蒙古高原北部典型草原区土壤风蚀的~(137)Cs示踪法研究

土壤风蚀是蒙古高原北部典型草原区土地退化的主导因素之一.运用137Cs核素示踪技术对蒙古国巴彦淖尔、哈拉和林的不同牧场和弃耕地土壤风蚀速率进行了研究.巴彦淖尔草原牧场、割草场采样点土壤风蚀速率在64.58~169.07t·km-2·a-1之间,均为微度侵蚀水平.哈拉和林弃耕地年均土壤风蚀厚度4.05mm·a-1,风蚀速率为6723.06t·km-2·a-1,达强度侵蚀水平,自20世纪60年代开垦以来,表层土壤累计风蚀损失17.4cm.牧场和弃耕地风蚀速率的差异表明,在蒙古高原北部典型草原区,人为翻动表土,发展种植业,会导致严重的土壤风蚀发生,而传统牧业生产方式对土壤表层扰动较少,未导致破坏性的土壤风蚀发生,对维持生态系统稳定性有重要作用.

蒙古高原塔里亚特-锡林郭勒样带土壤风蚀速率的~(137)Cs示踪分析

运用137Cs示踪技术,查明了蒙古高原西北-东南向的塔里亚特-锡林郭勒样带区域7个典型景观类型采样点风蚀速率及变化特征,分析了不同区域土壤风蚀速率的主要影响因素.研究表明:各采样点137Cs面积活度介于(265.63±44.91)~(1279.54±166.53)Bq·m-2,差异明显,相应的风蚀速率分别为64.58~419.63t·km-2·a-1.样带上蒙古国境内部分,人类活动较轻微,由北向南,随主要的植被景观和气候指标变化,相应的土壤风蚀速率基本呈逐渐加大趋势,表明该区域土壤风蚀过程主要受自然因素的影响和调节;样带上内蒙古锡林浩特和正镶白旗2个典型草原样点风蚀速率为蒙古国巴彦淖尔典型草原样点风蚀速率的近3倍,除导致风蚀加剧的自然条件差异之外,通过比较两地人口密度和载畜量水平,表明人类扰动是导致内蒙古典型草原样点风蚀加剧的主要因素之一.

风蚀土壤剖面(137)~Cs的分布及侵蚀速率的估算

研究137Cs在土壤剖面上的分布是应用137Cs方法定量评价土壤风力侵蚀的基础.以内蒙古太仆寺旗为研究区,采集了4个样点、共62个土壤样本;使用伽马能谱仪测定了各土壤样本的137Cs活度,计算得到各样点的137Cs总量.研究发现不同土地利用类型/土地覆盖等级的137Cs剖面分布特征差异明显.在低覆盖草地和中覆盖草地土壤剖面中,137Cs活度分布形态为负指数分布;在高覆盖草地土壤剖面中,137Cs活度分布形态在剖面上部为单峰状,单峰后继续为负指数分布;在耕地剖面中,137Cs集中在犁底层以上,且均匀分布.对耕地和草地样点分别使用质量平衡模型和剖面分布模型,可以估算得到农耕地、低覆盖草地、中等覆盖草地等3处样点的侵蚀速率分别为7990,4270和1808Mg/km2·a,分别属于强度侵蚀、中度侵蚀和轻度侵蚀,风力侵蚀强度与地面植被覆盖度呈负相关关系.

Estimation of wind erosion rates by using Cs-137 tracing technique: A case study in Tariat-Xilin Gol transect, Mongolian Plateau

Wind erosion is one of the major environmental problems in semi-arid and arid regions. Here we established the Tariat-Xilin Gol transect from northwest to southeast across the Mongolian Plateau, and selected seven sampling sites along the transect. We then estimated the soil wind erosion rates by using the Cs-137 tracing technique and examined their spatial dynamics. Our results showed that the Cs-137 inventories of sampling sites ranged from 265.63 +/- 44.91 to 1279.54 +/- 166.53 Bq.m(-2), and the wind erosion rates varied from 64.58 to 419.63 t.km(-2).a(-1) accordingly. In the Mongolia section of the transect (from Tariat to Sainshand), the wind erosion rate increased gradually with vegetation type and climatic regimes; the wind erosion process was controlled by physical factors such as annual precipitation and vegetation coverage, etc., and the impact of human activities was negligible. While in the China section of the transect (Inner Mongolia), the wind erosion rates of Xilin Hot and Zhengxiangbai Banner were thrice as much as those of Bayannur of Mongolia, although these three sites were all dominated by typical steppe. Besides the physical factors, higher population density and livestock carrying level should be responsible for the higher wind erosion rates in these two regions of Inner Mongolia.

Distribution characteristics of (CS)-C-137 in wind-eroded soil profile and its use in estimating wind erosion modulus

Due to its inert reaction in soil system and distinctive vertical distribution in soil profile, caesium-137 (Cs-137) has been used as a tracer to assess wind erosion. In this study, 62 soil samples were collected from 4 sampling sites in Taipusi County, Inner Mongolia; Caesium-137 activities for those soil samples were measured using a gamma-ray spectrometry in Sichuan University, Chengdu. Distribution pattern of Cs-137 in vertical soil profile was different for different land use and land cover types. Caesium-137 was distributed homogeneously in plow layer of cropland, and negatively exponential in low to medium cover grassland. Distribution pattern in high covered grassland was represented by a peak at 2-4 cm soil depth followed by a negative exponential curve. Based on those findings, simplified mass balance model was chosen to estimate the rate of wind erosion for cropland, while profile distribution model was used for grassland. Estimated wind erosion rates were 7990, 4270 and 1808 Mg(.)km(-2.)a(-1) for cropland, low cover grassland and medium cover grassland, respectively. Wind erosion intensity correlated negatively with plant cover.

红枫湖沉积物~(137)Cs扩散迁移性研究员

保存在湖泊沉积物~(137)Cs剖面中的环境信息记录，可能因~(137)Cs沉积后的再迁移作用而失真。~(137)Cs吸附动力学及离子交换实验表明红枫湖沉积物中的~(137)Cs绝大部分处于固定态，少量处于交换态和造反性吸附态。同时Cs~（+）浓度很低时，高Cs~(+)浓度下在各吸附态与粘土矿物表面的特定吸附部位之间，通常比较明确的对应关系变得有些模糊。本文以界面过程的数学模型为核心，通过模式分析，重建了红枫湖地区历年的~(137)Cs大气沉降通量值，获得了红枫湖集水区 ~(137)Cs流域侵蚀寄宿时间，约为550年。 ~(137)Cs的扩散和其它沉积后再迁移作用。虽然导致~(137)Cs剖面发生了一些变化，但通过适当的数据处理，仍可从中提取出有价值环境信息。

抗癌药长春新碱及其与微管蛋白相互作用的电化学研究

在0.05 mol/L Tris，0.15 mol/L NaCl溶液中，用吸附伏安法研究长春新碱(VCR)，其峰电位在-1.68 V(vs. Ag/AgCl)，峰电流与1.0*10^{-8}～2.0*10^{-7}mol/L VCR浓度成正比，检测限为7.0*l0^{-9} mol/L，用常规脉冲极谱法、线性扫描和循环伏安法等研究该体系的电化学行为，实验表明，电极还原过程为具有吸附特征的不可逆过程。VCR的吸附符合Frumkin吸附等温式。也研究了VCR与微管蛋白的相互作用。实验表明，VCR与微管蛋白形成一电活性的结合物，这一结合物具有吸附性，且还原过程也为不可逆过程。

太阳耀斑可能的储能过程

本文讨论了太阳活动区和黑子区的无力场的演化。文章分析了无力因子随时间变化的运动学含义,讨论了太阳耀斑具体的储能过程,给出了静力学无力场讨论太阳耀斑储能过程的局限性。最后,又提出了一种子午流场的储能过程。将这些“磁能的储存过程”与“适当的不稳定性导致的爆发过程”相结合起来讨论,就有可能来研究太北北阳耀斑的许多特征。

Molecular dynamics studies on the dislocation gliding near a tilt boundary

The gliding behavior of edge dislocation near a grain boundary(QB) in copper under pure shear stresses is simulated by using molecular dynamics(MD) method. Many-body potential incorporating the embedded atom method (EAM) is used. The critical shear stresses for a single disocation to pass across GB surface are obtained at values of sigma(c)=23MPa similar to 68 MPa and 137 MPa similar to 274 MPa for Sigma=165 small angle tilt GB at 300 K and 20 K, respectively. The first result agrees with the experimental yield stress sigma(y)(=42 MPa) quite well. It suggests that there might be one of the reasons of initial plastic yielding caused by single dislocation gliding across GB. In addition, there might be possibility to obtain yield strength from microscopic analysis. Moreover, the experimental value of sigma(y) at low temperature is generally higher than that at room temperature. So, these results are in conformity qualitatively with experimental fact. On the other hand, the Sigma=25 GB is too strong an obstacle to the dislocation. In this case, a dislocation is able to pass across GB under relatively low stress only when it is driven by other dislocations. This is taken to mean that dislocation pile-up must be built up in front of this kind of GB, if this GB may take effect on the process of plastic deformation.

Effects of g-jitter on the critical marangoni number

A half floating zone is fixed on a vibrational deck, which supports a periodical applied acceleration to simulate the effect of g-jitter. This paper deals with the effects of g-jitter on the fluid fields and the critical Marangoni number, which describes the transition from a forced oscillation of thermocapillary convection into an instability oscillatory convection in a liquid bridge of half floating zone with top rod heated. The responses of g-jitter field on the temperature profiles and flow pattern in the liquid bridge were obtained experimentally. The results indicated that the critical Marangoni number decreases with the increasing of g-jitter effect and is slightly smaller for higher frequency of g-jitter with fixed strength of applied gravity.

Mixed-mode fracture mechanisms near the fatigue threshold of aisi-316 stainless-steel

Near threshold, mixed mode (I and II), fatigue crack growth occurs mainly by two mechanisms, coplanar (or shear) mode and branch (or tensile) mode. For a constant ratio of ΔK_I/ΔK_II the shear mode growth shows a self-arrest character and it would only start again when ΔK_I and ΔK_II are increased. Both shear crack growth and the early stages of tensile crack growth, are of a crystallographic nature; the fatigue crack proceeds along slip planes or grain boundaries. The appearance of the fracture surfaces suggest that the mechanism of crack extension is by developing slip band microcracks which join up to form a macrocrack. This process is thought to be assisted by the nature of the plastic deformation within the reversed plastic zone where high back stresses are set up by dislocation pile-ups against grain boundaries. The interaction of the crack tip stress field with that of the dislocation pile-ups leads to the formation of slip band microcracks and subsequent crack extension. The change from shear mode to tensile mode growth probably occurs when the maximum tensile stress and the microcrack density in the maximum tensile plane direction attain critical values.

防护林带:湍流的数学模型与计算机模拟

虽然防护林用于减小风速、控制热量和水汽传递及污染物扩散、改善气候与环境、增加作物产量等已经有几百年了,但直到近几十年,人们才开始系统地研究防护林空气动力学的遮蔽机制.在本综述中,我们考察了绕防护林带的流动与湍流控制机制,最新的模型与数值模拟研究情况;通过数值模拟与实验数据的比较,来了解防护林带结构与防风效果之间的关系;讨论数值分析如何及为什么能够得到所需要的结果.本文将从多孔隙防护林带流动基本方程组的推导开始,讨论数值模型及模拟过程,对附体与分离流动进行预测;分析了遮蔽机制与动量交换;对风向、防护林密度、宽度和三维性对流动与湍流的影响作了系统的论述.还对热流和土壤水分蒸发的新模型及数值模拟作了简述.最后,我们对网络工作站、群和高性能分布式并行计算机及其对防护林带模型预报能力的提高作了讨论.

燃烧物理学基础