黄土高原水蚀风蚀交错区坡地土壤剖面饱和导水率空间异质性

在黄土高原水蚀风蚀交错区坡面(40 m×350 m)尺度上进行网格(10 m×10 m)取样,用经典统计学和地统计学相结合研究了180个土壤剖面(0-200 cm)各土层扰动土饱和导水率(Ks) 的空间异质性及分布格局。结果表明: 0-20 cm土层的Ks值(5.36×10^-3 cm/s)最大,>20-200 cm各土层的Ks值均小于表层,其值介于4.32×10^-3-4.76×10^-3 cm/s之间。各土层Ks的变异程度相近,均属于中等变异。>20-200 cm各土层Ks 的Kriging 插值图分布格局也表现出一致性,因此可用>20-40 cm土层的Ks值来代表深层Ks值对土壤水分运动进行模拟。除了0-20 cm 的Ks的基台值(C +C₀)为0.154,其它各土层基台值介于0.202-0.276之间,说明0-20 cm的Ks空间异质性小于>20-200 cm各土层。从比值C/(C+C₀)来看, 0-20 cm属于中等自相关,>20-200 cm土层属于强的空间自相关性,同样也验证了黄土高原水蚀风蚀交错区土壤剖面饱和导水率具有空间变异特征。     

液氮冻伤术建立动脉粥样硬化破裂斑块及血栓模型

目的创建一种操作简单、经济实用的动脉粥样硬化（AS）破裂斑块及血栓动物模型。方法21只雄性纯种新西兰白兔随机分为两组：液氮冻伤＋高脂喂养组（A组=11只）和高脂喂养组（B组=10只）。A组实施右颈总动脉内膜液氮冻伤术结合高脂饲料喂养,B组单纯给予高脂饲料喂养。8周末以液氮激发斑块破裂,激发前后分别采血检测血脂、hsC-RP、MMP-9及PAI-1水平;激发48h后处死所有动物,取出右颈总动脉作HE染色及免疫组化染色等,光镜及电镜观察破裂斑块及血栓形成情况。结果8周后兔血脂水平明显升高;激发后血浆hsC-RP、MMP-9及PAI-1均明显升高;所有A组兔子的右颈总动脉均可见AS破裂斑块及血栓形成,而B组兔子未见斑块或血栓形成;所建立的破裂斑块在组织结构、细胞构成、生长特征和脂质沉积方面与人类斑块相似。结论液氮冻伤术能简便、快速、高效地建立AS破裂斑块及血栓模型,从而为研究人类AS破裂斑块及血栓形成的机理和药物干预治疗提供了一种新型动物模型。     

SARS-CoV细胞空斑试验

目的建立适用于生物安全三级实验室操作的SARS．CoV空斑试验方法。方法SARS－CoVl0倍系列稀释接种Vero－E6细胞,用0．6％琼脂糖覆盖中性红着色（琼脂糖．中性红法）或覆盖1％甲基纤维素,4％甲醛固定,结晶紫染色（甲基纤维素－结晶紫法）,空斑计数。结果琼脂糖－中性红法病毒滴度为6．14Lg pfu／mL,甲基纤维素－结晶紫法病毒滴度为6．57Lg pfu／mL。结论二种空斑试验方法相比,病毒滴度无明显差异。甲基纤维素－结晶紫空斑试验法形成的空斑比琼脂糖－中性红法清晰、操作简单安全、结果可长期保存。     

Effects of vegetation cover and precipitation on the process of sediment produced by erosion in a small watershed of loess region

With growing concerns over changes of the living environment and ecological environment, more and more scholars have focused their researches on understanding how vegetation covers and atmospheric conditions respond to soil erosion in watersheds. Former studies show that both the natural factors such as precipitation, vegetation, slope of terrain, soil properties and human activities are the main factors to affect the amount of sediment produced by erosion in the watershed, and there are special conditions of climate and soil that are unique to loess areas for water and soil conservations. Thus the relationships between soil erosion and vegetation and precipitation are very complicated and interesting. As a loess area, the Lüergou watershed with the area of 12.1 km2 lies in west of China. The watershed was a key area of high water and soil erosion forty years ago, but the area of vegetation cover has become larger because of highly effective methods of water and soil conservation. In the factors affecting the amount of sediment produced by erosion in the study area, which is more important for soil erosion: vegetation cover or precipitation? The experts, community has discussed this question for a long time. And the Lüergou watershed has become the natural and ideal test watershed. Based on water observation data, climate data and NOAA/AVHRR NDVI images collected from 1982 to 2000 in the Lüergou watershed of loess areas, analyses of the correlation and multi-variable regression were used to discuss the relationships among the amount of sediment produced by erosion, water indexes, precipitation factors and vegetation cover. The conclusions showed that with the increase of precipitation indexes and the decrease of plant indexes, and the amount of sediment produced by erosion in the study area would become larger. In order to distinguish the influences of erosion due to human activity and natural factors, the paper introduced multi-variable regression method by standardization data to determine the relative contributing ratio to soil erosions in the study area. The conclusions showed that the contributing ratio of vegetation cover and precipitation changes were 45.7% and 54.3%. It was obvious that the influences of precipitation were larger than those of vegetation for the soil erosion in the study area.     

川西低山区土壤侵蚀经济损失及其评估模式——以名山县蒙山为例

借助中国坡面土壤流失预报方程（CSLE）估算研究区的土壤侵蚀量,并重点对该区土壤侵蚀生态经济损失进行计算和分析,结果表明研究区土壤侵蚀的直接经济总损失为1776．387万元,占同期当地第一产业总产值的5．001％,其中经济损失最严重的是林地和坡耕地,其次探讨了水土流失生态．经济面积边际损失比的概念,通过分析得出侵蚀所造成的直接经济边际损失每增加1万元,在此基础上,其生态价值的边际损失将增加76—91元。     

辽宁省生态系统敏感性评价

根据辽宁主要生态环境问题的形成机制,分析了生态系统敏感性的区域分异规律,并对多种生态环境问题的敏感性进行了综合分析。结果表明,全省处于轻度至高度敏感区域,高度敏感区、中度敏感区、轻度敏感区分别占全省陆域面积的34.00%、62.66%和3.34%。高度敏感区分布在辽东山地丘陵、辽东半岛、辽西低山丘陵、辽西北、柳绕地区和大洼县。辽东山地丘陵、辽东半岛和辽西低山丘陵主要是土壤侵蚀高度敏感。辽西北和柳绕地区主要是土地沙漠化高度敏感。大洼县是土壤盐渍化高度敏感。     

GIS支持下的土地利用与土壤侵蚀强度相关性研究--以陕北黄土高原为例

依托GIS软件作为技术平台,采用网格地图与数学分析方法,研究了陕北黄土高原土地利用强度与土壤侵蚀强度之间的相互关系。结果表明,陕北黄土高原土壤侵蚀强度和土地利用强度呈高度正相关,说明土地利用强度是导致陕北黄土高原本区域土壤侵蚀的重要驱动力。回归分析发现,在自然因子综合作用下,土地利用强度对土壤侵蚀强度的影响呈现不同状况,地势越平坦、气候越湿润的地区人类活动对土壤侵蚀强度的影响越小,反之亦然。     

Effects of aquatic macrophytes on organic matter deposition,resuspension and phosphorus entrainment in a lowland river

1. Although macrophytes play a key role in the structure and functioning of lowland rivers, most of the basic plant, hydrodynamic and sediment‐water interactions have only been described qualitatively. We therefore studied quantitatively, the seasonal dynamics of matter deposition and mobilisation inside and outside (free path) a representative patch of arrowhead, Sagittaria sagittifolia, in the lowland River Spree, NE Germany, in August 2006. Our in situ study combined resuspension experiments, a hydrodynamically calibrated erosion chamber and concurrent measurements of the prevailing flow characteristics and bed load. 2. Increasing entrainment rates (E) of particles (E_SPM) and total P (E_TP), with increments of shear velocity (U_*) from 0.53 to 2.42 cm s^?1, were significantly higher inside the plant patch than outside. Indeed, E_SPM and E_TP at the lowest U_* were 8‐ and 12‐fold higher inside than outside the patch, reflecting the resuspension potential of the upper nutrient‐enriched layer and the extent of pulsed P inputs even at small increases in U_*. 3. Vertical distribution of velocity (u) revealed a flow pattern of a mixing layer inside the S. sagittifolia patch, and that of a boundary layer in the free path. The highest gradient of u in the mixing layer was located in the water column at about 0.5 m depth, whereas the highest gradient of u for the boundary layer was found near the riverbed. The maximum of U_* (1.65 cm s^?1) was only 4 mm above the sediment. 4. A plant mosaic provides a low‐energetic environment promoting extensive particle trapping and the accumulation of a fine‐grained, nutrient‐enriched sediment, and forming a large resuspension potential. Consequently, after plant decay and the concomitant increase of U_* this material is preferentially entrained at higher rates. Hence, the key role of submerged macrophytes in lowland rivers is more directly related to modifying the dynamic equilibria between vegetation trapping and resuspension, than to the retention of nutrients, particularly P, and the reduction of P loads downstream to other waters.     

水蚀风蚀交错区柠条锦鸡儿叶片比叶面积和营养元素变化动态

通过对黄土高原水蚀风蚀交错区主要生长月份柠条锦鸡儿(Caragana korshinlii Kom.)叶片比叶面积(SLA)和矿质元素含量的测定,探讨其对生境条件及生长时间的响应规律,结果表明:不同生境柠条锦鸡儿叶片SLA随生长月份的变化趋势基本一致,但变化差异不显著;不同生境叶片有机碳(C)含量变化差异不显著;叶片全氮(N)含量、全钾(K)含量对生长月份的变化响应明显,变异幅度较大,而随生境条件发生的变异较小;叶片全磷(P)含量在不同生境随着生长月份发生的变异较大。不同生境叶片N/P随月份发生的变异较大、C/P的变异较小;叶片C/N、C/K在不同生境间无明显差异,但均随生长月份而产生较大变化,叶片N、P、K的含量与SLA相关性不明显。所以,生境条件和生长时间是柠条锦鸡儿叶片结构特性和养分组成发生变化的重要原因,其叶片比叶面积与矿质养分含量受外界环境因子和自身发育状况的共同调控。     

两种HSV-1及猴B病毒相关抗体测定方法的比较

目的以人单纯疱疹病毒（HSV-1）做为抗原,利用空斑法和IFA法比较猴BV和人HSV-1阳性血清两种不同血清的中和能力的差异,建立一种实用、准确、可靠的病毒毒力的检测方法。方法首先,将HSV-1病毒悬液作连续的10倍稀释,取1 mL接种于已经长成单层的Vero-E6细胞上,用1%甲基纤维素覆盖,待其出现蚀斑后计数,算出病毒悬液中每毫升所含蚀斑单位,即滴定出HSV-1的TC ID50。同时,用免疫荧光方法（IFA）对猴和人疱疹阳性血清进行滴定,得到其血清的效价。其次,用滴定出的病毒液分别与两种阳性血清体外中和后,接种到单层的Vero-E6细胞上,用1%甲基纤维素覆盖,待其出现蚀斑后计数。最后,计算出其蚀斑减少率。结果用1%甲基纤维素作覆盖层的蚀斑数量平均为10-5PFU,能形成115-116个/mL蚀斑,形状呈黍米大小的规则圆形,其蚀斑边缘清晰。IFA滴定的人HSV-1阳性血清与猴BV阳性血清的中和抗体均为1∶80。人HSV-1和猴BV两种阳性血清的空斑减少率均为100%。结论确定了利用1%甲基纤维素做为覆盖层可得到清晰可靠的蚀斑,由此方法检测到用人HSV-1可以代替猴B病毒,筛查猴B病毒抗体。且为将来进行药物筛选和中和实验中利用病毒空斑法建立方便、可靠的方法。