祁连山西段草地土壤温度、水分变化特征

研究土壤水热要素对合理预测祁连山气候变化特征及建立气候预警系统有重要意义。采用18套土壤温、湿度自动记录仪(HOBOU30)对祁连山西段草地进行3a连续定位监测,旨在探索分析该区土壤水热变化特征,阐明土壤水热互作效应及耦合机制。表明:1)冷期(1—3、11—12月)占全年的42%,暖期(4—10月)占58%;7月前土壤均温随月份增大而增大,月份增大1月土壤均温增大3.53℃,水分增大3.23%;7月后随月份增大而减小,月份增大1月土壤均温降低4.73℃,水分下降2.55%。2)日变化16:00前土壤均温为7.45℃,水分为16.26%,16:00后均温为9.1℃,水分为16.79%,16:00后比前均温高1.65℃,水分高0.54%。3)土温、水分与海拔均呈线性正相关,前者差异显著(P0.05),后者不显著(P0.05)。4)土温逐层(0—120 cm)平均递增0.07℃,水分递减0.58%;土温与土层深度呈显著线性正相关(P0.05,R2=0.99),水分呈显著线性负相关(P0.05,R2=0.97)。5)该区土温与水分呈显著线性负相关。因此,祁连山西段草地土温变幅较小,水分变幅大,两者在空间上变化均呈二次函数,时间上均呈一次函数。     

Projecting future grassland productivity to assess the sustainability of potential biofuel feedstock areas in the Greater Platte River Basin

This study projects future (e.g., 2050 and 2099) grassland productivities in the Greater Platte River Basin (GPRB) using ecosystem performance (EP, a surrogate for measuring ecosystem productivity) models and future climate projections. The EP models developed from a previous study were based on the satellite vegetation index, site geophysical and biophysical features, and weather and climate drivers. The future climate data used in this study were derived from the National Center for Atmospheric Research Community Climate System Model 3.0 ‘SRES A1B’ (a ‘middle’ emissions path). The main objective of this study is to assess the future sustainability of the potential biofuel feedstock areas identified in a previous study. Results show that the potential biofuel feedstock areas (the more mesic eastern part of the GPRB) will remain productive (i.e., aboveground grassland biomass productivity >2750 kg ha^?1 year^?1) with a slight increasing trend in the future. The spatially averaged EPs for these areas are 3519, 3432, 3557, 3605, 3752, and 3583 kg ha^?1 year^?1 for current site potential (2000–2008 average), 2020, 2030, 2040, 2050, and 2099, respectively. Therefore, the identified potential biofuel feedstock areas will likely continue to be sustainable for future biofuel development. On the other hand, grasslands identified as having no biofuel potential in the drier western part of the GPRB would be expected to stay unproductive in the future (spatially averaged EPs are 1822, 1691, 1896, 2306, 1994, and 2169 kg ha^?1 year^?1 for site potential, 2020, 2030, 2040, 2050, and 2099). These areas should continue to be unsuitable for biofuel feedstock development in the future. These future grassland productivity estimation maps can help land managers to understand and adapt to the expected changes in future EP in the GPRB and to assess the future sustainability and feasibility of potential biofuel feedstock areas.     

Nitrogen economy of alpine plants on the north Tibetan Plateau: Nitrogen conservation by resorption rather than open sources through biological symbiotic fixation

Nitrogen (N) is one of the most important factors limiting plant productivity, and N fixation by legume species is an important source of N input into ecosystems. Meanwhile, N resorption from senescent plant tissues conserves nutrients taken up in the current season, which may alleviate ecosystem N limitation. N fixation was assessed by the ¹⁵N dilution technique in four types of alpine grasslands along the precipitation and soil nutrient gradients. The N resorption efficiency (NRE) was also measured in these alpine grasslands. The aboveground biomass in the alpine meadow was 4–6 times higher than in the alpine meadow steppe, alpine steppe, and alpine desert steppe. However, the proportion of legume species to community biomass in the alpine steppe and the alpine desert steppe was significantly higher than the proportion in the alpine meadow. N fixation by the legume plants in the alpine meadow was 0.236 g N/m², which was significantly higher than N fixation in other alpine grasslands (0.041 to 0.089 g N/m²). The NRE in the alpine meadows was lower than in the other three alpine grasslands. Both the aboveground biomass and N fixation of the legume plants showed decreasing trends with the decline of precipitation and soil N gradients from east to west, while the NRE of alpine plants showed increasing trends along the gradients, which indicates that alpine plants enhance the NRE to adapt to the increasing droughts and nutrient‐poor environments. The opposite trends of N fixation and NRE along the precipitation and soil nutrient gradients indicate that alpine plants adapt to precipitation and soil nutrient limitation by promoting NRE (conservative nutrient use by alpine plants) rather than biological N fixation (open sources by legume plants) on the north Tibetan Plateau.     

内蒙古荒漠草原植物遗传多样性对模拟增温处理的响应

为探究全球变暖对温带荒漠草原地上种群的遗传影响,对已经接受模拟增温处理6年的短花针茅草原4种不同生活型植物,即半灌木、多年生禾草、多年生杂类草和一年生植物,应用AFLP分子标记方法研究了其遗传多样性和遗传结构。结果显示,对照处理与增温处理下的木地肤、短花针茅、细叶葱、猪毛菜4种植物的多态位点百分率(PPB)分别为11.32%,11.32%;40.83%,39.91%;14.29%,13.10%;19.85%,19.12%。Nei's基因多样性指数(He)分别为0.0274,0.0259;0.0812,0.0899;0.0131,0.0084;0.0506,0.0456。Shannon's信息指数值(I)分别为0.0447,0.0430;0.1354,0.1466;0.0267,0.0182;0.0811,0.0733。分子方差分析(AMOVA)显示4种植物的变异主要来源于实验处理内部,木地肤为85.03%,短花针茅为66.35%,细叶葱为70.00%,猪毛菜为66.52%;增温处理间的变异分别占-2.81%,-5.47%,-3.60%,2.53%(P0.05)。4种植物增温处理与变异程度之间在统计学上并无相关性。研究表明虽然短时间的模拟增温并不足以使4种生活型植物种群遗传多样性和遗传结构发生显著变化,但相对于3种多年生植物,一年生植物猪毛菜更容易受到增温影响。多年生和一年生植物对增温具有不同的遗传响应。     

半干旱区沙质退化草地造林对土壤质量的影响

采用野外调查与室内培养相结合的方法,研究了我国北方半干旱区科尔沁沙地退化草地营造樟子松人工林32年后0～10 cm表层土壤理化性状、土壤碳氮矿化量、土壤微生物量以及土壤酶活性等的变化. 结果表明32年生樟子松人工林土壤有机碳、全氮和全磷等养分含量分别下降了21%、42%和45%;5月和11月樟子松人工林土壤NH4 -N显著高于草地(P=0.001;P=0.019),而5、8和11月草地土壤NO3--N含量显著高于樟子松人工林(P＜0.001;P=0.048;P=0.031);5、8和11月樟子松人工林土壤有机碳日矿化释放的CO2-C量均大于草地,而二者土壤氮矿化率差异不显著(P＞0.05);5和8月樟子松人工林土壤微生物量碳含量与草地相比差异不显著,11月则显著高于草地;土壤养分和水分含量是影响土壤微生物量碳含量的重要因素;与草地相比,樟子松人工林土壤脲酶和蔗糖酶活性降低,而土壤过氧化氢酶活性升高. 上述结果说明半干旱区沙质退化草地营造樟子松人工林32年后土壤质量出现一定程度的下降;由于植被的改变,樟子松人工林土壤理化性状和生物学性状等表现出与草地不同的季节动态特征.造林作为我国北方半干旱区沙地退化生态系统的一种恢复手段具有一定的局限性.     

Not all droughts are created equal: the impacts of interannual drought pattern and magnitude on grassland carbon cycling

Climate extremes, such as drought, may have immediate and potentially prolonged effects on carbon cycling. Grasslands store approximately one‐third of all terrestrial carbon and may become carbon sources during droughts. However, the magnitude and duration of drought‐induced disruptions to the carbon cycle, as well as the mechanisms responsible, remain poorly understood. Over the next century, global climate models predict an increase in two types of drought: chronic but subtle ‘press‐droughts’, and shorter term but extreme ‘pulse‐droughts’. Much of our current understanding of the ecological impacts of drought comes from experimental rainfall manipulations. These studies have been highly valuable, but are often short term and rarely quantify carbon feedbacks. To address this knowledge gap, we used the Community Land Model 4.0 to examine the individual and interactive effects of pulse‐ and press‐droughts on carbon cycling in a mesic grassland of the US Great Plains. A series of modeling experiments were imposed by varying drought magnitude (precipitation amount) and interannual pattern (press‐ vs. pulse‐droughts) to examine the effects on carbon storage and cycling at annual to century timescales. We present three main findings. First, a single‐year pulse‐drought had immediate and prolonged effects on carbon storage due to differential sensitivities of ecosystem respiration and gross primary production. Second, short‐term pulse‐droughts caused greater carbon loss than chronic press‐droughts when total precipitation reductions over a 20‐year period were equivalent. Third, combining pulse‐ and press‐droughts had intermediate effects on carbon loss compared to the independent drought types, except at high drought levels. Overall, these results suggest that interannual drought pattern may be as important for carbon dynamics as drought magnitude and that extreme droughts may have long‐lasting carbon feedbacks in grassland ecosystems.     

内蒙古伊金霍洛旗农业生产力的评估与预测

运用伊金霍洛旗40年的气象与农业统计资料,分析了气候与化肥使用量对于粮食产量的综合影响．选取综合模型为基础,将化肥对粮食气候生产潜力的影响考虑为调节因子,建立了基于气候和化肥使用量的粮食产量评估模型．同时,基于伊金霍洛旗地区人口、气候以及化肥的未来变化情景,预测了未来30年的粮食需求增长量,指出在满足当地人民对粮食作物基本需求的基础上,从目前到2010年期间退耕面积达622～5948hm^2,相当于原有耕地的3％～31％;从2010年到2020年期间退耕面积最大,达3263～8164hm^2,相当于原有耕地的17％42％;随后10年由于土地单位面积的增产是有限度的,而人口继续增长,将导致耕地面积有所回升,但变动幅度不会太大,基本维持在2020年的水平。     

黄土高原草地畜牧业产业形成与发展的牧草生产力基础

在黄土高原197个区县土地利用方式重新规划的基础上,对黄土高原畜牧业产业形成与发展的牧草生产潜力进行了分析预测。结果表明：规划的牧、林、农、果用地占生产用地的比例分别是草地44％、林地22％、基本农田20％、果园14％;197个区县草地牧草生产、作物秸秆、草田轮作和果园种草预测的总牧草饲料生产潜力达104881028t／a(其中,草地牧草生产潜力约占45％,达47196462．7t／a),可载畜104881028个羊单位／a(其中草地可载畜47196462．7个羊单位／a)。按1999年不变价格计算,黄土高原预测畜牧业总产值将达到5244051万元RMB／a,是1999年畜牧业总产值的5．3倍,超过1999年黄土高原农业总产值14％。农业人口人均预测畜牧业产值大于l000元的区县占59％;小于l000元的区县占41％。此外,预测的农业总产值将达到l147．2234亿元RMB／a,其中畜牧业、果业、林业和农业产值占农业总产值的比重分别是46％、27％、14％和13％。随着畜牧业产业链的逐步建立与完善,产业发展布局的日趋合理,黄土高原畜牧业生产总值将有较大幅度的提高,黄土高原生态环境将有进一步的改善。黄土高原草地畜牧业蕴藏着巨大的发展潜力,有望成为黄土高原优化的生产一生态新产业带建制中的支柱产业。     

草原火烧严重度燃烧指数的适用性比较分析

基于遥感影像的燃烧指数被广泛应用于火烧严重度(fire severity)研究,选取适宜燃烧指数定量评估草原火烧严重度,对草原生态系统植被的恢复与管理具有重要意义。以呼伦贝尔草原火烧迹地为研究区域,基于landsat8 OLI影像分别构建4种燃烧指数(NBR、NSTV1、d NBR和Rd NBR)与综合燃烧指数(CBI)的回归模型并进行精度验证,对比分析不同燃烧指数识别草原火烧严重度等级的能力。结果表明:在燃烧指数与CBI构建的回归模型中,d NBR指数的相关性(n=70,R~2=0.856)最高;4种燃烧指数识别火烧严重度的精度存在差异,中度火烧区域(1CBI≤2)内,NSTV1指数识别精度最高,未过火(CBI=0)、轻度火烧(0CBI≤1)和重度火烧(2CBI≤3)区域内,d NBR指数识别精度均表现最好,分别为80%、62.5%和100%;基于不同燃烧指数的草原火烧严重度制图中,d NBR指数的总体精度同样高于其他燃烧指数,为82.1%,Kappa系数高达0.76。综上所述,d NBR指数是草原火烧严重度分析与评价的适宜遥感指数。     

刈割制度对呼伦贝尔草原群落特征及牧草质量的影响

为确定呼伦贝尔草原高效生产和可持续利用的最佳刈割制度,于2019—2021年在呼伦贝尔草原开展刈割时间(7月31日、8月10日、8月20日、8月30日、9月9日)、留茬高度(3、9、15 cm)及两者交互作用对草原群落特征、牧草产量和品质影响的研究。结果表明: 较晚时间刈割和低留茬刈割会降低翌年群落高度和盖度;低留茬刈割降低翌年地上部分生物量,但刈割时间对其影响不显著。禾草、莎草相对生物量随刈割时间的延迟表现出先增加后减少的趋势,杂类草则与之相反,而豆科植物无明显变化。低留茬刈割在当年能够获得高的干草产量,但翌年的干草产量显著下降;8月30日,留茬3 cm刈割时干草产量达到最高值(469 g·m^-2),高于最低值361.5%。牧草品质中粗蛋白含量在8月30日刈割时亦达到峰值,高于最低值约6.5%,且在高留茬刈割下含量更高;酸、中性洗涤纤维含量随刈割时间延迟逐渐升高,9月9日刈割高于7月31日8.0%、5.9%,并且随留茬高度增加而降低。呼伦贝尔草原刈割制度设置为留茬高度9 cm左右、8月20—30日刈割为最佳,但需更长期的刈割试验观测才能得到更可靠、更客观的结论。