青海高原春小麦籽粒蛋白质积累规律研究

分析了阿勃,青春５３３,青农４６９、青农４５２等四个春小麦品种（品系）在青海西宁地区籽粒蛋白质相对含量的变化规律和蛋白质绝对含量的积累进程,结果表明,从开花至成熟,籽粒蛋白质相对含量的变化呈“Ｕ”型曲线,并以花后籽粒发育初期含量最花,花后３１天左右是该地区春小麦籽粒中蛋白质相对含量最低的时期。不同品种在花后不同时期蛋白质相对含量各不相同;籽粒蛋白质绝对含量的积累过程呈“Ｓ”形曲线,可用概率转换方程     

Holocene lake deposits of Bosten Lake, southern Xinjiang, China

A 9.25-m-long sediment core from Bosten Lake,Xinjiang, provides detailed information about changes in the water budget and biological acticity over the last 8400 cal-endar years. The chronology is constructed from six AMS radiocarbon dates on the terrestrial plant remains. Based onanalyses of TOC, CO3, detrital compounds and biogenic SiO2,lake level fluctuations and periods of remarkably-negative water budget appeared at 8.4-8.2 cal ka, 7.38-7.25 cal ka,5.7-5.5 cal ka, 3.7-3.4 cal ka and 3.3-2.9 cal ka, respec-tively. As they are in-phase with low lake levels at Sumxl Co and Bangong Co in western Tibet Plateau and with paleo-lakes in Inner Mongolia, a climate-induced change to some-what drier and warmer conditions is inferred. A further drop in lake level after 1320 AD of about 200 yr duration may heattributed to a negative water balance prior to the main phase of the Little Ice Age. Deep and stable lake phases of 1500 yr and 1800 yr duration at 7.2-5.7 cal ka and 5.5-3.7cal ka coincide with maximum moisture during the Holocene Megathermai in China. The long term trend towards aridity since about 4.3 cal ka can dearly be recognised. The reduced water budget of Bosten Lake from 640-1200 AD may be attributed to local effects.     

Temperature variations on the Tibetan Plateau over the last two millennia

The paleoclimate data recovered from ice cores,tree rings and lake sediments indicate regional features of cfimatic change on the Tibeta n Plateau (TP) during the last 2000 years. The composite temperature reconstructions in-dicate that several main climatic episodes, such as the “LittleIce Age“ between 1400 and 1900, the “Medieval Warm Pe-riod“ in 1150-1400, a less warm period in 800-1100, and an earlier cold period between the 3rd and 5th centuries,occurred in the TP. In addition, temperature varied from region to region. The period from AD 800 to 1100, which waswarm in northeastern TP, was contemporaneous with cool-ing in the western and southern TP. The southern TP ex-perienced warming between 1150 and 1400. For western TP,the δ^18O records of the Guliya ice core indicate that the pe-Hod 1250-1500 witnessed a clear warming. Large-scaletrends in the temperature history from northeastern TP aremore similar to those in eastern China than are the trendsfrom the Guliya ice cap far to the west and southern TP. The most prominent similarities between the temperature varia-tions of the TP and eastern China are such cold phases as 1100-1150, 1500-1550, 1650-1700 and 1800-1850, andthe latter three cold events match with three widespreadg lacial advances which occurred on the TP during the Little Ice A2e.     

我国南方的生态特点及其保护措施

经济的飞速发展，带来的副作用是生态环境的破坏。章以湖北省为研究对象，指出我国南方生态环境的特点和由于追求经济发展而日益突出的四个主要生态问题，并且针对这些问题提出保护措施。     

湖泊沉积研究中一种定量估算陆源有机碳的方法

湖泊沉积研究中常把总有机质含量(TOM)或总有机碳含量(TOC)作为判识湖泊环境的一个重要指标.事实上,湖泊沉积物中的有机碳来源广泛,简单地可分出内源和陆源两部分.     

湖泊原生碳酸盐化学沉积模型及其应用

对湖泊原生碳酸盐化学沉积体系的模型化作了初步的尝试，并把经与对胜利油区早第三纪的古老营湖的研究相结合，定量化地探讨了古东营湖中的由气候的旋回性变化所控制的富碳酸盐／富碎屑物的韵律沉积现象。     

青藏高原冬季积雪异常对东、南亚夏季风影响的初步数值模拟研究

利用一个耦合了简化的简单生物圈模式的大气环流谱模式（ＳＳｉＢ－ＧＣＭ），初步探讨了青藏高原冬季积雪异常对东、南亚夏季风环流和降水的影响及其机理。结果表明，高原地区冬季积雪增加将使随后的夏季东、南亚季风明显减弱，主要表现为东、南亚季风区降水减少，索马里急流、印度季风槽和印度西南气流减弱。另外，还提出欧亚大陆雪盖与整个高原雪盖和高原东部雪盖对东、南亚夏季风影响的敏感性问题。与欧亚大陆雪盖相比，高原雪盖是影响东、南亚季风的更敏感区，冬季高原以外雪盖增加，有可能使亚洲季风增强；当高原东部雪盖增加时，高原以东地区及印支半岛降水减少，印度东部、南部和孟加拉湾西北部降水反而增加     

应用主成份分析法评判湖泊营养类别

采用主成份分析法对１８个湖泊的是总磷、总氮、耗氧量、生物量、透明度进行了分析，并对湖泊营养类别进行了评判。分析结果表明，湖泊营养状态是总磷、总氮，耗氧量、生物量、透明度综合作用的结果，其中总磷的作用最大，其次是总氮。     

Quinghai-Tibet Railway and Environment Protection

TheQinghai TibetPlateauhasthehonorof“theroofoftheworld”.Comparingitwiththe NorthPoleandSouthPole,thegeoprapherscallithethirdpoleoftheglobe.Itnotonlycanbe calledthefirstintheworldintermsofthealtitude andarea,butalsotheyoungestplateauontheearth.TheQinghai TibetPlateauhastheunique naturallandscape,specialstructureofearthcrustandearthmantle,complicatedbiota,diversified ecosystemandabundantnaturalresources.Theshapingup,evolvingandexistingoftheplateau broughtwideanddeepeffectonitself,andalsoon…     

对我国优秀女足赛前高原训练疲劳判定及恢复措施状况的调查

疲劳是运动训练的必然结果,轻则影响运动水平的发挥,重则严重影响机体的健康水平。赛前在高原环境下训练的特殊时期,准确地判断高原训练的疲劳程度,及时采取恢复措施具有重大意义。以我国优秀女足为研究对象,对其赛前高原训练疲劳判定及恢复措施状况进行调查,以期为今后的训练实践提供参考。