1)cultural sediments文化沉积
2)electroless deposition化学沉积
1.Study of nanocrystalline Co-P alloy electroless deposition and its influencing factors on deposition rate;化学沉积纳米晶Co-P合金及其沉积速率影响因素的研究
2.Study on preparation of Ni-P-SiC(C) composite coatings by electroless deposition;化学沉积法制备Ni-P-SiC(C)复合镀层的研究
3.Effect of rare earth element on electroless deposition of cobalt-nickel-boron alloy;稀土元素对钴-镍-硼合金化学沉积的影响
英文短句/例句
1.The Chemical Deposition Alloy/electroless Composite Coating with Nanometer Particles;化学沉积合金/纳米粒子化学复合涂层
2.Preparation of Biaxial Textured Metal Substrate by Electro-Plating;电化学沉积制备双轴织构化金属薄膜
3.Preparation and Anti-corrosion Study of TiO_2 Film;TiO_2薄膜的电化学沉积及耐蚀性能研究
4.Studies on Process and Corrosion Resis tance of Electrodeposited Polyaniline;电化学沉积聚苯胺膜及其耐蚀性研究
5.Effects of pH Value on CdS Thin Films Grown by Chemical Bath Deposition;pH值对化学沉积CdS薄膜性质的影响
6.Study on Synthesis of MgB_2 by Electrochemical Deposition Method电化学沉积法制备MgB_2的研究
7.thermally activated chemical vapour deposition热活化化学气相沉积
8.plasma activated chemical vapour deposition等离子体化学气相沉积
9.chemically formed sedimentary rock化学作用形成的沉积岩
10.epitaxial CVD growth外延化学气相沉积生长
11.HT-CVD(high temperature chemical vapour deposition)高温化学蒸汽沉积法
12.modern marine sedimentary geochemistry现代海洋沉积地球化学
13.STUDY ON CHARACTERIS TICS OF SEDIMENTATION FOR CHEMICAL FLOCCULATED AND COAGULATED SUSPENSION化学絮凝及凝聚浆体沉降－沉积特性的研究
14.chemical components of discharges and deposits排放物及沉积物的化学组分
15.geochemical stream sediment survey水系沉积物地球化学测量
16.BASIC CHARACTERISTICS OF GEOCHEMISTRY OF SEDIMENTS IN OKINAWA TROUGH冲绳海槽沉积物地球化学的基本特征
17.Study of CVD Function coating on Molybdenum Substrate钼表面化学气相沉积功能涂层的研究
18.Study on Environmental Geochemistry of the Sediments in Modaomen Estuary of the Pearl River;珠江磨刀门河口的沉积化学环境研究
相关短句/例句
electroless deposition化学沉积
1.Study of nanocrystalline Co-P alloy electroless deposition and its influencing factors on deposition rate;化学沉积纳米晶Co-P合金及其沉积速率影响因素的研究
2.Study on preparation of Ni-P-SiC(C) composite coatings by electroless deposition;化学沉积法制备Ni-P-SiC(C)复合镀层的研究
3.Effect of rare earth element on electroless deposition of cobalt-nickel-boron alloy;稀土元素对钴-镍-硼合金化学沉积的影响
3)electroless plating化学沉积
1.Impact of electroplate and electroless plating on nano-Co-B alloy functional film;Co-B纳米合金功能膜化学沉积和电沉积的比较
2.Test study on electroless plating of Ni-W-P/Ni-P alloys;Ni-W-P/Ni-P合金的化学沉积试验研究
3.The Study on the Microstructure and Properties of Electroless Plating Multicompnent Cobalt Based Soft Magnetic Film with Rare Earth Joined;化学沉积稀土多元钴基软磁薄膜结构和性能的研究
4)Sedimentary evolution沉积演化
1.The Tertiary sedimentary evolution of the Qaidam Basin, Northwest China;柴达木第三纪湖盆沉积演化史
2.Tectonic-sedimentary evolution of the first and second members of the Kongdian Formation in southern Kongdian,Huanghua depression;黄骅坳陷孔南地区孔一、孔二段构造沉积演化
3.Discussion on relationship between sedimentary evolution of the Triassic Yanchang Formation and the Early Indosinian Movement in Ordos Basin;鄂尔多斯盆地三叠系延长组沉积演化及其与早印支运动关系的探讨
5)sedimentation chemistry沉积化学
6)chemical deposition化学沉积
1.Copper oxide/porous carbon composite materials were prepared by a chemical deposition method.通过化学沉积法制备了金属铜氧化物/多孔炭复合电极材料,考察了热处理温度及金属铜氧化物负载量对其理化性能的影响。
2.Poly(ethylene covinyl alcohol)end-capped with potassium sulfonate (EVOH-SO3 K)was synthesized by sulfonification of poly(ethyl- ene covinyl alcohol)(EVOH)with 1,3-propane suhone and was modified by toluene-2,4-diisocyanate (TDI)to get a cross-linked ionic polymer (EVOH-TSO3 K),and then the IPMC based on EVOH-TSO3 K was prepared through the method of chemical deposition.由聚乙烯-乙烯醇(EVOH)和1,3-丙烷磺酸内酯合成了EVOH磺酸钾离子聚合物(EVOH-SO_3K),并用2,4-甲苯二异氰酸酯(TDI)对其进行了交联改性,得到TDI改性EVOH磺酸钾离子聚合物(EVOH-TSO_3K),通过EVOH-TSO_3K溶液的铸膜和化学沉积制得离子聚合物膜金属复合材料(IPMC)。
3.A composite electrode of nickel hexacyanoferrate(NiHCF),graphite power,and methyltrimethoxysilane(MTMOS) was prepared by chemical deposition technology.利用化学沉积技术制备了NiHCF/石墨粉/MTMOS复合修饰电极,研究了NiHCF/石墨粉/MTMOS复合修饰电极作为安培型L—半胱氨酸传感器的电化学行为。
延伸阅读
半深海沉积 水深大致在 200～2000米范围的沉积物。主要分布在大陆坡，又称陆坡沉积。大陆坡是一个分开大陆和大洋的全球性巨大斜坡，是大陆和洋盆之间的过渡地带。陆坡沉积物也具有明显的过渡性质，它既不同于浅海沉积，又有别于深海沉积。滑坡所造成的影响是它的显著特点。其物质来源以陆源碎屑为主，生物与化学作用形成的沉积多于浅海区，少于深海区。在有些地区，碳酸盐沉积的比重明显增加。 陆坡沉积物的粒度小于浅海沉积，沉积物中约60％是泥，25％是砂，10％是岩块和砾石,其余的5％是贝壳和生物沉积。越过陆架坡折线后，沉积物往往从砂变成泥。粗粒沉积只呈斑块状分布，有些海区基岩裸露，它们常与崎岖的海底形态有关。 滑坡沉积物在陆坡沉积中占有突出地位。其形成与陆坡的不稳定性有关，坡度过陡或沉积速率过大常导致滑坡。滑坡沉积体后缘遭受拉张,导致断裂;前端遭受挤压，形成冲断层、褶皱和拱起的小丘。在地形和地震剖面上显示为岗丘状、杂乱的坡面，不连续的反射层。在沉积岩心中可见到扭曲层理。 大陆坡上广泛发育海底峡谷。它虽为侵蚀地形，但有的谷底堆积有大量沉积物，其主要特征是：沉积物主要为泥质，夹有少量粗碎屑物质；峡谷出口处往往是浊流沉积分布区；沉积物中普遍含有浅水有孔虫及海绿石；峡谷中常有更新世末期和冰后期的沉积物。 第四纪冰期低海位时,河流穿过当时的滨海平原(现在的大陆架),将大量物质直接搬运到陆坡上堆积。沉积速率增大，沉积粒度变粗，滑坡沉积物尤其常见，在陆坡，特别是它的下部形成了巨厚的沉积。 濒临中国的南海和东海的陆坡上，沉积物虽以陆源为主，但生物和自生成因的沉积也占显著地位，如南海北部陆坡上形成了自生海绿石砂；东海陆坡出现有孔虫等生源沉积物，并有浊流沉积分布。
