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矿化作用

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Results:(1) CBC possesses a natural trabecular structure. Its components is similar to the mineral of bone.(2) CBC has great cellur biocompatibility. It can promote cell adhesion, proliferation and secretory while needn t modification.(3) In nude mice, the ectopic osteogenesis of MCCAB was obvious which was better than that of CBC alone and the new bone formation increased in pace with time. In the MCCAB, both intramembranous and cartilaginous osteogeneses were seen but the former dominated.(4) When MCCAB was autotransplanted intramuscularly, the osteogenesis was much better than that of negative control groups.(5) The MCCAB can repair autogenous calvaria defects effectively and the effect was much better than that of CBM alone and blank group. Conclusion:(1) CBC possesses good biocompatibility, osteoconduction and porous structure, can be used as scaffold material for constructing of tissue engineering bone.

结果:(1)CBC具有天然的多孔网状结构,最大程度地保持了骨矿的微结构特征,可以作为骨组织工程的支架材料;(2)CBC细胞亲和性好,不需作修饰即能促进成骨细胞的粘附、增殖和分泌活动;(3)MSO/CBC复合人工骨在裸鼠皮下异位成骨作用明显,兼有膜内成骨和软骨内成骨的特点,成骨效果明显优于单纯CBC植入组;(4)MSO/CBC复合人工骨兔自体肌袋异位成骨作用明显,血管化充分,成骨效果明显优于单纯CBC植入组;(5)MSO/CBC复合人工骨修复兔颅骨临界性缺损效果好,明显优于单纯植入CBC组和空白对第四旱区大学硕士学位论文一照组,可以作为骨移植替代材料用于骨缺损畸形修复。

Under the condition of laboratory incubation,the C loss of organicmaterials during their mineralization was greater than their N loss,inducing ahigher residual amount of organic organic N.During the decay of maize andrice staw with a wide ratio of C/N.soil microbes could fix N,but the fixationrate was quite low,only 0.2-0.9g N/assimulated 100g organic C.

在实验室培养条件下有机物料在矿化分解过程中C的损失总是大于N的损失,因此有机N的残留率明显高于有机C的残留;且由于灰分总量不变,有机物料的残留率也略高于有机C的残留率;〓比较宽的玉米秸和稻秸在腐解过程中发生了自生固N作用,但其固N效率仅为C:N=100:0.2-0.9,即每同化100g有机C,只能固定

In fact, some of organicphosphorus was easy to be mineralized and plays an important role to the supply of phosphorus.

事实上,土壤中某些有机磷是易矿化的,对土壤磷素供应起着重要的作用。

Dynamical metamorphism under greenschist facies is the condition of mineralizing enrichment.

绿片岩相以下的动力变质作用是矿化富集的条件。

The proliferation of osteoblast was measured by thiazolyl blue,activity of alkaline-phosphotase was observed with Golden s method and alizarin red stain was used to measure the mineral nodes of osteoblasts.

结果 0 10 g·L-1的麦胚提取物可以促进体外培养大鼠成骨细胞的增殖和分化作用,0 5 0g·L-1促使成骨细胞矿化结节的形成。

The circular centrifugal flotation cell has many originalities on the pulp aeration, air bubble mineralization, air pulp flow format in the ring shaped tank of the cell, feed method ect, due to the results of fluidics and turbulence and the action of centrifugal and gravitational force ect.

新型高效圆形离心浮选机充分发挥了湍流射流及离心—重力力场的作用,使其在矿浆充气、气泡矿化、浮选槽内矿浆流动形式、给料方式等方面独具特色。在普通喷动床环形区底部引入&充气&可消除环形区底部颗粒&死区&的影响,并能改善环形区气固间的热、质传递。

The circular centrifugal flotation cell has many originalities on the pulp aeration, air bubble mineralization, air pulp flow format in the ring shaped tank of the cell, feed method ect, due to the results of fluidics and turbulence and the action of centrifugal and gravitational force ect.

新型高效圆形离心浮选机充分发挥了湍流射流及离心—重力力场的作用,使其在矿浆充气、气泡矿化、浮选槽内矿浆流动形式、给料方式等方面独具特色。

Laccase (benzenediol: oxygen oxidoreductase: EC 1.10.3.2) is a type of multi copper-containing polyphenol oxidases capable of oxidizing a wide range of polyphenols and other lignin-derived aromatic compounds, and the enzyme is involved in lignin degradation and in the development of soil humus.

漆酶(EC 1.10.3.2,对苯二酚:氧氧化还原酶)是一种含多个铜原子的多酚氧化酶,催化氧化多种芳香族化合物,在木质素矿化降解、腐殖质形成等过程中发挥重要作用。

The compost of agricultural waste materials is the process that under the function of microorganism, the organic matter turn into well-rotted manure by the way of the organic matter being mineralized and humus and harmless.

农业废弃物的堆腐是在微生物作用下,通过发酵使有机物矿质化、腐殖化和无害化而变成腐熟肥料的过程,在微生物分解有机物的过程中,不但生成大量可被植物吸收利用的有效态氮、磷、钾化合物,而且又合成新的高分子有机物---腐殖质。由于这一过程是在微生物分泌酶的作用下酶促反应过程,研究酶活性变化可以从本质上揭示堆腐的生物行为。

The relationship between mantle fluid and U ore-forming was studied preliminarily,according to the results,the author considered theΣCO_2 of mineralizer and heat source came from mantle,which is because upwelling mantle forced by crustal extention and deep-seated faulting produced melt blending with lower crust,during this process,mantle provided the heat and releaseΣCO_2 to crust through outgassing.U mainly came from mantle-curst fluid formed by mantle-curst melt blending and the wall rock during fluid uplift.H_2O mainly generated from mantle fluid and the wall rock during mantle fluid uplift,and partly from atmospheric water in the late period of ore-forming.

初步探讨了地幔流体与铀成矿作用的关系,认为矿化剂∑CO_2和热源来源于地幔,是地壳拉张和深大断裂活动导致部分熔融地幔上涌,与下地壳产生壳幔混熔作用,在混熔过程中提供热量和向地壳&去气&释放∑CO_2;U主要来源于壳幔混熔形成的壳幔混合流体和流体上升途经的围岩;H_2O主要来源于地幔流体、地幔流体上升途经的围岩,在成矿晚期有部分来源于大气降水。

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