玉米自交系氮效率基因型差异的比较研究

采用溶液培养的方法。选用经田间，土壤试验对N反应有典型差异的玉米自交系478，H21，Wu312,Zong31,Baici，在4个供氮水平下（0.04,0.4,2和4nmol/L)，研究了不同基因型玉米苗期氮素吸收，利用的差异及其原因，结果表明：极低N胁迫条件下（０.04mmol/L),总干重的基因型差异是由根系，地上部的共同作用的结果，高N下，总干重是由地上部的差异所决定的（表1），极低供N条件下，4578的总干重最大，且有较高的氮效率，Wu312,Zong31相对较低，478相对较高的氮效率主要来源于吸收效率的差异。该基因型在低N下总吸氮量最高，H21居中，Baici,Zong31相对较低，478相对较高的氮效率主要来源于吸收效率的差异。该基因型在低N下总吸氮量最高，H21居中，Baici,Zong31,Wu312相对较低（图1），吸收效率的差异主要是由于根系全N量的不同所致（图3），而根系全N量的差异主要是由于根系大小不同（表1），在极低氮水平下，不同基因型玉米根系全氮量的变幅比地上部高出28.1%，高N下（4mmol/L)，全N量的变幅比地上部高出15.4%(图2，图3），在0.04mmol/L下，478与Wu312,Zong31的利用效率不存在显著差异（表2）。     

环境光强对糯玉米籽粒主要品质成分的影响

作物生长发育期间的环境光强是影响作物品质的主要因素之一。为了解不同环境光强对鲜食型糯玉米籽粒品质的影响,以香白糯(Xiangbainuo)为材料,采用人工遮光的方法模拟不同的环境光强,在糯玉米籽粒灌浆期间测定其籽粒粗蛋白、淀粉、脂肪、水分含量的变化规律和收获时籽粒的氨基酸总量及氨基酸各组分含量。结果表明,遮光没有明显改变糯玉米灌浆期间籽粒中主要品质成分的变化趋势,但对主要品质成分所占质量分数的影响很大。弱光(40%全光照)与自然光照(100%全光照)相比,糯玉米授粉后30d时,其籽粒中粗蛋白和淀粉的质量分数分别增加1.56和3.5个百分点,脂肪减少了1.5个百分点;自然光照条件下糯玉米籽粒的含水量每天以1.31%的速率减少,其脱水速率高于弱光下糯玉米籽粒脱水速率0.17个百分点。收获时,40%全光照条件下糯玉米籽粒中粗蛋白质量分数、氨基酸总量和赖氨酸质量分数高于自然光照和80%全光照时的质量分数,而糯玉米籽粒的百粒干质量显著降低。     

土地利用变化对城郊农业区生态效益的影响——以四川省南充市高坪区为例

借鉴生态效益综合评价的有关理论和数学模型,以四川省南充市高坪区为例,选取生物多样性指数、植被覆盖指数、水土保持效益指数、土壤改良指数、涵养水源指数、拦截径流指数和湿度指数7个指标作为评价因子,建立生态效益评价体系,对该区域1996和2005年2个时期综合生态效益进行评估和比较.结果表明,该区域综合生态效益值分别为7.85和7.95,2005年比1996年略为升高;基于GIS的图层叠置、分割等分析功能,就区域土地利用变化对其内部生态效益造成的变化进行了分析,该区域可被划分为生态效益显著增强区、增强区、保持区、减弱区和显著减弱区5个等级.     

江西赣州西坑银矿地质特征

西坑银矿为20世纪80年代在检查验证化探异常时发现的,后经详查评价确定为中低温热液充填交代形成的硅化破碎蚀变岩型银矿床,其银资源储量达中型规模。因其矿体硫化物少,蚀变弱,肉眼难于辨别,但银品位富等特点而倍受找矿界的关注。本文介绍了矿床的发现过程,成矿地质特征和找矿标志。     

福建省“尤德地体”的成矿特征和找矿远景

“尤德地体”位于闽中裂谷带南端 ,与紫金山金矿处于同一成矿带。在“尤德地体”中 ,目前已发现元古界麻源群变质岩和侏罗系长林组、南园组 ,火山岩中均存在韧性剪切带型矿床和热液交代充填矿床。区域构造、地层含矿性、物化探重砂异常等表明其找矿前景很好。找矿工作重点应紧扣层控矿床 ,大断裂带 ,斑岩型金矿和红土型金矿     

环太平洋陆缘成矿带区段对比及中国东南找矿思路

环太平洋陆缘弧系按其演化历史不同可分为挤压型、盆岭型和裂解型三种。不同类型弧系的不同区段金属成矿分带互有差别,甚至相反,其主要原因在于:1.构造演化历史不同,板块俯冲的势态不同;2.火山岩系列和火山岩组合,花岗岩成因类型及其发育程度和分布特征不同;3.地壳厚度和结构、基底杂岩的性质、基底构造特点和基底所赋存时代较老的金属矿化不同。在对比环太平洋成矿带各区段金属成矿特征的基础上,提出中国东南Au、Cu找矿的战略目标应在浙中闽西,江南古陆南缘和长江中下游;矽卡岩型Pb-Zn-Ag矿在浙闽沿海火山岩区有一定远景;裂谷式火山构造洼地可成为浅成热液贵金属和有色金属矿化的远景地段。     

江南复合混杂岩带基本特征

江南复合混杂岩带是扬子板块与华夏板块长期活动所致，构造极为复杂。江南大地构造重新划分为三个1级构造单元：扬子板块、江南复合混杂岩带及华夏板块。江南复合混杂岩带又可进一步划分II级构造单元5个(宜丰一景德镇一歙县构造混杂岩亚带、万年构造单元、赣东北蛇绿混杂岩亚带、怀玉构造单元及丰城一鹰潭一龙游构造混杂岩亚带)；各构造单元之间以构造(蛇绿)混杂岩亚带或韧性剪切带相拼接。沿宜丰一景德镇一歙县发育一条构造花岗岩浆带；而沿赣东北断裂带形成了该区重要的燕山期构造岩浆带及Cu、Au、Ag、Pb、zn及金刚石等成矿带。     

平原河网地区地表水环境保护功能区划分的研究

从地表水环境保护功能区划分工作的实践出发 ,针对复杂的水文、水质条件 ,探讨平原河网地区地表水环境保护功能区划分的工作方法和实现区划目标的对策措施。     

Palaeorunoff estimations achieved from palaeoclimatic information for the southwest part of the North China Plain: an attempt to apply a climatological approach to palaeohydrology

Palaeoclimatic scenario projecting annual temperature and annual precipitation is firstly formalized with data available and speculations for the southwest part of the North China Plain (35- 37°N, 115-119°E) during the last 25000 years. Then, with three regression equations relating annual runoff to annual precipitation and derived with data of modern hydrological and meteorological records, values of annual runoff are calculated in terms of the corresponding values of annual precipitation from this palaeoclimatic scenario for this region during this temporal interval. These results indicate that runoff is the most during 8000-3000a B.P. and the least during 25000-12000 a B. P.; runoff occurring during 12000-8000 a B.P. and during 3000-0 a B.P. is less than the one occurring during 8000-3000 a B.P. and more than the one occurring during 25000-12000 a B. P.; and the runoff occurring during 25000-12000 a B. P., 12000-8000 a B. P., and 3000-0 a B.P. is respectively 43, 46 and 66 percent of the one occurring during 8000-3000 a B.P. Values of bankfull discharge for palaeochannels of the Yellow River flowing in this region during the same interval are calculated from available estimates of slope of stream-bed of these palaeochannels with a regression equation relating bankfull discharge to slope of stream-bed and ratios of bankfull-discharge are further calculated from these values for different groups of palaeochannel formed during different time spans embraced in this interval. To conduct a cross-check, these values and ratios of bankfull-discharge are compared to the corresponding values and ratios of runoff occurring during roughly the same time spans. The same direction and similar relative magnitude of changes of the surface water occurring in this region during the last 25000 years are indicated by these comparisons.     

High-risk behaviors while driving: A population-based study from Iran

Objective: Traffic injuries are becoming one of the most important challenges of public health systems. Because these injuries are mostly preventable, the aim of this study is to evaluate the four main high-risk behaviors while driving.

Methods: This cross-sectional study was conducted on a random sample from the population of Mashhad, Iran, in 2014. A checklist and a previously validated questionnaire for the transtheoretical stages of change model (TTM) were used for data collection. Statistical analyses were performed using SPSS 11.5 software with P <.05 statistically significant.

Results: Totally 431 individuals were included with a mean age of 30 ± 11.3 years. Forty-three percent (183) were male. The TTM model revealed that participants were mostly in pre-actional phases regarding not using a cell phone while driving (80%), fastening the driver's seat belt (66%), front seat belt (68%), and rear seat belt (85%) The penalty was a protective factor only for using cellphone (odd ratio [OR] = 0.82, 95% confidence interval [CI], 0.68–0.98). Lower education (OR = 0.12, 95% CI, 0.01–0.94) and male gender (OR = 0.35, 95% CI, 0.14–0.83) were indicative of lower rates of fastening the front and rear seat belts.

Conclusion: The stages of change model among study participants is a proper reflection of the effectiveness of the current policies. More serious actions regarding these high-risk behaviors should be considered in legislation.