青藏高原东北部3种野豌豆植物学特性及资源储量

采用野外定点法、最小样方法和统计学方法对生长于青藏高原东北部的3种野豌豆属植物的植物学特性、生态环境、群落数量特征及资源储量进行研究。结果显示,救荒野豌豆、山野豌豆和三齿萼野豌豆的植物学特性、生态环境和群落数量特征具有一定差异,3种野豌豆在青海省的资源总储量分别为0.46×10~6、0.23×10~6、0.27×10~6 kg,表明3种野豌豆属植物的资源总量在青海省并不高,应对其进行有效的引种驯化,实现人工繁育和增加资源储量,这既可保护青海省甚至青藏高原的生态环境,也可对其资源进行有效地保护和合理开发利用。     

祁连山南麓高寒灌丛GPP变化特征及对生长季积温的响应

全球气候变化背景下气温逐渐升高,将会对陆地生态系统碳循环产生重要影响。研究利用2003?2016年的涡度相关系统观测资料,研究了祁连山南麓高寒灌丛生长季(5月?9月)总初级生产力(gross primary productivity,GPP)在不同时间尺度上对生长季有效积温(growing season degree days,GDD)的响应,对于研究气候变暖对高寒生态系统碳循环的影响有重要意义。结果表明:高寒灌丛生态系统在生长季的月GPP、GDD都表现为先增大后减小的单峰变化趋势,都在7月或8月达到峰值,在5月达到最小值。在整个生长季尺度上,GPP与GDD具有较高变异性,但整体上表现为逐渐增加的趋势(P<0.05)。2003?2016年整个生长季GPP与GDD的均值分别为507.11 g·m^?2和975.93℃。在月尺度和生长季尺度上,GPP与GDD都呈显著正相关关系(P<0.05)。但是,通过比较生长季每个月GPP与GDD的关系发现,5、9月的GPP与GDD没有显著相关性(P>0.05),而在7月相关性最为显著(P<0.01)。整体上看,高寒灌丛生态系统植被的总初级生产力与热量条件表现为正相关关系,由此说明在全球气候变暖的背景下,青藏高原高寒灌丛生态系统植被的光合生产能力将会提高。     

青藏铁路格唐段高海拔地区植被恢复研究——I高寒草原植被现状与恢复基本途径探讨

青藏铁路的修建加强了西藏与内地的联系,对其经济发展、社会稳定具有重要的意义。但在修建过程中不可避免地对沿线的局部植被生态系统造成不同程度影响和破坏,如何尽快恢复植被生态系统至关重要。对青藏铁路青海境内的高海拔的气候条件及现有植被状况作了统计调查,提出尊重科学,因地制宜的指导原则,恢复与重建的工作一起抓:一方面要增强环保意识,加强管理,综合治理;另一方面通过原有草皮回植,科学管理以及异地繁殖当地草种等途径尽快提高地表覆盖度和植物种群多样性,以期达到最佳的生态效应。     

青藏高原低云量的年际变化及其稳定性

利用青藏高原80个测站1961-2000年1～12月低云量资料,分析了青藏高原低云量的年际变化规律.结果表明:青藏高原的低云量从东南向西北减少,云量的稳定性夏季高于冬季,南部高于北部.江河上游区域、藏东谷地、川西高原、甘南高原和祁连山区是青藏高原低云量多,且比较稳定的地区;青藏高原西部低云量月变化振幅大,尤以西南部为最,夏季云量最多;高原东南部江河上游区和藏东谷地3～9月低云量多,且起伏变化小,6月和9月出现峰值;高原东南部低云量稳定性较好;低云量的年际变化总体呈下降趋势, 江河上游区和高原东南部的低云量变化缓慢,高原西北部有显著上升趋势;变化趋势在季节上表现为冬、春、夏、秋西北上升西南下降,春、秋季中东部持平,夏、冬略降.     

高寒地区多年生禾草混播草地种间竞争效应分析

从高寒地区3组分禾草混播草地群落的种问竞争机制出发,建立了适合高寒地区3组分禾草混播草地群落种间竞争机制的Lotka—Volterra竞争效应模型,并对该模型所描述的竞争进行了计算机模拟试验。模拟结果表明,试验所选的3种高寒地区3组分禾草混播草群的种间相容性分为两种类型,即不稳定的群落：多叶老芒麦 无芒雀麦 垂穗披碱草和垂穗披碱草 多叶老芒麦 扁穗冰草,其竞争结局是：群落内多叶老芒麦和垂穗披碱草二者共同表现为优势种群,无芒雀麦或扁穗冰草与优势植物的竞争结果将导致其从群落中消失,多叶老芒麦和垂穗披碱草种群将能稳定共存;不稳定-稳定过渡群落：无芒雀麦 多叶老芒麦 扁穗冰草,在没有多叶老芒麦种群的时候,无芒雀麦和扁穗冰草种群可以共存,但是如果多叶老芒麦种群加入无芒雀麦和扁穗冰草所占的区域,它将导致无芒雀麦和扁穗冰草种群趋于灭绝。通过对3个混播试验组计算机模拟竞争模型的竞争效应分析,其结果与方法对科学建植同类型的多年生混播人工草地具有一定的指导意义。     

高原鼠兔干扰对高寒草地碳循环的影响研究进展

高原鼠兔(Ochotona curzoniae)是青藏高原的关键种,其干扰导致高寒草地下垫面形成植被和裸地斑块镶嵌共存的景观格局,加剧了植被生产力和土壤有机碳的空间异质性分布,改变了生态系统碳交换过程。为了增进对高原鼠兔干扰在高寒草地碳循环中作用的认识,本文综述了高原鼠兔干扰对高寒草地生态系统有机碳储量和碳交换的作用过程和影响机制。总结出采食、堆土和挖掘是高原鼠兔直接影响高寒草地的主要方式,同时堆土和挖掘也是高寒草地秃斑化的潜在诱因,秃斑侵蚀、扩张以及本身的热岛效应也会对高寒草地生态系统功能产生影响。尽管高原鼠兔挖掘活动促进了土壤养分循环有利于生态系统有机碳的累积,但是堆土以及与高原鼠兔干扰相关联的秃斑化也会引起潜在的有机碳流失。高原鼠兔挖掘洞穴打破了生态系统原有的碳交换平衡,加速了CO₂通过鼠兔洞道扩散排出,而堆土和秃斑化后植被物种组成改变,地上、地下生物量分配格局的变化以及土壤暖干化是生态系统碳交换发生改变的主要原因。基于现有研究进展,未来的研究需要重点关注大尺度高原鼠兔干扰对生态系统有机碳储量的量化评估,以及耦合生态系统碳储量和碳收支的综合研究。     

Methane emissions from different vegetation zones in a Qinghai-Tibetan Plateau wetland

We measured methane (CH₄) emissions in the Luanhaizi wetland, a typical alpine wetland on the Qinghai-Tibetan Plateau, China, during the plant growth season (early July to mid-September) in 2002. Our aim was to quantify the spatial and temporal variation of CH₄ flux and to elucidate key factors in this variation. Static chamber measurements of CH₄ flux were made in four vegetation zones along a gradient of water depth. There were three emergent-plant zones (Hippuris-dominated; Scirpus-dominated; and Carex-dominated) and one submerged-plant zone (Potamogeton-dominated). The smallest CH₄ flux (seasonal mean=33.1 mg CH₄ m⁻² d⁻¹) was observed in the Potamogeton-dominated zone, which occupied about 74% of the total area of the wetland. The greatest CH₄ flux (seasonal mean=214 mg CH₄ m⁻² d⁻¹) was observed in the Hippuris-dominated zone, in the second-deepest water area. CH₄ flux from three zones (excluding the Carex-dominated zone) showed a marked diurnal change and decreased dramatically under dark conditions. Light intensity had a major influence on the temporal variation in CH₄ flux, at least in three of the zones. Methane fluxes from all zones increased during the growing season with increasing aboveground biomass. CH₄ flux from the Scirpus-dominated zone was significantly lower than in the other emergent-plant zones despite the large biomass, because the root and rhizome intake ports for CH₄ transport in the dominant species were distributed in shallower and more oxidative soil than occupied in the other zones. Spatial and temporal variation in CH₄ flux from the alpine wetland was determined by the vegetation zone. Among the dominant species in each zone, there were variations in the density and biomass of shoots, gas-transport system, and root-rhizome architecture. The CH₄ flux from a typical alpine wetland on the Qinghai-Tibetan Plateau was as high as those of other boreal and alpine wetlands.     

Change in soil microbial biomass and regulating factors in an alpine meadow site on the Qinghai-Tibetan Plateau

ABSTRACT

The change in soil microbial biomass (SMB) content and its direct links to soil organic matter (SOM) and environmental factors are not well understood for high-elevation regions. Therefore, this research investigated the temporal variation of SMB and its relationship with SOM and environmental factors in an alpine meadow site on the Qinghai-Tibetan Plateau. The soil organic carbon (SOC) and total nitrogen (TN) contents in alpine meadows showed monthly and seasonal variations and were higher in colder months, and the soil C/N ratio was higher in winter and in autumn than it was in the other seasons (P < 0.05). In addition, the changes in the SMB C and SMB N contents were notable at monthly and seasonal scales, whereas the SMB C and SMB N contents were higher in the winter and spring than they were in the other seasons (P < 0.05); the ratio of SMB C/SOC was higher in spring than it was in the other seasons; the ratio of the SMB N/TN content was higher in cold or cool months than it was in the other months; and the ratio of the SMB C/SMB N was highest in August (P < 0.05). Moreover, the SMB C and SMB N contents were significantly positively correlated to the SOC and TN contents (P < 0.01), and the SMB content was also significantly positively correlated to soil water content and air temperature (P < 0.05), or to soil bulk density and soil pH (P < 0.05). The results suggested that the change in the SMB in the alpine meadows was highly regulated by the SOC and TN and by monthly and seasonal changes in the soil bulk density, the soil pH, soil moisture, and air temperatures.     

藏族的草原游牧文化(Ⅱ)——藏区的草原和生产文化

青藏高原是全球海拔最高的自然地域单元,由于地势高耸、气候寒冷而被称之为“地球第三极”.它是南亚、东南亚众水发源地,哺育了中华黄河、长江流域文明和印度河流域文明.至当代,它仍然对中华民族乃至南亚、东南亚人民的生存和发展有着决定性影响.草原分为高寒草原、高寒草甸、荒漠草原、高寒灌丛等.在各类草地类型中,以高寒草原与草甸草地...     

青藏高原云杉针叶水提物抑菌作用研究

研究青藏高原若尔盖云杉针叶水提物(NAEPA)的抗菌作用并初步分析其活性成分。NAEPA抗菌活性显著,对供试6种常见的革兰氏阳性和革兰氏阴性病原菌都有较强的抑菌作用和杀菌作用,最小抑菌浓度(MIC)和最小杀菌浓度(MBC)分别为3.8～15 mg/mL和7.5～30 mg/mL。抑菌物质在酸性环境中活性最强,对中性和碱性环境敏感;对121℃高温比较稳定。GC-MS分析表明,有机酸是NAEPA的主要成分;苯甲酸、间羟基苯甲酸、邻苯二酚、角鲨烯和桃金娘烯醇是主要抑菌物质。NAEPA中还含有抗氧化、降血脂以及抗血栓成分。NAEPA具有有效的抑菌物质和各种保健成分,是一种可应用于食品和饲料工业的潜在天然植物防腐剂资源。