基于热湿交换理论的巷道风流温、湿度影响因素研究

为了研究巷道风流参数的影响因素、预测风流温湿度的变化规律,结合热湿交换理论,建立了风流与围岩壁面之间热湿交换的数学模型,以及贴体坐标系下围岩内部温度场的导热微分方程;利用数值方法,将围岩内部的导热问题与影响风流参数变化的热湿交换问题耦合起来,并以大柳塔煤矿52505综采工作面为例进行计算,得到了与实测参数较为一致的模拟结果,验证了该数值方法的有效性。研究结果表明:风流温度受原始岩温、入风流温度、局部热源强度等因素的影响,风流相对湿度与入风流温、湿度以及井下湿源的数量和强度有关;巷道壁温作为将围岩温度场与风流参数之间关联起来的主要因素,对模拟结果影响较大,其数值取决于壁面与风流之间热湿交换以及围岩原始岩温。     

不同组合比例煤岩的电荷感应与微震规律试验研究

针对煤岩在屈服破坏过程中有微震和电荷信号产生这一特征,利用自行设计的微震和电荷感应信号监测试验系统,分析不同组合比例煤岩在变形破裂过程中微震和电荷信号的变化规律。研究结果表明:微震和电荷信号是低频信号,信号频谱集中分布在0~80 Hz,应力突变与微震信号和电荷信号的产生及变化有较好的一致性;随着“煤-岩”高度比的增加,试样的单轴抗压强度减小,试样屈服破裂时微震和电荷信号幅值增大,同步性增强,试件破坏的突发性增强;试件破坏过程中电荷比微震信号数更多,初次明显的电荷信号也早于初次明显的微震信号。     

爆破荷载作用下隧道中隔岩稳定性研究

为研究爆破动力荷载作用下隧道中隔岩稳定性评价标准,以福州地铁2号线为工程背景,结合强度折减动力分析法和数值模拟,同时考虑中隔岩塑性区贯通、位移超过规范值、计算不收敛3种判据,综合对隧道中隔岩进行动力安全系数分析,研究隧道不同净距、不同开挖进尺后行洞隧道爆破开挖对隧道整体安全系数的影响。研究结果表明:中隔岩塑性区贯通时特征点位移和规范中位移限值较为接近,可共同作为评价中隔岩稳定性的最终评价标准;隧道净距越大、进尺越小,隧道整体安全系数越高;对围岩质量较差且净距小于1.6 m的双线隧道进行爆破开挖时,建议将爆破进尺控制在2 m以内。研究结果可为类似工程提供理论参考依据。     

低磷胁迫下不同水稻品种根系吸收能力差异的生理与遗传本质

在低磷（1mg L-1)和适磷水平（10mg L^-1)下，分别以混合培养方式研究了粳稻京系17（Oryza sativa ssp.japonica)(JX17)和粘稻窄叶青8号（Oryza sativa ssp.indica)(ZYQ8)对磷营养的反应。结果表明，低磷胁迫下，JX17较ZYQ8吸收更多磷素，干物重也显著增加。相反，ZYQ8则受到更强的磷胁迫，吸磷量和干物重降低，主要是因为JX17具有较高的吸磷速度，单位根长吸磷量大，即根系高亲和力磷酸盐转运蛋白表达强，最大限度地吸收可能利用的磷素，从而改善植株营养状况，同时又有较多的磷被分配到根系，使根第，根表面积和根干重相应提高，进一步增加了其在低磷胁迫条件下的竞争磷营养的优势。图3表2参17     

厌氧条件总磷还原为磷化氢种泥筛选及功能菌株鉴定

厌氧除磷是一种高效、节能、低耗的方法。获取经济、方便、高效的种泥是实现该方法的前提,种泥中产生磷化氢功能菌株的组成及特性是提高处理效能和开发新工艺的基础,目前此研究未见有关报道。本研究依据厌氧除磷理论,利用厌氧培养反应瓶、筛选培养基和微生物筛选、分离、鉴定的方法。以A2/O厌氧池、污泥浓缩池污泥、养殖场新鲜猪粪、鸡粪、牛粪及鸭粪为研究种泥,通过跟踪厌氧培养过程培养液中总磷的去除率和吸收液中磷化氢的生成量筛选出最佳种泥,并对最佳种泥的菌株进行筛选、分离和鉴定。结果表明,6种泥中鸡粪的厌氧除磷能力最强,鸭粪能力最弱,浓缩池中的污泥和猪粪次之,牛粪及厌氧池污泥有一定的作用。本试验条件下鸡粪是厌氧除磷的最佳种泥。经过3个周期的厌氧培养,6种泥培养液总磷的去除率和吸收液中磷化氢的含量随培养时间增长都有不同程度增加。鸡粪的最佳培养时间为5d。鸡粪培养液经21d培养后分离到1株芽孢杆菌属、1株假单胞菌属及2株肠杆菌科,明确了2株肠杆菌科中1株为埃希氏菌属另1株为柠檬酸杆菌属。     

常张高速公路岩石边坡仿原生态植被恢复技术的应用研究

介绍了常张高速公路岩石边坡仿原生态植被恢复技术的施工工艺、新型的生态防护技术与传统的边坡防护相比较,具有投资省、见效快,且能稳定表层边坡,综合造价仅为客土喷播植草的50%～60%,能在短期内使边坡整体环境景观效果与周边协调一致,尤其适宜于对客土喷播植草难以成活的极陡边坡(坡率大于1∶0.75)的生态防护,探索出了一条适合我省实际情况的且成本低、效果好的新的生态防护模式.仿原生态植被恢复技术是常张高速公路生态防护措施的典型代表,对今后我省山区高速公路生态防护建设具有一定的指导意义.     

Effect of low-molecular weight organic acids on phosphorus release and phytoavailabilty of phosphorus in phosphate rocks added to soils

Phosphorus (P) is critically needed to improve soil fertility in many parts of the world. The use of water-soluble P fertilizers, e.g., single super-phosphate and triple super-phosphate in developing countries to improve crop production has been limited primarily by their high cost. The presence of indigenous phosphate deposits in some countries provides an incentive for direct application or local chemical treatment at low cost to improve the solubility of low reactive phosphate rocks (PRs). The use of naturally occurring low-molecular weight organic acids (LMWOAs) that are produced in soil as microbial metabolites or plant exudates from dead or living cells represents a new perspective in PR research. The LMWOAs contain various functional groups that may play a significant role in PR dissolution. Little information is available, however, about the potential of LMWOAs in releasing P from PRs. This study reports P release from 12 PRs, four each of low, medium, and high reactivity, obtained from various deposits (Kodjari, Tahoua, North Carolina, Gafsa, Khouribga, Tilemsi Valley, Central Florida, Sechura, Minjingu, North Florida, Hahotoe, and Parc W) using nine LMWOAs containing mono-, di-, and tri-carboxylic groups and a mineral acid (H₂SO₄). Laboratory studies showed that the organic acids are effective in releasing P from low and medium reactive PRs, but very ineffective in releasing P from high reactive PRs. The average amounts of P released by all the organic acids from the three types of PRs were 65.5 mmol kg⁻¹ PR from the low reactive PRs, 55.1 mmol kg⁻¹ from the medium, and 11.1 mmol kg⁻¹ from the high; those released from across all the PRs were 21.9 by the mono-carboxylic acid group, 54.2 by the di-carboxylic acid group, and 57.0 mmol P kg⁻¹ by the tri-carboxylic acid group. The P released was negatively correlated with the equilibrium pH, but positively correlated with Ca released from the PRs. Laboratory incubation studies on the release of P from PRs added to soils with or without organic acids and incubated at 25 °C for 15, 30, and 45 days showed that the percentage of plant-available P released varied considerably from 0.95 in the Kodjari PR to 40.1% in the North Carolina PR and was related to PR reactivity. A greenhouse study with corn (Zea mays L.) grown for 60 days on soils treated with PRs or with PRs mixed with organic acids showed that corn response to addition of oxalic or citric acid varied with P rates and PR sources, suggesting that organic acids have potential as amendments for increasing plant-available P in PR-treated soils.     

等度洗脱快速分离SO4^2-、PO4^3-的新方法和

多聚磷酸盐在分离柱上保留能力强，不易洗脱，因此采用离子色谱分析测定多聚磷酸盐时大多采用梯度淋洗的方法，实现多聚磷酸盐、硫酸盐的分离。具体方法为采用美国戴安ICS-1000型离子色谱仪，METROSEP A Supp 5 100型分离柱，36mmol LiOH＋2％乙腈的淋洗液等度淋洗；进样20μL，流速0．7mL／min，8min内实现SO4^2-：PO4^3-和P2O7^4-的完全分离，保留时间分别为3．9，4．9和6．4min；检出限分别为4、11和17ng／L；加标回收率分别为96．88％，96．41％和98．48％。     

A triple-continuum approach for modeling flow and transport processes in fractured rock

This paper presents a triple-continuum conceptual model for simulating flow and transport processes in fractured rock. Field data collected from the unsaturated zone of Yucca Mountain, a repository site of high-level nuclear waste, show a large number of small-scale fractures. The effect of these small fractures has not been considered in previous modeling investigations within the context of a continuum approach. A new triple-continuum model (consisting of matrix, small-fracture, and large-fracture continua) has been developed to investigate the effect of these small fractures. This paper derives the model formulation and discusses the basic triple-continuum behavior of flow and transport processes under different conditions, using both analytical solutions and numerical approaches. The simulation results from the site-scale model of the unsaturated zone of Yucca Mountain indicate that these small fractures may have an important effect on radionuclide transport within the mountain.     

厌氧／缺氧SBR反硝化除磷效能的研究

采用厌氧 缺氧SBR反应器对以硝酸盐作为电子受体的反硝化除磷过程进行了研究。结果表明 ,反硝化聚磷菌完全可以在厌氧 缺氧交替运行条件下得到富集。稳定运行的厌氧 缺氧SBR反应器的反硝化除磷效率 >90 % ,出水磷浓度 <1mg L。进水COD浓度对反硝化除磷的效率影响很大 ,在COD浓度 <180mg L时 ,进水COD浓度越高 ,除磷效率也就越高。较高浓度的进水COD浓度将导致有剩余的COD进入缺氧段 ,对反硝化吸磷构成不利影响。污泥龄为 16d时 ,厌氧 缺氧SBR反应器取得稳定和理想的反硝化除磷效果。污泥龄减少到 8d ,由于反硝化聚磷菌的流失导致反硝化除磷效率的下降。当污泥龄恢复到 16d时 ,经过一段时间的运行 ,反硝化聚磷菌重新得到富集 ,除磷效率恢复到 90 %以上。