to be unaffected by metamorphism and whose age, based on total fusion 40Ar/39Ar dating of biotite, argues for a Jurassic age for the Yixian Formation. The third tuff is a previously undated tuff from the upper part of the underlying Tuchengzi Formation. Single crystal total fusion 40Ar/39Ar analyses of the Sihetun sanidine showed homogeneous radiogenic Ar, Ca/K ratios, excellent reproducibility and gave a mean age of 125.0 ± 0.18 (1SD) ± 0.04 (SE) Ma. Single sanidine crystal total fusion 40Ar/39Ar analyses of the Hengdaozi tuff gave a mean age of 125.0 ± 0.19 (1SD) ± 0.04 (SE) Ma, which is indistinguishable from the Sihetun tuff. The Tuchengzi Formation tuff gave a mean age of 139.4 ± 0.19 (1SD) ± 0.05 (SE) Ma. Detailed laser incremental-heating analyses of biotite from Sihetun, Hengdaozi, and Tuchengzi tuffs show disturbed Ar release patterns and evidence of trapped argon components. We conclude from these analyses that the total fusion dates on biotite by Lo et al. are erroneously old and isotopic dating of both biotite and sanidine from tuffs of the Yixian Formation point to a middle Early Cretaceous age. The upper part of the Tuchengzi Formation can be referred to the Early Cretaceous. 相似文献