基于PSO-BP神经网络的高原寒地维修器材换算系数研究

针对高原寒地部队担负任务和所处地理环境的特殊性,军械装备维修器材受各种因素的影响,需求规律难以掌握,从5个方面18个对维修器材需求影响因素分析的基础上,分别对18个影响因素进行量化并归一化处理。运用粒子群优化算法对BP神经网络进行优化,提出了一种基于PSO-BP神经网络的维修器材换算系数模型,将影响因素作为输入变量,对不同种类的维修器材进行预测,通过算例分析验证该方法的合理性和准确性。

基于能力匹配的高原寒地弹药保障需求分析

为做好高山寒地战场环境下的战时弹药保障,深入剖析了高寒地区弹药供应保障需求,对弹药供应保障的数量需求、供应种类需求进行了分析。利用目标价值排序、需求量测算的方法分析了弹药供应的数量需求,给出了弹药需求量测算流程;结合弹药目标配对流程,通过计算各弹种打击该目标的经济性指标、时间性指标给出了弹药供应种类需求。科学的弹药保障供应需求研究,对于做好物资保障准备,科学应对边境反击作战具有重要的意义。

高原寒地军用物资供应保障研究

目的研究适应高原寒地作战环境下的军用物资供应保障模式与方法。方法分析高原寒地特殊的战场环境和未来作战特点对军用物资保障的影响,找出未来装备保障的特点及存在的主要问题。结果总结得到提升高原寒地作战军用物资保障能力的方式与方法。结论该研究为提升高原寒地作战军用物资保障能力,指导该方向作战保障实践提供了有价值的参考。

高原寒旱条件下蒙古黄芪种植技术

为了推动我国《中医药发展战略纲要规划(2016-2030)》和青海省《关于加快中藏药材种植基地建设的意见》的全面实施,通过蒙古黄芪引种、栽培、田间管理、病虫害防治、采挖、初加工等研究与种植示范,总结出了适合青海省冷凉气候条件下的蒙古黄芪稳产、高产种植技术。旨在推广蒙古黄芪种植技术,提高其种植水平,促进青海省农业产业调整,提高农牧民收入,加快脱贫致富的步伐。

高原寒旱条件下金银花种植技术

分别从山东、河南引进2个品种金银花,在高原寒旱地区青海省同仁县进行引种、栽培、田间管理、越冬、病虫害防治等研究与种植示范。结果表明:引进的2个品种的金银花采取越冬保护措施后,能在高原寒旱条件下生长,扩大了金银花在国内的种植区域。

优化神经网络下阿富汗东北高原寒旱区滑坡危险性评价

阿富汗东北部是典型的高原寒旱地区,滑坡灾害发育,除受地形地貌、地质构造、人类活动等因素影响外,还由积雪覆盖、冰雪消融等方面控制;为研究高原寒旱地区滑坡危险性,在遥感解译基础数据上,考虑高原寒旱地区积雪覆盖和冰川活动对滑坡发育的影响,引入积雪覆盖度和消融水当量两个评价指标,基于证据权‒全连接神经网络模型建立滑坡易发性评价模型,以度日模型、SCS-CN模型建立滑坡危险性评价体系,并根据混淆矩阵对评价模型进行检验;危险性评价结果表明极高危险性区域占全区10.46%,分布灾害面积占比82.71%,主要分布在努尔斯坦省东部库纳尔‒奇特拉尔河段、巴达赫尚省除瓦罕走廊段的中东部高山区和帕尔万省赫尔曼德河段;高危险性区域占全区14.83%,分布灾害面积占比12.11%,主要分布在巴达赫尚省东部区域、努尔斯坦省和帕尔万省西部.检验结果及统计结果均表明结合证据权法取负样本对神经网络精度提升显著;研究成果为阿富汗滑坡灾害早期预警与工程防治提供科学依据.

Effects of Temperature and Nitrogen Input on Nitrogen Mineralization in Alpine Soils on Tibetan Plateau

[Objective] The study aimed to investigate the effects of temperature and nitrogen input on nitrogen mineralization in alpine soils on the Tibetan Plateau.[Method]An incubation experiment in the laboratory was conducted using three alpine soils.These soils were collected from the top 10 cm depth in three grassland types：alpine meadow in Haibei,alpine steppe in Naqu and alpine wetland in Dangxiong.[Result] Temperature significantly affected nitrogen mineralization in alpine soils of three grassland types.The mineralization rate in alpine steppe soil rose with the rise of temperature,while the mineralization rate in the alpine meadow soil and alpine wetland soil decreased with the rise of temperature.Nitrogen input had no significant effect on nitrogen mineralization in the alpine meadow soil,but significantly increased nitrogen mineralization in the alpine steppe soil and the alpine wetland soil.Grassland types significantly affected nitrogen mineralization in alpine grasslands.[Conclusion] The effects of temperature and nitrogen input on nitrogen mineralization in alpine soils on the Tibetan Plateau were significant.And those different effects depended on different types of grassland.

高原寒环境暴露对急进入高原健康人群肾功能的影响

目的:探讨高原低压低氧寒环境对急进高原的平原健康人群肾功能的影响。方法:选取30例长期居住兰州地区急进高原(海拔3300米、日平均气温-4度)健康人群,对比分析所有受试者进驻高原前和进驻高原后第24 h、72 h、7天、14天、28天尿IL-18(白介素-18)、尿NAGL(中性粒细胞明胶酶相关性脂质运载蛋白)、尿KIM-1(肾损伤因子-1)及血肌酐水平的变化。结果:共28人完成全部6次尿液及血标本采集并检测,其中2名女性因某次采集点处于月经期剔除,其中男性17人、女性11人,平均年龄26.8±3.2岁(男性28.3±4.2岁,女性24.8±2.6岁)。进入高原前和进驻高原后第24 h、72 h、7天、14天、28天尿IL-18检测值分别为3.62±0.32 ng/L、11.20±0.65 ng/L(P<0.001,较进入前组比较)、6.32±0.46 ng/L(P<0.001)、4.36±0.68 ng/L(P<0.05)、3.58±0.71 ng/L、3.32±0.46 ng/L;尿NAGL水平分别为0.126±0.20μg/L、0.513±0.003μg/L(P<0.001)、0.116±0.006μg/L、0.009±0.001μg/L、0.121±0.010μg/L、0.632±0.009μg/L;尿KIM-1水平分别为2.61±0.22 ng/L、18.20±0.69 ng/L(P<0.001)、6.32±0.46 ng/L(P<0.001)、6.36±0.68 ng/L(P<0.001)、2.58±0.31 ng/L、2.32±0.26 ng/L;血肌酐水平分别为61.0±9.16μmol/L、58.5±8.13μmol/L、80.3±10.38μmol/L(P<0.05)、76.5±12.04μmol/L(P<0.05)、62.6±10.14μmol/l、62.3±8.18μmol/L。结论:急进高原健康入群早期肾功能有改变,其中尿IL-18、尿KIM-1、尿NAGL水平较血肌酐水平变化更早、更敏感。

Dynamics of Above-and Below-ground Biomass and C,N,P Accumulation in the Alpine Steppe of Northern Tibet

The temporal dynamics of the biomass, as well as the carbon （C）, nitrogen （N）, phosphorus （P） concentrations and accumulation contents, in above- and below-ground vegetation components were determined in the alpine steppe vegetation of Northern Tibet during the growing season of 2OLO. The highest levels of total biomass （311.68 g m-2）, total C （115.95 g m-2）, total N （2.60 g m-2）, and total P （0.90 g m-2） accumulation contents were obtained in August in 2010. Further, biomass and nutrient stocks in the below-ground components were higher than those of the above-ground components. The dominant species viz., Stipa purpurea and Carex moorcrofli had lower biomass and C, N, P accumulations than the companion species which including Oxytropis. spp., Artemisia capillaris Thunb., Aster tataricus L., and SO on.

Research on the Soil Carbon Storage of Alpine Grassland under Different Land Uses in Qinghai-Tibet Plateau

In this article, we mainly analysis the soil carbon storage of the alpine grassland under different land uses in Qinghai-Tibet Plateau. The samples of this investigation include six experimental fields which are fenced mowing grassland, artificial grassland, winter and spring grazing meadowland, summer and autumn mild grazing land, summer and autumn moderate grazing pasture and summer and autumn severe grazing land and seven soil layers included 0 cm-5 cm, 5 cm-10 cm, 10 cm-20 cm, 20 cm-30 cm, 30 cm-50 cm, 50 cm-70 cm and 70 cm-100 cm. The results show that the soil carbon storage in different soil layers will gradually reduce and the difference was remarkable （P 〈 0.05）. What is more, the soil carbon storage of alpine grassland under different land uses has following sequence： winter and spring grazing grassland 〉 summer and autumn mild grazing land 〉 artificial grassland 〉 summer and autumn moderate grazing meadowland 〉 summer and autumn severe grazing pasture 〉 fenced mowing meadow, and the significant difference between them is remarkable （P 〈 0.05）.

Biomass Allocation Patterns of Alpine Grassland Species and Functional Groups along a Precipitation Gradient on the Northern Tibetan Plateau

Variations in the fractions of biomass allocated to functional components are widely considered as plant responses to resource availability for grassland plants. Observations indicated shoots isometrically relates to roots at the community level but allometrically at the species level in Tibetan alpine grasslands. These differences may result from the specific complementarity of functional groups between functional components, such as leaf, root, stem and reproductive organ. To test the component complementary responses to regional moisture variation, we conducted a multi-site transect survey to measure plant individual size and component biomass fractions of common species belonging to the functional groups： forbs, grasses, legumes and sedges on the Northern Tibetan Plateau in peak growing season in 2010. Along the mean annual precipitation （MAP） gradient, we sampled 7o species, in which 2o are in alpine meadows, 20 in alpine steppes, 15 in alpine desert-steppes and 15 in alpine deserts, respectively. Our results showed that the size of alpine plants is small with individual biomass mostly lower than 1.0 g. Plants keep relative conservative component individual responses moisture functional fractions across alpine grasslands at the level. However, the complementary between functional components to variations specifically differ among groups. These results indicate that functional group diversity may be an effective tool for scaling biomass allocation patterns from individual up to community level. Therefore, it is necessary andvaluable to perform intensive and systematic studies on identification and differentiation the influences of compositional changes in functional groups on ecosystem primary services and processes.

Sources of uncertainty in exploring rangeland phenology： A case study in an alpine meadow on the central Tibetan Plateau

Global climate change has been found to substantially influence the phenology of rangeland,especially on the Tibetan Plateau. However, there is considerable controversy about the trends and causes of rangeland phenology owing to different phenological exploration methods and lack of ground validation. Little is known about the uncertainty in the exploration accuracy of vegetation phenology.Therefore, in this study, we selected a typical alpine rangeland near Damxung national meteorological station as a case study on central Tibetan Plateau, and identified several important sources influencing phenology to better understand their effects on phenological exploration. We found man-made land use was not easily distinguished from natural rangelands, and therefore this may confound phenological response to climate change in the rangeland. Change trends of phenology explored by four methods were similar, but ratio threshold method(RTM) was more suitable for exploring vegetation phenology in terms of the beginning of growing season(BGS) and end of growing season(EGS). However, some adjustments are needed when RTM is used in extreme drought years. MODIS NDVI/EVI dataset was most suitable for exploring vegetation phenology of BGS and EGS. The discrimination capacities of vegetation phenology declined with decreasing resolution of remote sensing images from MODIS to GIMMS AVHRR datasets. Additionally, distinct trends of phenological change rates were indicated in different terrain conditions, with advance of growing season in high altitudes but delay of season in lower altitudes. Therefore, it was necessary to eliminate interference of complex terrain and man-made land use to ensure the representativeness of natural vegetation. Moreover, selecting the appropriate method to explore rangelands and fully considering the impact of topography are important to accurately analyze the effects of climate change on vegetation phenology.

Mechanism of plant-soil feedback in a degraded alpine grassland on the Tibetan Plateau

Although biotic and abiotic factors have been confirmed to be critical factors that affect community dynamics,their interactive effects have yet to be fully considered in grassland degradation.Herein,we tested how soil nutrients and microbes regulated plant-soil feedback(PSF)in a degraded alpine grassland.Our results indicated that soil total carbon(STC;from 17.66 to 12.55 g/kg)and total nitrogen(STN;from 3.16 to 2.74 g/kg)exhibited significant(P<0.05)decrease from non-degraded(ND)to severely degraded(SD).Despite higher nutrients in ND soil generating significantly(P<0.05)positive PSF(0.52)on monocots growth when the soil was sterilized,a high proportion of pathogens(36%)in ND non-sterilized soil resulted in a strong negative PSF on monocots.In contrast,the higher phenotypic plasticity of dicots coupled with a higher abundance of mutualists and saprophytes(70%)strongly promoted their survival and growth in SD with infertile soil.Our findings identified a novel mechanism that there was a functional group shift from monocots with higher vulnerability to soil pathogens in the ND fertile soil to dicots with higher dependence on nutritional mutualists in the degraded infertile soil.The emerging irreversible eco-evolutionary in PSF after degradation might cause a predicament for the restoration of degraded grassland.

Species Richness and Diversity of Alpine Grasslands on the Northern Tibetan Plateau:Effects of Grazing Exclusion and Growing Season Precipitation

Species richness and diversity indices （Shannon-Wiener index, Simpson dominance index and Pielou evenness index） in alpine grassland ecosystems （alpine meadow, alpine steppe and desert steppe） under grazing-excluded and freely grazed sites were investigated along the Northern Tibetan Plateau Alpine Grassland Transect during summer 2009 and 2010. We found that species richness and diversity have not been significantly altered by short-term grazing exclusion since 2006 at vegetation and regional scales. Species richness and diversity were mainly driven by growing season precipitation （GSP）, which accounted for over 87 % of the total variation observed, Species richness and diversity at grazing- excluded and freely grazed sites appear to respond to growing season precipitation in parallel. Species richness exponentially increased with GSP while diversity indices showed positively linear relationships with GSP. This indicates that GSP on the Northern Tibetan Plateau is crucial in regulating species richness and diversity and should be taken into account in future studies on alpine grassland conservation.

Climatic and Edaphic Controls on Soil pH in Alpine Grasslands on the Tibetan Plateau,China:A Quantitative Analysis

Soil acidity is an important parameter that can regulate ecosystem structure and function.However,a quantitative understanding of the relationships between soil pH and environmental factors remains unavailable.In this study,relationships of soil pH with both climatic and edaphic factors in alpine grasslands on the Tibetan Plateau,China were quantified using data obtained from a regional soil survey during 2001-2004.Our results showed that soil pH decreased along the gradient of both mean annual temperature and precipitation.Likewise,soil pH exhibited consistent negative correlations with soil moisture and silt content.However,soil organic and inorganic carbon contents played opposite roles in shaping patterns of soil pH:the accumulation of soil organic matter led to higher soil acidity,while the existence of soil inorganic matter was favorable for maintaining higher soil alkalinity.The variation partitioning analysis indicated that the combination of climatic and edaphic variables explained 74.3%of the variation in soil acidity.These results suggest that soil pH could be predicted from routinely-measured variables,allowing a robust pedotransfer function to be developed.The pedotransfer function may facilitate land surface models to generate more reliable predictions on ecosystem structure and function around the world.

Distribution of fatty acids in the alpine grassland soils of the Qinghai-Tibetan Plateau

As an important biomarker, fatty acids(FAs) have been extensively used to trace the origin of organic matter in sediments and soils. However, studies of the distribution and abundance of FAs in alpine grassland soils are still rare, especially on the Qinghai-Tibetan Plateau(QTP), the highest plateau in the world, which contributes sediments to many large rivers in Asia. This study investigates the composition, distribution and source of FAs with increasing soil depths from 17 typical alpine grassland sites in the QTP. The most abundant FAs included the ubiquitous C16 FA and even-numbered long-chain FAs(C20–C30), indicating mixed inputs from microbial and higher plant sources. Source apportionment showed that higher plants were the dominant contributor of FAs(approximately 40%) in QTP soils. The abundance of FAs decreased with soil depth, with the highest value(1.08±0.09 mg/g C) at a 0–10 cm depth and the lowest value(0.46±0.12 mg/g C) at a 50–70 cm depth, due to much lower plant inputs into the deeper horizons. The total concentration of FAs was negatively correlated to the mean annual temperature(MAT; P<0.05) and soil p H(P<0.01), suggesting that the preservation of FAs was favored in low-MAT and low-p H soils on the QTP. The abundance of fresh C source FAs increased significantly with the mean annual precipitation(MAP; P<0.05), indicating that high MAP facilitates the accumulation of fresh FAs in QTP soils. Other environmental parameters, such as the soil mineral content(aluminum and iron oxide), microbial community composition as well as litter quality and quantity, may also exert a strong control on the preservation of FAs in QTP soils and warrant further research to better understand the mechanisms responsible for the preservation of FAs in QTP soils.