构件预挤压孔的工艺弹塑性和残余应变分析方法

在对工艺应力进行理论分析的基础上,提出了一种构件预挤压孔的工艺弹塑性和残余应变分析方法,通过采用释放残余应变的方法和单光束激光散斑干涉术,分析了三种不同挤压量带孔铝板的预挤压孔对称面上的残余应力,验证了这种分析方法的可行性。     

A Sensitive Spectrophotometric Determination of Nitrite in Water and Soil

A highly sensitive spectrophotometric method for the determination of nitrite in water and soil has been developed. The reaction of nitrite with acidified potassium iodide to liberate iodine which oxidizes leuco‐crystal violet (LCV) to form crystal violet having absorption maxima at 590 nm forms the bases of this method. In aqueous medium the system obeys Beer's law in the range of 0.1 to 1.0 μg per 25 mL (0.004–0.04 ppm), while in an extractive system the range is 0.025–0.25 μg in 100 mL (0.00025–0.0025 ppm). The molar absorptivity and Sandell's sensitivity were found to be 1.54 × 10⁶ 1 mol^?1 cm^?1 and 44 pg cm^?2, respectively.     

喷网锚在加筋土挡土墙加固中的应用

根据山东省淄博市梧台立交桥加筋土挡土墙加固的工程实际,结合理论计算,讨论了高压注浆提高锚固力的原理,提出了局部采用双层钢筋网的喷浆支护方法.结果表明,该加固方法有效地限制了墙体的侧向位移,加固效果良好,适用于失稳挡土墙加固.     

对饱和土孔隙压力系数的探讨

在三轴试验基础上提出采用归纳定义方法来确定孔隙压力关系方程，其结论与根据弹性力学理论推导的结论是一致的，并指出了弹性力学理论推导过程中存在的不严密之处和理论适应性问题．     

富钾硅复合物对水稻土中有效K，Si，Ca，Mg的影响

富钾硅复合物为绿豆岩煅烧产物，本文通过盆栽对比实验研究它对水稻土中有效K，Si，Ca，Mg的影响，结果表明：水稻土中施入K，Si，Ca，Mg后，被水稻带走部分养分，土壤养分仍有变化；尽管富钾硅复合物中的K，Si，Ca，Mg多为枸溶性养分，但均能供给水稻生长发育需要，并具有一定后效．     

水土保持的生态效益价值分析--以重庆市南岸区为例

在基于GIS技术的水土保持项目规划基础上，探索生态经济学的视角来分析评价城市化发展过程中水土保持工作的生态效益，并以货币的价值形式测评．测评结果，项目区水土保持的直接经济价值预测值为1207．61万元，生态经济价值预测3017．75万元，潜在的生态价值是直接经济收入的2．5倍．因此，在水土保持规划过程中，城区的生态效益价值分析是不能忽视的．     

某滑坡滑带非饱和土强度特性试验研究

借助专门的能够控制吸力的四联式非饱和土直剪仪,对清江水布垭坝区古树包滑坡滑带土的重塑样进行了一系列抗剪强度试验,验证了F red lud提出的非饱和土抗剪强度公式对滑带土的适用性,求出了该滑带非饱和土的强度参数;通过在一定基质吸力条件下量测含水率-固结压力之间的关系,指出土-水特征曲线与固结压力相关的特性。     

^210Pbex depth distribution in soil and calibration models for assessment of soil erosion rates from ^210Pbex measurements

Throughout the past decade, the potential for using nuclear weapon-produced 137Cs ( half-life 30.2 a) fallout to quantify soil erosion rates on both cultivated and uncul- tivated lands for medium-term timescales (≈ 40 a) has been successfully demonstrated in a wide range of envi- ronments in different regions of the world[1—6]. Because in difficulties of distinguishing Chernobyl-derived compo- nent from total 137Cs input in many parts of Europe, and in measuring low activity samples of…     

Triassic U-Pb age for zircon from granites in the Tonghua area and its response to the Dabie-Sulu ultrahigh-pressure collisional orogenesis

Single-grain zircon U-Pb dating was carried out to constrain the emplacement timing of granitic plutons at Chaxinzi, Xiaoweishahe and Longtou in the Tonghua area, south of Jilin Province. The results show that these plutons formed in the Triassic with ages of 203—217 Ma. Geological and geochemical characteristics indicate that the plutons are composed of quartz diorite and granite. The former was derived from partial melting of mafic lower crust, whereas the latter originated from thickened crust with garnet as the residue in the source. It appears that protoliths of these two types of granitits are different although they have the same emplacement age. Considering that these plutons are petrologically different from the coeval granites in the Xingmeng (Xing‘an-Mongolian) to Jihei (Jilin-Heilongjiang) orogenic belt in the north, it is suggested that their formation was related to the Dabie-Sulu ultrahigh-pressure collisional orogenesis since their ages are only 10—20 Ma younger than timing of the ultrahigh-pressure metamorphism, but comparable to that of the first rapid exhumation of the ultra-high-pressure metamorphic rocks and the emplacement of the post-collisional granites.     

Loess-soil sequences in southern Anhui Province： Magnetostratigraphy and paleoclimatic significance

Two parallel loess-soil sequences from Xuancheng and Fanchang in southern Anhui Provinces are dated using geomagnetic and luminescence methods.The Brunhes/Matuyama(B/M) reversal boundary is recognized within the lower part of the so-calles Vermiculated Red Soil (VRS) in the Xuancheng section while the entire Fanchang sequence is of Brunhes age.This indicated that the most recent VRS in southern China,a stratigraphic marker and an indication of extremely warm-humid conditions,was formed during the middle Pleistocene,chronologically correlative with the S4 and S5 soil units in northern China.Microscopic and sedimentologic in vestigations reveal that eolian deposition started in this region at about 0.85 MaBp,roughly synchronous with the well-known Mid-Pleistocene climate change of global significance.The strengthening of both summer and winter monsoon circulations and the consequent river hydrological changes at that time would have provided favorable conditions for sustained eolian deposition in the middle-lower reaches of the Yangtze River since 0.85 MaBP.