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利用分光光度计比色法测定了温度、pH值和Hg^2+等9种金属离子对体长24.2cm±0.7cm仿刺参(Apostichopus japonicus)消化道中蛋白酶活性的影响。结果表明,蛋白酶的最适温度为40℃,对热不稳定,最适pH为7.2。Hg^2+,Mn^2+,Ag^+,Pb^2+,Ba^2+,Ca^2+对蛋白酶的活性有抑制作用,抑制作用由强至弱依次为Hg^2+〉Ag^+〉Mn^2+〉Pb^2+〉Ca^2+〉Ba^2+,其中Hg^2+和Ag^+与对照差异极显著(P〈0.01),表现出极强的抑制作用;Cu^2+,Zn^2+,Mg^2+则对酶活有一定的促进作用,其促进作用大小依次为Mg^2+〉Zn^2+〉Cu^2+,Mg^2+与对照差异显著(P〈0.05)。 相似文献
115.
据开发应用水产饲料膨化机实践,初步论述了膨化机生产能力与动力匹配,螺杆设计参数长径比,物料在腔内滞留时间,膨化腔设计及其温度调控,并提出改进设计的见解. 相似文献
116.
光生物反应器中光衰减特征与螺旋藻生长动力学研究 总被引:3,自引:0,他引:3
分析了光照强度在光生物反应器中的分布特征,结果表明,当光波长及光传播的路径确定时,光生物反应器中光衰减特征主要受培养物生物量浓度的影响,由回归的模型对实验数据的拟合可分析光衰减特征与培养物生物量浓度的相关性,为光生物反应器中平均光照强度的确定奠定基础。在光生物反应器中,当营养底物和环境温度不是螺旋藻生长限制因子时,通过平均光照强度对螺旋藻比生长速率的影响分析,结果表明,在实验条件下,螺旋藻比生长速率与平均光照强度的动力学模型可用Aiba光生长抑制方程描述,光亲和系数Ks为238.29umol/(m^2.s),光抑制系数Ki为0.00493s.m^2/umol,光生物反应器中螺旋藻生长的饱和光照强度出现在190-272umol/(m^2.s)的范围内。 相似文献
117.
Moo Hee Kang Hyun-Chul Han Hyesu Yun Gee Soo Kong Kyong O. Kim Youn Soo Lee 《Marine Geophysical Researches》2007,28(3):257-269
A seamount chain with an approximately WNW trend is observed in the northeastern Ulleung Basin. It has been argued that these
seamounts, including two islands called Ulleung and Dok islands, were formed by a hotspot process or by ridge related volcanism.
Many geological and geophysical studies have been done for all the seamounts and islands in the chain except Anyongbok Seamount,
which is close to the proposed spreading ridge. We first report morphological characteristics, sediment distribution patterns,
and the crustal thickness of Anyongbok Seamount using multibeam bathymetry data, seismic reflection profiles, and 3D gravity
modeling. The morphology of Anyongbok Seamount shows a cone shaped feature and is characterized by the development of many
flank cones and flank rift zones. The estimated surface volume is about 60 km3, and implies that the seamount is smaller than the other seamounts in the chain. No sediments have been observed on the seamount
except the lower slope, which is covered by more than 1,000 m of strata. The crustal structure obtained from a 3D gravity
modeling (GFR = 3.11, SD 3.82 = mGal) suggests that the seamount was formed around the boundary of the Ulleung Plateau and
the Ulleung Basin, and the estimated crustal thickness is about 20 km, which is a little thicker than other nearby seamounts
distributed along the northeastern boundary of the Ulleung Basin. This significant crustal thickness also implies that Anyongbok
Seamount might not be related to ridge volcanism. 相似文献
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-The hydrodynamic forces on a smooth inclined circular cylinder exposed to oscillating flow were experimentally investigated at Reynolds number (Re) in the range 40000-200000 and Keulegan-Capenter number (KC) in the interval from 5-40. In the test, Re number and KC number were varied systematically. The inertia force coefficient (Cu) and the drag force coefficient (CD) in Morison equation were determined from the measured loads and the water particle kinematics. In this analysis a modified form of Morison equation was used since it uses the normal velocity and acceleration. Thus, the applicability of the Cross Flow Principle was assumed. This principle, simply stated, is as follows: the force acting in the direction normal to the axis of a cylinder placed at some oblique angle with the direction of flow is expressed in terms of the normal component of flow only, and the axial component is disregarded. Both the total in-line force coefficient (CF) and transverse force (lift) coefficient (Cf) were analyzed 相似文献
120.
K. S. Jeong J. K. Kang K. Y. Lee H. S. Jung S. B. Chi S. J. Ahn 《Geo-Marine Letters》1996,16(2):123-131
In the northwestern margin of the Clarion and Clipperton fracture zones, manganese nodules are latitudinally variable in character, resulting from the progressive (re)generation of nodules since the Oligocene as the Pacific Plate migrates northwestward beneath the equatorial production zone. Complemented by the surface water productivity, bottom current activities have concentrated nodules in the Oligocene to Miocene siliceous clay. Resedimentation processes on nodules form three types of nodules with concentric structures and 10 Å-manganaterich bottoms, by periodically causing the diagenetic growth of nodules within the topmost sediment layer. 相似文献