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71.
1土地利用特点 泽市土地总面积121.94万hm2,已利用土地115.28万hm2,土地利用率为94.54%,农用土地97.99万hm2,占土地总面积的80.36%,其中耕地83.30万hm2,占土地总面积的.68.26%,园地1.22万hm2,占土地总面积的1.00%,林地6.38万hm2,占土地总面积的5.22%;其他农用地7.24万hm2,占土地总面积的5.88%;建设用地18.93万hm2,占土地总面积的15.52%;未利用土地5.35万hm2,占土地总面积的4.12%. 相似文献
72.
东营凹陷南斜坡原油生物标志物特征和油源对比 总被引:1,自引:0,他引:1
对东营凹陷南斜坡沙四段油砂采样和高分辨率的GC-MS分析,研究了南斜坡沙四段原油的生物标志物特征,并且进行了油源对比,分析了原油成因.C29甾烷20 S/20(R S)和C29甾烷ββ/(αα ββ)参数显示纯化、乐安、广利、金家和王家岗部分样品为低成熟原油.小营、正理庄、高青和王家岗部分地区样品为成熟油原油.C27/C29>1反映广利、纯化和金家母源输入有低等水生生物输入,C27/C29<1反映王家岗、草桥、高青和小营地区母源有高等植物的贡献.原油中正构烷烃主要以奇数碳占优势,碳数分布为nC14-nC34,普遍存在生物降解,个别样品正构烷烃几乎消失殆尽.多数样品Pr/Ph<1,具有明显地植烷优势,伽马蜡烷/C30藿烷分布介于0.15~1之间,说明母源沉积环境为半咸水-咸水还原沉积环境.油源对比表明博兴地区的原油主要来自于博兴洼陷的沙三、沙四上段烃源岩.纯化油田油源主要来自于利津和博兴洼陷沙四上亚段,乐安、八面河、羊角沟、王家岗、广利油田的原油来自牛庄洼陷沙四上亚段. 相似文献
73.
Rossby waves with linear topography in barotropic fluids 总被引:1,自引:0,他引:1
Rossby waves are the most important waves in the atmosphere and ocean, and are parts of a large-scale system in fluid. The theory and observation show that, they satisfy quasi-geostrophic and quasi-static equilibrium approximations. In this paper, solitary Rossby waves induced by linear topography in barotropic fluids with a shear flow are studied. In order to simplify the problem, the topography is taken as a linear function of latitude variable y, then employing a weakly nonlinear method and a perturbation method, a KdV (Korteweg-de Vries) equation describing evolution of the amplitude of solitary Rossby waves induced by linear topography is derived. The results show that the variation of linear topography can induce the solitary Rossby waves in barotropic fluids with a shear flow, and extend the classical geophysical theory of fluid dynamics. 相似文献
74.
???????????????????????????????????????嶫?????????GPS????????????????????????????????λ??ó?????????β???????仯???????????2001???????8.1???????????β?????????д?????μ?仯????????仯?????????ж??????????С????????????????????????????????????????8.1????????????????????????????????о????????????????β???????п??????????????????? 相似文献
75.
76.
A combined numerical model of wind, wave, tide, and storm surges was built on the basis of the “wind field model in limited
sea surface areas”. When used to forecast the sea surface wind, wave height and water level, it can describe them very well.
Contribution No. 4108 from the Institute of Oceanology, Chinese Academy of Sciences.
This work supported by Stress Project (KZ952-S1-420), Chinese Academy of Sciences; 863 Project (863-818-06-05), and (863-818-Q-07) 相似文献
77.
Based on in-situ observation, satellite and reanalysis data, responses of the western North Pacific subtropical ocean(WNPSO) to the slow-moving category 5 super typhoon Nanmadol in 2011 are analyzed. The dynamical response is dominated by near-inertial currents and Ekman currents with maximum amplitude of 0.39 m/s and 0.15 m/s, respectively. The near-inertial currents concentrated around 100 m below the sea surface and had an e-folding timescale of 4 days. The near-inertial energy propagated both upward and downward, and the vertical phase speed and wavelength were estimated to be 5 m/h and 175 m, respectively. The frequency of the near-inertial currents was blue-shifted near the surface and redshifted in ocean interior which may relate to wave propagation and/or background vorticity. The resultant surface cooling reaches -4.35℃ and happens when translation speed of Nanmadol is smaller than 3.0 m/s.When Nanmadol reaches super typhoon intensity, the cooling is less than 3.0℃ suggesting that the typhoon translation speed plays important roles as well as typhoon intensity in surface cooling. Upwelling induced by the slow-moving typhoon wind leads to typhoon track confined cooling area and the right-hand bias of cooling is slight. The mixed layer cooling and thermocline warming are induced by wind-generated upwelling and vertical entrainment. Vertical entrainment also led to mixed layer salinity increase and thermocline salinity decrease, however, mixed layer salinity decrease occurs at certain stations as well. Our results suggest that typhoon translation speed is a vital factor responsible for the oceanic thermohaline and dynamical responses, and the small Mach number(slow typhoon translation speed) facilitate development of Ekman current and upwelling. 相似文献
78.
Journal of Geographical Sciences - Runoff generation is an important part of water retention service, and also plays an important role on soil and water retention. Under the background of the... 相似文献
79.
Chen Wei Pradhan Biswajeet Li Shaojun Shahabi Himan Rizeei Hossein Mojaddadi Hou Enke Wang Shengquan 《Natural Resources Research》2019,28(4):1239-1258
Natural Resources Research - Groundwater is a vital water source in the rural and urban areas of developing and developed nations. In this study, a novel hybrid integration approach of... 相似文献
80.
Huang Chi-Yue Shao Lei Wang Ming-Huei Xue Wei-Guang Qiao Pei-Jun Cui Yu-Chi Hou Yuan-Li 《Marine Geophysical Researches》2019,40(2):111-127
Marine Geophysical Research - Early Cenozoic rift basins developed commonly on the Mesozoic basement along the SE Asia Continent. However, Eocene–Oligocene sequences were only exposed widely... 相似文献