人工湿地塘床系统净化污水的机理研究

人工湿地处理污水实验场经过多年的运行已形成了较稳定的具有多 种生物种类的适合污水处理的生态系统，活水公园人工湿地塘床系统运行时间仅一年，初步显示了湿地生态系统的生物多样性特点。筛选出了菖蒲、芦苇、茭白、香蒲、水竹、马蹄莲、凤眼莲、浮萍、睡莲等适合本地人工湿地塘床系统种植的湿地植物。人工湿地塘床系统是由各种湿地单元与各种各样的高、低等生物和所处的开放式的环境共同构成了较为完整的具有净化污水功能的生态系统，因此，与生物滤池相比，把人工湿地塘床系统称为生态滤池显得更为合适。其出水具有生物安全性。实验结果表明，实验场对生活污水中的COD_(Cr)、BOD_5、TP的去除率在80％以上，对TN的去除率为60.60% ～ 86.4%，细菌总数的去除率为86.9% ～ 99.6%，总大肠菌群的去除率为94.6% ～ 99.7%，其出水水质能够满足二级污水处理的要求。活水公园对枯水期府河水中的COD_(Cr)、BOD_5、TN、TP的去除率在85％以上，总大肠菌群的去除率为99.97%，其净化效果能够满足污水深度处理的需要。湿地植物光合作用向水体供氧能力的试验研究结果表明，在几种光照控制条件静态试验和现场试验中，菖蒲、香蒲、茭白、水竹、凤眼莲等植物植株水面以上的茎、叶在光照条件下进行光合作用时并没有引起根层区水体内溶解氧浓度的升高（氧增），反出现下降（氧亏）。说明这些植物水上部分光合作用对水体DO没有贡献。浮萍光合作时引起氧增的作用较弱，仅维持低水平，试验期间9:00 ～ 15:00的氧增幅度在0.11 ～ 1.13mg/L之间，平均为0.44mg/L。芦苇在9:00 ～ 15:00光合作用时根层区水体氧增幅在-0.20 ～ 1.07mg/L之间，平均为0.30mg/L。上述这些植物植株的水面以下的根、根茎、茎、叶如果暴露在光照条件下时，会进行光合作用，产生的氧直接释放到水体并引起氧增的作用非常明显，试验期间9:00 ～ 15:00的氧增幅度在1.91 ～ 16.1mg/L之间。人工湿地处理污水系统植物床基质内各测点的上、下层COD_(Cr)值虽有一定的差别，但经过成对平均数比较分析发现这种差别并未形成明显的趋势。污水在植物床基质中流动时，随着迁移距离的延长，其中的COD_(Cr)的降解速率呈现先快后慢的趋势，根据动态变化规律，建立了COD_(Cr)在植物床基质层内沿程水平迁移降解动态变化模型：C_L = C_o exp(4.629 * 10~(-5)L~2-0.01567L，0 ≤ L ≤ 100。经验证，模型预测值与实际监测值呈非常显著相关（r ≥ 0.9946 > r_(0.0005(4))，r_(0.0005(4)) = 0.9741)。在人工湿地塘床系统运行监测过程中，发现处于光照下的水体中的pH呈周期性变化，与DO的变化规律相似，在试验期间，9:00 ～ 15:00的pH和DO都呈上升趋势，两者呈协同周期性变化。经相关性回归分析，pH的变化规律与DO呈非常显著相正关，植物床表层渍水区pH与DO的回归关系相关系数r = 0.9129 > r_(0.01(70))(r_(0.01(70)) = 0.302)，植物塘内的pH与DO的相关系数r = 0.8584 > r_(0.01(60))(r_(0.01(60)) = 0.325)，植物床基质层内的pH与DO之间的相关性较差。相关分析结果表明，DO变化幅度大的水体中，pH的变化幅度也就越大，两者之间的相关性也就越显著，这可能与水体中氧化还原电位和水生植物光合作用伴随的代谢活动有关。这种相关性和协同周期性变化具有一定的生态学意义，并会给净化污水的效果产生影响。

甲基对硫磷水解酶结构和功能的研究

本研究以本实验室分离的有机磷农药高效降解菌Pseudomonas sp．WBC-3为材料，通过X-射线晶体学研究确定了甲基对硫磷水解酶（MPH）的三维结构，并在结构基础上探讨了甲基对硫磷水解酶的结构与功能的关系。利用生物信息学手段对Pseudomonas sP.WBC-3中的甲基对硫磷水解酶基因进行分析，推测论H的结构基因的编码序列为398-1393 bp，蛋白大小为331个氨基酸，且具有一个由35个氨基酸组成的信号肤。同时发现，MPH是一个不同于具有相似生物学功能的有机磷水解酶（OPH）的蛋白质，而且在PDB库中尚无与MPH同源性较高的蛋白结构。晶体的生长依赖于高纯度的蛋白质的获得。在本研究中，我们采用阳离子交换树脂和凝胶过滤两步纯化获得了纯度达95％以上的MPH溶液，并采用等离子体质谱仪测定MPH为含锌的金属酶。采用悬滴蒸汽扩散法获得了PI和P43212两种晶型的晶体以及硒标记的MPH晶体。在获得单晶以后，最终利用尸43212晶型的晶体通过多波长反常散射法（MAD）解析了MPH的三维结构。MPH的晶体结构为同源二聚体，具有与OPH类似的二价金属离子组成的活性中心：其中一个单体含有两个锌离子，另一个单体含有一个锌离子和一个锅离子；每个单体的两个金属离子通过AsP 151、His 152、His 302、His 147、His 149、His 234和A印255与蛋白质相连，一个H2O分子桥连于两个金属离子，还有一个H2O分子只与一个金属离子配位。在MPH三维结构知识的基础上，利用分子生物学手段对MPH活性中心附近可能的底物结合氨基酸位点进行了研究。通过定点突变获得了针对Trp179，Phe 196和Phe 119三个位点的六个突变体W179F、W179A、F196W、F196A、FllgW和Fll9A，系统比较了突变体与野生酶的催化动力学特点。结果表明Trp 179，Phel％是MPH活性中心的底物结合部位的关键氨基酸。而Phe 119在与底物结合中的作用不明显。

Initiation and development of water film by seepage

When water seeps upwards through a saturated soil layer, the soil layer may become instability and water films occur and develop. Water film serves as a natural sliding surface because of its very small friction. Accordingly, debris flow may happen. To investigate this phenomenon, a pseudo-three-phase media is presented first. Then discontinuity method is used to analyze the expansion velocity of water film. Finally, perturbation method is used to analyze the case that a water flow is forced to seep upwards through the soil layer while the movement of the skeleton may be neglected relative to that of water. The theoretical evolutions of pore pressure gradient, effective stress, water velocity, the porosity and the eroded fine grains are obtained. It can be seen clearly that with the erosion and re-deposited of fine grains, permeability at some positions in the soil layer becomes smaller and smaller and, the pore pressure gradient becomes bigger and bigger, while the effective stress becomes smaller and smaller. When the effective stress equals zero, e.f. liquefaction, the water film occurs. It is shown also that once a water film occurs, it will be expanded in a speed of (U)(t)/(1 - E >).

A study on water film in saturated sand

Water film can serve as a sliding surface and cause landslides on gentle slopes. The development of "water film" in saturated sand is analyzed numerically and theoretically based on a quasi-three-phase model. It is shown that stable water films initiate and grow if the choking state (where the fluid velocity decreases to near zero) remains steady in a liquefied sand column. Discontinuity can occur in pore water velocity, grain velocity and pore pressure after the initiation of a water film. However, the discontinuity and water film can disappear once the choking state is changed. The key to the formation of water film is the choking in the sand column caused by eroded fine grains.

Characteristic rainfall for warning of debris flows

A characteristic rainfall is introduced to overcome the difficulties encountered in determining a critical rainfall value for triggering debris flow. The characteristic value is defined as the rainfall at which debris-flow occurrence probability shows a rapid increase, and can be used as a warning rainfall threshold for debris flows. Investigation of recorded debris flows and 24-hour rainfall data at Jiangjia basin, Yunnan Province, in southwestern China, demonstrates the existence of such a characteristic rainfall. It was found that the characteristic rainfall corresponds to the daily rainfall of 90% cumulative probability by analyzing the basin's daily rainfall histogram. The result provides a simple and useful method for estimating a debris-flow warning rainfall threshold from the daily rainfall distribution. It was applied to estimate the debris-flow warning rainfall threshold for the Subaohe basin, a watershed in the 2008 Wenchuan earthquake zone with many physical characteristics similar to those of the Jiangjia basin.

降雨作用下滑坡转化泥石流分析研究

对降雨入渗条件下诱发北川县魏家沟泥石流起动的影响因素进行研究。在室内人工降雨试验模拟泥石流起动的基础上,得到魏家沟泥石流起动的临界雨强,并利用FLAC软件建立降雨在坡体中入渗分析的数值模拟模型,分析坡度、雨强、土性参数以及土体饱和度对坡体失稳的影响,坡体在降雨情况下塑性区的出现与延展及坡面拉应力区的发展情况。研究结果表明:降雨入渗后孔隙水压力的升高主要在坡脚附近,即距坡脚1/5的坡高范围内。坡脚处孔隙水压力最大,沿着坡面往上逐渐减小,且坡面较大水平位移也主要集中在1/5坡高范围内。因此,降雨入渗诱发泥石流的起动最先可能出现在坡脚附近,并随着坡度增加、雨强增大、土体饱和度增大,坡体稳定性降低至失稳,促进泥石流的起动。

粉土地层中桶形基础水平动载响应的离心机实验研究

对动载作用下分层土中单桶基础动承载特性、四桶基础动承载特性进行了离心机实验模拟,并对动载后桶基静承载力进行了模拟。结果表明:桶顶与粘土面相同时,有上覆粘土层条件下的桶基动力响应较无上覆粘土层条件下的孔压增长小,但沉陷大;桶顶与粘土层下的砂土面相同时比与粘土面相同时的响应大。桶基在动载后的静承载力得到提高。由于液化区的滤波和对动载的衰减作用,发生沉降的范围有限,离桶壁约一倍桶高距离。超孔隙水压从桶基边沿水平向逐渐衰减,从土面开始往下逐渐衰减到零。桶基周围砂土完全液化的厚度随载荷幅值的增加而增加,最大值约为桶高的40%。

川西亚高山云杉人工林天然更新与生境异质性研究

川西亚高山针叶林是四川森林的主体，是长江上游重要的生态屏障。云杉作为亚高山针叶林人工更新的主要树种，已经在该地区形成了大面积的人工纯林。目前，许多云杉人工林分已经进入更新成熟龄，而这些人工林的持续更新却成为日益凸现的问题。探讨这些云杉人工林的自我更新潜力及云杉种子种群更新特点，可为培育后续森林资源提供科学依据。 本文以川西米亚罗亚高山60a云杉人工林为研究对象，并以该区域内相对稳定的植被群落——天然林为对照，采用种子收集器、土壤种子库筛选、室内外种子萌发实验及野外幼苗调查等方法，从异质性微生境的角度研究了种子雨下落之后，不同微生境对种子库、种子萌发、幼苗建立及分布这一前期更新过程的影响，得出如下结果： 1、通过对川西亚高山60a云杉人工林和天然林6年内种子雨雨量、形态特征、散步动态等的持续观测和综合比较可以发现，云杉林结实特点由于林木自身的特征存在着巨大的变动，2002年和2006年两个种子结实大年内，60a人工林种子雨强度分别达到1088.2 ± 52.3粒/m2和704.3 ± 48.9粒/m2，远大于天然林579.9 ± 28.9粒/m2 和507.5± 30.7粒/m2；且云杉林结实质量优于天然林。60a人工林结实量大，种子质量也最好，相对天然林来说对种群的天然更新以及群落的演替都有最大的贡献潜力。应该说，在川西亚高山云杉人工林的天然更新过程中，种源不是影响天然更新的因素。在种子结实大年里，达到更新成熟的云杉人工林有着优于该地区相对稳定植被群落——天然林的种源优势。至少在种子结实大年，种子供应不是该区域人工林天然更新的限制因子。 2、相对于天然林种子库，人工林种子库在种子萌发前能够有较多的有活力种子。虽然这其中有种子雨输入量有差别的因素存在，但两种林分种子库对种子的保存率的不同才是造成这种差异的主要因素。在人工林中，不同地被类型形成的微生境显著地影响了种子库中种子的密度、垂直分布。有地被物存在的微生境能够将种子雨的大部分截留在地被层中，成为幼苗出现的主要场所；同时不同的地被物对种子的保存情况存在显著的差异，苔藓和凋落物层能都较好地保持其中的种子，到种子萌发前，这两种种子库类型能分别为天然更新提供366.1粒/m2和302粒/m2的有效种子。从这点来看，林下地被物上的种子库能够为天然更新萌发阶段提供数量可观的物质基础。 3、种子的萌发和幼苗的定居是天然更新过程中种子库向幼苗库转化的关键环节。总的说来，米亚罗人工林区60a云杉人工林种子向幼苗的转化率十分低下，凋落物、苔藓、草本、裸地四种主要地被物以及天然林内种子/幼苗的转化率分别仅为2.22%、2.14%、0.57%、0.67%、1.05%。这种低的转化率成为云杉林天然更新的限制性因子。但在现有更新条件下，微生境对这一环节仍然显示出十分显著的影响，表现为凋落物和苔藓对现有更新的新幼苗的保存率高于其它类型及天然林。苔藓和凋落物在种子萌发，幼苗保存，以及幼苗分布上都要优于其它地被物类型；另外，微地形对天然更新过程的影响也很显著，凹立地上更适宜于种子的汇集、萌发和定居。 Subalpine coniferous forests dominate most parts of the forested areas in western Sichuan, and they are important ecological barriers in the upper reaches of the Yangtze River. Picea asperata is one of the keystone spruce species for re-afforestation after felling of the natural forests and there have been a total of ca. 13 000 ha of plantations dominate by this species established. Nowadays, many P. asperata plantations have reached reproductive maturity. However, continued regeneration becomes to an important problem in these plantations. Understanding their self-regeneration potential and the regeneration characteristics of seed populations in spruce plantations of these plantations can have some insights on the management of these plantations and the establishment of following forest resources. A subalpine 60a P. asperata plantation distributed in Miyaluo artificial forest area was studied in this paper, at the same time. Synchronously, a 150a natural spruce forest was studied as comparison. Using seed collecting traps, sieving method for soil seed bank, seed germination experiments and seedling investigations in the field, the effects of heterogeneous microsites on early natural regeneration processes after seed rain were studied, which included seed banks, seed germination, seedling establishment and distribution. The main results are as follows. 1. Through a 6-year long term investigation of seed rain intensities, characteristic, dispersal dynamics of 60a P. asperata plantation, we could concluded that the seed setting properties of 60a P. asperata plantation have a great variation for the characteristics trees. In the mast seed year of 2002 and 2006, the seed rain intensities of plantation was 1088.2 ± 52.3 seeds/m2 and 704.3 ± 48.9 seeds/m2 respectively, which were much greater than that of natural spruce forest (579.9 ± 28.9 seeds/m2 in 2002, and 507.5± 30.7 seeds/m2 in 2006). Furthermore, the quality of seed rain in P. asperata plantation was better than that of natural spruce forest. Contrasting with natural spruce forest, 60a P. asperata plantation has a greater potential on natural regeneration of P. asperata population and succession of community for the reason of greater seed rain intensities and better seed quality. We can confirm that seed source was not a limiting factor which influences the natural regeneration progress of P. asperata population distributed in subalpine mountain zone, at least in the mast seed year. 2. Contrasting with natural spruce forest, P. asperata population had more viable seeds in seed bank before the germination. Although the difference of seed rain intensities of two forests has effect on this phenomenon, the difference of seed conservation ability in two forests was the main factor. In the P. asperata plantation, the seed densities and seed vertical distribution pattern were significant effected by the microsites, which posed by different ground cover types. In other word, Microsite with ground covers can obstruct most seeds and keep them in ground cover layer from seed rain, and these ground covers would be the main site for seed occurrence. There was a significant difference about seeds conservation ability among these ground covers. Litter and moss could better conserve P. asperata seeds which distributed in this two covers. Seed banks exist in litter and moss ground cover types could respectively provide 302seed/m2 and 366.1seed/m2 for natural regeneration before the seed germination. From this point of view, we could conclude that ground covers can ensure considerable numbers of seeds for the germination process. 3. Seed germination and seed establishment are key steps that the seeds invert to seedlings in natural generation process. In sum, the seed/seeding transform rate in 60a P. asperata plantation distributed in Miyaluo artificial forest area is very low. the seed/seeding transform rates in litter, moss, herb, soil surface and natural spruce forest were 2.22%、2.14%、0.57%、0.67%、1.05%, respectively. The low transform rate become to a limiting factor of P. asperata natural regeneration process. However, under the existing conditions of natural regeneration, microsit still had significant effect on this transform. The states of Seed germination, new seedling conservation, and older seedling distribution in litter and moss were better than in any other ground cover type or natural spruce forest. In addition, the micro-relief has significant effect on natural regeneration process. Concave site was more suitable for seed collection, seed germination and seedling distribution.