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。     

针刺疗法治疗血管性痴呆的临床研究进展

血管性痴呆（vascular dementia,VD）是由各种脑血管病引起脑组织损害而产生的痴呆,它是仅次于阿尔茨海默病的常见痴呆类型。针刺疗法对血管性痴呆的认知功能及社会活动功能康复有积极作用,临床应用广泛。本文综述中文数据库中近五年相关针刺疗法治疗血管性痴呆临床文献报道,科学评价针刺疗法的优势和不足,以期为临床治疗血管性痴呆提供参考。     

梵净山国家级自然保护区固氮维管束植物资源研究

应用个体生态学和种群生态学等生物多样性研究的原理与方法,对贵州省梵净山区域内的固氮维管束植物进行点与面相结合的系统调查,并对其生态分布特征进行研究。结果表明,梵净山固氮植物种类丰富多样,有固氮维管束植物10科44属104种(包括种下分类群),其中蕨类植物门1科1属4种,裸子植物门2科2属3种,被子植物门7科41属97种。其中木本植物73种,草本植物31种(包括水生植物4种)。梵净山低山林带、中山林带和高山林带等不同海拔高度分布着不同的固氮植物。     

内蒙古赛罕乌拉国家级自然保护区维管束植物区系研究

本研究通过对赛罕乌拉自然保护区植物进行调查,并对该区植物地理区系进行研究,在植物调查和标本采集的基础上,从科、属、种3个层次对植物区系的组成特点,地理分布规律等进行分析.结果表明:该植物区系物种多样性丰富,保护区内共有维管植物792种(包括8亚种、48变种、2变型),隶属于348属,91科,其中被子植物占主导地位.优势科明显,中生植物种类丰富.生活型以多年生草本植物占优势.分布区类型多样,地理成分复杂.温带成分明显,并与其他成分有较广泛的联系,过渡性突出.     

人和哺乳动物支气管动脉与肺动脉吻合现象研究进展

对人和哺乳动物支气管动脉与肺动脉吻合问题的研究进行了概述.肺动脉与支气管动脉吻合的意义在于支气管动脉的高氧血液可以进入肺动脉代偿供应肺泡组织,肺动脉的营养血液也可以进入支气管动脉代偿供应肺间质.肺动脉与支气管动脉之间血管吻合常可以发生在胸膜面、支气管壁、终末细支气管或呼吸性细支气管等部位,也可以在毛细血管上发生支气管动脉与肺动脉的吻合.根据血管吻合的长度和口径,将其分为长吻合型和短吻合型,按照血管吻合的方式分为端-端吻合和端-侧吻合.在某些病理情况下,肺动脉与支气管动脉之间的吻合支还会通过管径扩张,增加血流量来供应局部的病变组织,因此有利于防御不利因素对机体造成的损伤,为机体实施正常的呼吸功能提供保障.     

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.     

慈溪市水生维管束植物的区系特点及保护利用

2007~2009年对慈溪市水生维管束植物区系特点进行了调查研究。结果表明：慈溪有水生维管束植物131种,隶属于88属41科。将88个属归纳为11个分布区类型,世界分布类型比例最高,其次依次为热带分布属、温带分布属。此外,对保护与合理利用慈溪市水生维管束植物资源提出了必要性及具体措施。     

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.     

Accumulation and Mobility of Salts in Soil as Influenced by Primary Biomethanated Spentwash

A soil column laboratory experiment was carried out at the central campus, Mahatma Phule Agricultural University, Rahuri, India during 2008–2009 to study the accumulation and mobility of salts in Typic Haplusterts as influenced by primary biomethanated spentwash (PBSW). The PBSW was applied in three different levels (0.5, 1.0, and 2.5 cm) and then tap water with low salinity and low sodium hazard (C₁S₁ class) was used to carry out leaching in four different levels of water at the pore volume of soil (WPVS) (0.5, 1.0, 1.5, and 2.0). The electrical conductivity (EC) in the soil increased significantly with increasing levels of PBSW and decreased with increasing levels of WPVS in surface (0–15 cm deep) and subsurface (15–30 cm deep) soil layers. The exchangeable calcium (Ca²⁺), magnesium (Mg²⁺), and potassium (K⁺) increased, whereas exchangeable sodium (Na⁺) decreased with increasing levels of PBSW and WPVS in surface and subsurface layers of soil. The organic carbon content increased with increasing levels of PBSW and decreased with increasing levels of WPVS in both the soil layers. The cation exchange capacity (CEC) increased with increasing levels of PBSW and WPVS in both the soil layers. The exchangeable sodium percentage (ESP) decreased with increasing levels of PBSW and WPVS over the initial values of soil in both the layers. The pH of saturated paste (pHs) was reduced and electrical conductivity of extract (ECe) was increased with increasing levels of PBSW and WPVS in both the layers. The Na⁺ content of saturation paste extract increased significantly with increasing levels of PBSW and WPVS in both the soil layers.