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Dynamics of aboveground net primary production of boreal steppe of northern Mongolia.

机译:蒙古北部寒带草原地上净初级生产力的动态。

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摘要

Understanding the spatial and temporal variability in aboveground net primary production (ANPP) of grassland ecosystems has remained a challenge because of complexity of ecological processes and patterns relating with temporal and spatial scales. In this dissertation, I studied the landscape scale (spatial) and temporal (annual) variability in ANPP while taking account of year-to-year variation of climatic factors, livestock grazing and vegetation structure as well as the gradient from wet and nutrient-rich sites (north-facing steppe) to dry and nutrient-poor site (south-facing steppe) in the cold and dry boreal steppe of Northern Mongolia, which is one of the hot spots of climate change because of its location at high latitude (51°N).;Livestock grazing increased species richness of wet and nutrient-rich sites as grazing tolerant species locally colonized and the species in the wet and nutrient-rich sites were driven to local extinction. In dry and nutrient-poor sites, no significant change was observed. However, plant communities in the dry and nutrient-poor south-facing steppe under grazing shifted to dominance by short and prostrate forb species.;For temporal variability in ANPP of the boreal steppe, the ungrazed north-facing lower had highest mean annual plant biomass while the lowest was observed in the grazed north-facing lower. For the other three landscape positions, mean annual plant biomass at the peak biomass period was not substantially different between our grazing levels. We found more temporal variability in total plant biomass in the grazed landscape than the ungrazed landscape. Climatic variables included in our analyses had more explanatory power for the temporal variability in total plant biomass in the grazed landscape. This might indicate a shift from dominance of effects of internal vegetation constraints on total plant biomass in an ungrazed landscape to dominance of effects of climate factors in a grazed landscape.;Nitrogen (N) is one of the main factors controlling ANPP in grassland ecosystem. We carried out a water and N manipulation experiment along a topographical gradient (south-facing upper and lower slopes) of the boreal steppe. We found results supporting co-limitation of water and N along the topographical gradient. We found strong positive effect of the interaction of water and N (H20 x N treatment) on ANPP at the both slopes; 3.5 times higher at the upper and 2.5 times at the lower slope.;Without a grazing effect, litter (plant dead material) is accumulated in the steppe. There is almost 4-fold high litter mass in ungrazed areas compared with grazed areas of mountain steppe of Northern Mongolia. Litter influences many important functions in grasslands including the water cycle, vegetation structure and ANPP. Using a litter and rainfall manipulation field experiment and water flux simulations, we found that the litter effect on soil water content was inconsistent among years; in a dry year with frequent small rainfall events, litter significantly affected the soil water while this effect was not detected in a wet year with frequent large storms. In the boreal steppe, the mean litter mass, 64 g m-2, did not significantly affect the amount of infiltration.;Traditional seasonal movement of Mongolian nomads can be an important part of the sustainability of boreal steppe. The traditional movement can lessen loss of species diversity at either local or regional scale. Especially in the permafrost area, livestock grazing resulted in the disappearance of moss cover, and the species adapted to the wet and nutrient rich site. Moss cover is the main insulator of permafrost. The loss of moss cover could potentially accelerate a thawing of permafrost and warming of this region. Also nomadic movement might lessen the high N limitation in the Mongolian grasslands through redistribution of soil nutrients by livestock. In order to prevent loss of litter biomass, which has a significant effect on the ANPP of the boreal steppe, I suggest that encouraging seasonal movement of Mongolian herders will make it possible to maintain the sufficient litter mass to support plant production for livestock. (Abstract shortened by UMI.).
机译:由于生态过程和与时空尺度有关的模式的复杂性,了解草原生态系统地上净初级生产(ANPP)的时空变化仍然是一个挑战。在这篇论文中,我研究了ANPP的景观尺度(空间)和时间(年度)变化,同时考虑了气候因素,牲畜放牧和植被结构以及湿润和养分丰富的梯度的逐年变化。蒙古北部寒冷干燥的北方草原的干旱地区(朝北的草原)到营养贫乏的地区(朝南的草原),这是气候变化的热点之一,因为它位于高纬度地区(51 °N).;家畜放牧增加了湿地和养分丰富的地方的物种丰富度,因为耐草的物种在当地定居,湿地和养分丰富的地方的物种被迫局部灭绝。在干燥和营养缺乏的地区,没有观察到明显的变化。然而,干旱和营养贫瘠的朝南草原放牧条件下的植物群落由短而pro的福布斯树种转移至优势地位。;对于北方草原ANPP的时间变异性,未放牧的朝北较低植物的年平均生物量最高最低的地方是朝北的草丛。对于其他三个景观位置,在我们的放牧水平之间,在生物量高峰期的年平均植物生物量没有显着差异。我们发现,放牧景观中植物总生物量的时间变异性要高于未放牧景观中植物的总生物量。我们的分析中包括的气候变量对于放牧景观中植物总生物量的时间变化具有更大的解释力。这可能表明从无植被景观中内部植被约束对总植物生物量的影响的主导向放牧景观中气候因子的影响的主导转变。氮是控制草地生态系统中ANPP的主要因素之一。我们沿着北方草原的地形梯度(朝南的上下坡度)进行了水和氮处理实验。我们发现了支持水和氮沿地形梯度共限制的结果。我们发现在两个斜坡上水和氮的相互作用(H20 x N处理)对ANPP都有很强的正效应。上部坡度高3.5倍,下部坡度高2.5倍;;没有掠食作用,凋落物(植物死皮)积聚在草原中。与蒙古北部山区草原的放牧地区相比,未擦拭地区的凋落物质量几乎提高了4倍。凋落物影响草地的许多重要功能,包括水循环,植被结构和ANPP。通过凋落物和降雨操纵场实验以及水通量模拟,我们发现凋落物对土壤水分的影响在多年间是不一致的。在干旱少雨的干旱年份,凋落物显着影响土壤水分,而在暴风雨频繁且潮湿的年份没有发现这种影响。在北方草原,平均凋落质量为64 g m-2,并没有显着影响入渗量。蒙古游牧民族的传统季节性运动可能是北方草原可持续性的重要组成部分。传统运动可以在地方或区域范围内减少物种多样性的丧失。特别是在多年冻土地区,放牧牲畜导致苔藓覆盖消失,并且该物种适应了潮湿和营养丰富的地区。苔藓覆盖物是永久冻土的主要绝缘体。苔藓覆盖的丧失可能会加速该地区多年冻土的融化和变暖。游牧运动也可能通过牲畜重新分配土壤养分来减轻蒙古草原的高氮限制。为了防止凋落物生物量的流失,这对北方草原的ANPP产生重大影响,我建议鼓励蒙古牧民的季节性迁徙将有可能保持足够的凋落物质量,以支持牲畜的植物生产。 (摘要由UMI缩短。)。

著录项

  • 作者

    Lkhagva, Ariuntsetseg.;

  • 作者单位

    University of Wyoming.;

  • 授予单位 University of Wyoming.;
  • 学科 Biology Ecology.;Agriculture Range Management.
  • 学位 Ph.D.
  • 年度 2014
  • 页码 185 p.
  • 总页数 185
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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