基于环境DNA宏条形码的青岚湖自然保护区鱼类组成及分布特征

为探究在不同引物、不同参考数据库下环境DNA技术检测结果的差异,于2021年4月,采用环境DNA宏条形码技术分析了青岚湖鱼类多样性。选取16S rRNA及Cytb 2种引物,NCBI及本地数据库2种数据库,分别进行比对注释。结果表明:在青岚湖29个采样点中,共检测到7目15科43属64种鱼类,其中在16S-NCBI情形下获得4目9科19属20种鱼类,在16S-本地数据库情形下获得6目13科27属38种鱼类,在Cytb-NCBI情形下获得4目6科16属19种鱼类,在Cytb-本地数据库情形下获得2目5科15属20种鱼类。在青岚湖29个采样点中,鱼类更多地分布于湖面宽阔的中间地带(如S31附近),且南部较北部更少,鱼种的分布呈现一定的空间相似性。就研究区域而言,选择16S rRNA引物及本地数据库可以获得更全面的鱼类物种。通过与青岚湖鱼类历史数据比对发现,环境DNA技术在研究区域具有较强的适用性,如能选择适当的引物和本地数据库,可以更全面地反映研究区域的物种组成情况。     

植物群落蒸散耗水量研究进展

本文主要介绍了植物群落蒸散量的研究方法及影响因素，并根据作者所处地区的特点，对内蒙古典型草原的蒸散研究进展进行了综述。     

氧弹燃烧-BaSO4重量法用于柴油中硫成分分析标准物质的定值

研究并确定了氧弹燃烧—BaSO4重量法测定柴油中硫含量的燃烧条件、吸收液种类、沉淀溶液pH、沉淀和转移条件等实验条件。在实验确定的优化条件下，该方法的定值结果与其他方法吻合良好。对定值结果进行了全面的不确定度评定，对于硫含量0．515％和1．027％的柴油中标准物质，获得的展伸不确定度分别为1.3％、1.4％(K=2)。利用该方法成功地实现了较低含硫量样品的定值。     

同化箱装置在温带落叶阔叶林CO2交换研究中的应用

本文探讨了森林生态系统中植物－－土壤－－大气ＣＯ２气体交换测定装置。本装置在草原生态系统植物群落光合作用测定装置基础上改进而来，适用于森林地带无交流电源，效能运输不便的地区，利用便携式ＣＯ２红外线分析仪和粉尘采样器替代气泵，具有经济，轻便，实用等特点。     

介绍一种新编制的环境试验用相对湿度查算表

介绍了一种新的环境试验用相对湿度查算表及其编制目的、编制方法,该查算表用较小的篇幅实现更宽的温度和相对湿度的查算范围(与GB6999鄄86《环境试验用相对湿度查算表》比较)。该查算表中对风速与大气压的修正方法有与其他查算表不同的特点,它对提高相对湿度测量(查算)精度有一定的作用。     

论我国降水丰度和适度

本文以全球陆地年平均降水量、农田蒸散量和作物需水量等指标为尺度,衡量我国降水量的丰度,从降水的时空分布,及其稳定性等方面评价我国降水量的适度,从经济现状分析我国降水条件对国土开发的影响程度,并和欧美各国对比,说明我国降水条件的优劣程度,指出我国的降水条件和降水量不是黄万里先生所说的那样优越和丰富。     

Climatic Controls on Watershed Reference Evapotranspiration Varied during 1961–2012 in Southern China

Reference evapotranspiration (ET_o) is an important hydrometeorological term widely used in understanding and projecting the hydrological effects of future climate and land use change. We conducted a case study in the Qinhuai River Basin that is dominated by a humid subtropical climate and mixed land uses in southern China. Long‐term (1961–2012) meteorological data were used to estimate ET_o by the FAO‐56 Penman–Monteith model. The individual contribution from each meteorological variable to the trend of ET_o was quantified. We found basin‐wide annual ET_o decreased significantly (p < 0.05) by 3.82 mm/yr during 1961–1987, due to decreased wind speed, solar radiation, vapor pressure deficit (VPD), and increased relative humidity (RH). However, due to the increased VPD and decreased RH, the ET_o increased significantly (p < 0.05) in spring, autumn, and annually at a rate of 2.55, 0.56, and 3.16 mm/yr during 1988–2012, respectively. The aerodynamic term was a dominant factor controlling ET_o variation in both two periods. We concluded the key climatic controls on ET_o have shifted as a result of global climate change during 1961–2012. The atmospheric demand, instead of air temperature alone, was a major control on ET_o. Models for accurately predicting ET_o and hydrological change under a changing climate must include VPD in the study region. The shifts of climatic control on the hydrological cycles should be considered in future water resource management in humid regions.     

官厅水库上游河流营养物参照状态的制定

采用参照河流百分位法、一般河流百分位法和多元线性回归法,制定了官厅水库上游流域河流雨季和旱季的营养物参照状态,探讨季风气候对河流营养物参照状态的季节性影响,并识别影响官厅水库上游河流营养物浓度的主要人类活动.结果表明：参照河流点和一般河流点总氮（TN）和总磷（TP）浓度在雨季和旱季均表现出明显的季节性差异.参照河流百分位法、一般河流百分位法和多元线性回归法制定的营养物参照状态在雨季和旱季也均存在季节性差异,取3种方法的平均值作为官厅水库上游河流的营养物参照状态：TN在雨季和旱季参照状态的建议值分别为1.580和1.672mg/L; TP在雨季和旱季参照状态的建议值分别为0.075和0.055mg/L.影响河流TN浓度的人类活动按贡献大小依次为：畜禽养殖污染负荷强度、耕地（坡度0~8°）比例和城市用地比例.影响河流TP浓度的人类活动按贡献大小依次为：耕地（坡度0~8°）比例和畜禽养殖污染负荷强度.     

ESTIMATION OF REGIONAL EVAPOTRANSPIRATION FROM ARID AND SEMI-ARID SURFACES1

ABSTRACT: Evapotranspiration (ET) from oasis and Gobi surfaces in the Heihe River region of China was estimated by Kotoda (1986) and Advection-Aridity (Brutsaert and Stricker, 1979) models. The ET estimates were compared with eddy-correlation ET estimates. The ET estimated by both models are in good agreement with ET obtained by means of eddy-correlation method for the oasis surface while underestimating ET as compared to the eddy-correlation method. For the Gobi surface, the models yielded obviously overestimates of evapotranspiration. In order to estimate evapotranspiration from arid surfaces, the Kotoda model was modified by introducing the surface moisture availability parameter a from Barton (1979). The modified Kotoda model yielded ET estimates that were very close to that from the eddy-correlation method for the Gobi surface. The modified Kotoda model was used to estimate evapotranspiration from the Heihe River watershed, an area with complicated topography and land use, and the results compared with those from a water balance method. A sensitivity analysis of the modified model was performed. The results show that the modified Kotoda model can reflect the relationship between the actual evapotranspiration and the main controlling factors on it for both wet and arid surfaces reasonably. From this study, it can be concluded that the modified Kotoda model is applicable fro the estimation of regional evapotranspiration from areas with complicated topography and land use.