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891.
给出了求解中立型时滞抛物方程初边值问题t[u(x ,t) -λu(x ,t-τ) ] =2x2 u(x ,t) +f(x ,t) , (x ,t)∈ ( 0 ,l)× ( 0 ,T]u(x ,t) =φ(x ,t) , (x ,t)∈ ( 0 ,l)× [-τ ,0 ]u( 0 ,t) =u(l ,t) =0 , t∈ [-τ,T]的差分方法 ,并获得了该差分格式的收敛性 相似文献
892.
对2-连通非Hamilton赋权图G,本文证明:若P(u,v)是G中最重的最长路,则G的赋权周长C^w(G)≥d^w(u) d^w(v),假设G满足文中描述的额外条件C1,C2,则max{d^w(x),d^w(y)|d(x,y)=2}≥m/2时,对每个顶点v,G含量最重长v-路P(u,v)使d^w(u)≥m/2,而d^w(x) d^w(y) d^w(z)≥m(当d(x,y,z)=2)时,c^w(G)≥2m/3.改进了非赋权图的周长及赋权图的赋权周长的若干已有结果。 相似文献
893.
林江珠 《厦门理工学院学报》2002,10(1):56-60
平潭素有“千礁岛县”的美誉 ,主岛海坛风景名胜区以优质海滨沙滩和奇特的海蚀地貌被专家誉为海蚀地貌博物馆 ,于 1 994年被国务院确定为国家重点风景名胜区。但几年来平潭旅游在我省的旅游产业发展中却默默无闻 ,本文通过对平潭旅游业发展现状的换位思考 ,提出为适应新经济环境的变化 ,平潭旅游业应长远谋划来做心灵的生意 相似文献
894.
1999年至 2 0 0 1年每年 4~ 7月在吉林省西部地区对栗斑腹种群数量及繁殖情况进行了调查 ,发现三年来栗斑腹种群数量连续下降 .其原因是 :人为干扰导致栗斑腹繁殖成功率及繁殖成活率降低 ,从而导致栗斑腹种群数量下降 ;研究地区内近几年连续高温干旱的天气也导致了栗斑腹种群数量的下降 ,气温升高 (R2 =0 9964 )、降雨量减少 (R2 =0 84 98)对栗斑腹种群数量下降的影响很大 . 相似文献
895.
江虹 《贵州大学学报(自然科学版)》2002,19(2):145-153
介绍连续反应精馏过程设计的两种研究方法:静态分析法和有限元正交搭配OEFE法,静态分析法是对反应精馏图进行热力学和拓扑学分析,鉴定反应精馏过程的基本可能性,此方法不需要依靠确定的对象的特性,要求最少最反应混合物的物理化学特性,有限元正交配技术应用了把整级评估模型转变成连续的模型。OCFE能精确地吻俣逐板模型的优化设计,而只是使用一套较小的模型公式和避免使用与塔级数有关的总决策变量,用静态分析寻找一个最大转化率稳定态,用OCFE确定反应精馏塔的级数(塔级数)及进行精级(塔板)位置。 相似文献
896.
常江 《贵州师范大学学报(社会科学版)》2002,(3):106-108
班级规模是影响教学质量的重要因素。本讨论班级规模与教学质量的关系,班级规模变动的原因,以及在现代教学条件下班级规模扩大所产生的利与弊及其应对办法。 相似文献
897.
898.
Loess in the Tian Shan and its implications for the development of the Gurbantunggut Desert and drying of northern Xinjiang 总被引:8,自引:0,他引:8
Xiaomin Fang Zhentao Shi Shengli Yang Maodu Yan Jijun Li Ping’an Jiang 《科学通报(英文版)》2002,47(16):1381-1387
Eolian loess is widely distributed on the various geomorphic surfaces between 700–2400 m a.s.l. on the northern slope of the
Tian Shan. It is formed in a synchronous manner with dust transported from the Gurbantunggut Desert in the Junggar Basin.
The thickest section of loess was found in the Shawan and Shihezi regions. Paleomagnetic and climatic proxy analyses of over
71 m of a loess-paleosol sequence on the highest terrace of the Qingshui He (River) in the Shawan show that the paleomagnetic
Bruhues/Matuyama (B/M) boundary lies at the bottom of paleosol S8, at a depth of 69.5 m, and the bottom of the sequence was
estimated to be ∼0.8 Ma. This implies that the extremely dry climatic conditions in the Junggar Basin and the initial Gurbantunggut
Desert were present at least by 0.8 Ma. High-resolution grain size series demonstrate that this area and desert expansion
experienced two dramatic periods of desert expansions that occurred at ∼0.65 Ma and 0.5 Ma, respectively; and the subsequent
continuous enhancement led to the environment presently observed. This tremendous environmental effect, caused by large-scale
expansion of the desert and arid region of inner Asia, might be an important driving force for the global temperature drop
that occurred in the mid-Pleistocene. 相似文献
899.
An ammonia leaching process was utilized to extract Co, Ni and Cu from oceanic polymetallic nodules, whereas an acid leaching
process was utilized to extract Co, Ni, Cu, Zn and Mn from cobalt-rich crusts. Both processes produced nanometer materials—ammonia
leaching residue and acid leaching residue. A systematic study was conducted on the phase, composition and physicochemistry
properties of these residues. The result shows that both residues contain a large amount of nanometer minerals. Ammonia l
eaching residue mainly consists of rhodochrosite, with the average grain diameter of 17.9 nm; whereas the acid leaching residue
mainly consists of well-developed bassanite, with the average grain deameter of 9.5 nm. The bassanite also has a microporous
structure, the volume of the pore space is 1.23 × 10−2 mL/g. Both the ammonia and acid leaching residues have a large specific surface area, and they display a strong adsorption
capacity to saturate sodium chloride vapour, N2 and SO2. Both residues have high contents of rare earth elements, and most of these elements exist in the state of ionic adsorption.
The content of σ FeO is high. The P2O5 enrichment is observable in acid leaching residues. The unique composition and nanometer solid properties of the leaching
residues displayed their potential value and promised a bright future for their application in the field of environmental
protection and materials. 相似文献
900.
Carbon isotopic records in paleosols over the Pliocene in Northern China: Implication on vegetation development and Tibetan uplift 总被引:2,自引:0,他引:2
Carbon isotopic composition of pedogenic carbonate can be used to estimate the proportion of C4 and C3 plants. Here we present carbon isotopic data of carbonate in a red earth section at Xifeng, central Loess Plateau. Results
show that C4 vegetation increased in ∼4.4 Ma B.P., stabilized between 4.0 and 3.0 Ma B.P. The character and timing of C4 expansion on the Loess Plateau are similar, but different with other localities, e.g. Pakistan and Africa, implying that
regional climate changes were main factors driving the expansion of C4 plants. This event is comparable in timing with increased aridity evidenced by Xifeng grain size and North Pacific eolian
dust records. Therefore we argue that the Pliocene expansion of C4 plants in northern China might have been caused by the increased aridity, which in turn might be related to rapid uplift
of the Tibetan Plateau. 相似文献