不同农垦地下垫面对风蚀起沙风速的影响分析

以新疆塔里木盆地垦区为例,研究不同地表粗糙度下垫面对风蚀起沙的临界摩擦速度和起沙风速的影响。根据Shao的方法计算不同下垫面起沙风速,结果表明:塔里木盆地垦区所选的小麦、棉花、红枣这3种地类2m高度临界摩擦速度(u*t)分别为棉花地0.40m/s,红枣地0.43m/s,小麦地1.85m/s;2m高度临界起沙风速(ut)分别为棉花地5.3m/s,红枣地5.7m/s,小麦地7.5m/s,小麦地较其他2种地类更具有抵抗风蚀的作用。     

霍林河下游洪泛区湿地土壤中铵态氮水平运移模拟研究

选择二百方子洪泛区湿地作为典型研究区,以NH4Cl为示踪剂,模拟研究了铵态氮在洪泛区湿地不同土层中的水平运移过程。结果表明,沼泽湿地土壤中铵态氮的运移通量随运移距离的增加呈一阶衰减指数变化;0-10cm土层中铵态氮的运移通量最小,20~60cm土层次之,10~20cm土层具有最高的铵态氮通量。各层土壤运移通量在0~6cm内最大,而后迅速下降,到18cm时3层土壤中铵态氮的运移通量相近并趋近于零。各层土壤中铵态氮的运移通量与土壤水扩散率及土壤含水量都呈一阶指数增长变化;在土壤水扩散率或土壤含水量达到一定数值前,铵态氮运移通量增长缓慢,之后则开始骤然增加。     

河西灌区覆草滴灌对酿造葡萄土壤水分运移及温度的影响

针对甘肃省河西灌区大面积栽培酿酒葡萄而水资源短缺的现状,试验采用烘干法结合GCM2010S太阳能数据采集系统,研究了地面覆草滴灌、覆膜滴灌等节水措施对干旱荒漠地区酿酒葡萄园土壤水分和土壤温度的影响.结果表明:覆盖滴灌措施明显减少了土壤水分蒸发,提高了土壤蓄水保墒作用;覆盖滴灌措施减弱了土壤的升温幅度,剧烈降温时,覆草滴...     

天津滨海盐渍土水盐运动规律研究

通过对自然状态下典型的天津滨海盐渍土进行定期调查和监测,研究天津滨海盐渍土的水盐运动规律。结果表明:土壤剖面中盐分含量随季节性变化存在明显的积盐、脱盐过程。土壤的盐化程度越高,盐分的积累与淋溶变化幅度就越大,土壤表层盐分变化频繁,变化幅度较大,底层盐分变化幅度较小。     

从儒教祭祀乐章看古代诗歌的作用

自汉至清,历代封建王朝不仅继承了原始宗教教义,而且也继承了以诗事神的古老传统。他们信奉"感天地,动鬼神,莫近乎诗"的古训,坚持"放郑近雅",以《诗经》雅颂为典范,大力创制与使用儒教祭祀乐章,旨在借助诗歌"感鬼神而通教化"的作用,为国家统治服务。在儒者看来,诗歌的主要作用是祀奉神祗,教化民众。认为祭祀诗歌是中国古代最重要的诗歌,也是最有价值的文学作品。     

柑橘黄龙病疫情运动规律与预警模型研究

为了揭示柑橘黄龙病整体疫情入侵、扩散、流行等运动规律,对柑橘木虱种群的数量消长情况进行多年多点的系统监测,同时在柑橘黄龙病果实显症期采用全境式普查方法开展疫情调查。2002-2010年连续8年的监测和普查结果表明,柑橘黄龙病疫情入侵分布呈南重北轻、东高西低的特征,其扩散趋势为自南而北逐年推进,并呈螺旋式上升。疫情长期运动一般需经历入侵上升、高位运行、受控回落周期性变化,其运动周期为10年左右,并建立时序运动模型: P=-00044N2+0056N －00698(n=9,r=09552**,r001=07977)。应用上述模型进行逐年修补,若预测下年度果园加权发病率在1%以上,则可发布预警。     

北疆土壤温度变化对滴灌棉田水盐运移规律的影响研究

以北疆常年膜下滴灌棉田为研究对象,分析棉花整个生育过程中土壤温度变化对棉田水盐运移规律的影响,并对灌溉制度进行优化调整。研究结果表明：土壤温度随着气温的升高而升高,降低而降低,气温影响作用随着土壤深度的增加而减弱,滞后时间随着深度的增加而延长;8月份之前,土壤温度自上而下呈递减分布,随着土壤温度的升高,土壤水分扩散率不断增大,土壤持水能力不断降低,造成5～60 cm处土壤含水率降低,而90～150 cm处土壤含水率增高,导致5 cm和90～150 cm处土壤盐分相对增高;8月份之后,随着土壤温度的降低,土壤温度分布发生变化,土壤水分扩散率不断减小,土壤持水能力不断增强,土壤水分蒸腾降低,渗漏减小,各层土壤含水率相对保持较高,各层土壤含盐率相对保持较低;在灌溉定额不变的条件下,在5、6月份相对减小灌水定额,7月和8月份相对减小灌水周期、增加灌水定额,8月之后相对增加灌水周期、减小灌水定额,在生育期末,通过穿插灌水,加大灌水定额,对土壤洗盐、抑盐有着明显的作用。     

沙漠地区风沙活动特征——以中国科学院风沙观测场为例

运用中国科学院风沙科学观测场的实测资料,对腾格里沙漠风沙环境特征进行初步分析,内容包括起沙风、风沙活动强度、风沙流结构和沙漠边界层的风速廓线.该地区的起沙风以6～8 m/s为主,占总起沙风的71.63%,其次为8～10 m/s,占19.24%,两者之和占90.87%;大风日数为4天;风向以W-N组风向为主;占全年的53.14%.年输沙势为36.56VU,风能属于低风能环境,单一主风向和单风态风环境.风沙流主要集中在地表的0.1 m,占总输沙量的95.46%.观测场近地层厚度大于50 m.     

Main stem movement of Atlantic salmon parr in response to high river temperature

Atlantic salmon become thermally stressed when water temperatures exceed 23 °C. To alleviate this stress, they behaviourally thermoregulate by moving to patches of cold water, often forming large aggregations. These patches are known as thermal refuges. Given the consensus that climate change will increase temperatures in Atlantic salmon catchments, thermal refuges will become increasingly important in minimising summer mortalities. While the behaviour of salmonids within thermal refuges is fairly well understood, less is known about their main stem movement in search of thermal refuges or its thermal and temporal cues. We detail the results of a PIT telemetry study to investigate the main stem movement behaviour of thermally stressed Atlantic salmon parr in a temperature‐impacted river. PIT antennas placed around two thermal refuges and at the upstream and downstream limits of their surrounding reach were used to record the movement of salmonids during a heatwave. We observed parr movement at the upstream and downstream antennas 135 min prior to the occurrence of the midpoint of aggregations in the thermal refuges, indicating that Atlantic salmon parr make reach‐scale movements in search of cool water prior to aggregating. Logistic regression showed that the number of degree hours >28 °C predicted the occurrence of main stem movement with a good degree of accuracy, indicating that this temperature represents a fundamental threshold causing Atlantic salmon parr to move towards cool water. Such data could be instrumental in allowing river managers to place limits on human activity within rivers, allowing salmon populations time to recover following heat stress events.     

Dispersal and tributary immigration by juvenile coho salmon contribute to spatial expansion during colonisation

Anadromous fishes are frequently restricted by artificial barriers to movement such as dams and culverts, so measuring dispersal helps identify sites where improved connectivity could promote range expansion and population viability. We used a combination of DNA‐based parentage analysis and mark–recapture techniques to evaluate dispersal by juvenile coho salmon (Oncorhynchus kisutch) in a population in the initial stages of colonisation following installation of fish passage structures at a previously impassable dam on the Cedar River, WA, USA. The spatial distribution of individuals within maternal families revealed that dispersal was common. Among the offspring of radio‐tagged mothers, 28% were collected outside the spawning reach and dispersed up to 6.3 km (median = 1.5 km). Most juveniles captured in a tributary (Rock Creek, where few adults spawned) had immigrated from the Cedar River and represented many different families. Juvenile dispersal therefore provided a secondary phase of spatial expansion following initial colonisation by adults. Consistent with the condition‐dependent dispersal hypothesis, juveniles that dispersed farther upstream in the tributary were larger than fish collected near the tributary mouth. Overall, the results demonstrated widespread dispersal in a system with low coho salmon densities, and this might increase the rate of population growth if it reduces the effects of local density dependence. By implication, juveniles can take advantage of rearing habitats reconnected through barrier removal, even when such areas are located several kilometres from adult breeding grounds.