极端干旱区沙土掩埋对凋落物分解速率及盐分含量动态的影响

极端干旱区由于降水稀少, 植被盖度低, 太阳辐射强烈, 以及土壤稳定性差, 导致其凋落物周转不同于非干旱区。为探究极端干旱区凋落物分解规律, 该研究利用凋落物分解袋法, 以塔克拉玛干沙漠南缘沙漠-绿洲过渡带优势物种花花柴(Karelinia caspia)、骆驼刺(Alhagi sparsifolia)和胡杨(Populus euphratica)凋落叶为研究对象, 设置不同的沙土掩埋处理: 地表、2 cm和15 cm埋深, 以模拟自然条件下凋落物分解环境, 测定分解过程中凋落物质量和水溶性盐的变化特征。结果表明: 极端干旱区凋落物分解速率与凋落物初始碳(C)含量、氮(N)含量、C:N和木质素含量的关系与非干旱区存在较大差异, 在地表处理下, 木质素含量越高, 质量损失越快。不同分解环境下凋落物质量和水溶性盐损失具有显著差异, 与15 cm埋深相比, 地表和2 cm埋深处理显著增加了凋落物的质量损失和水溶性盐总量损失。地表处理增加了凋落物分解前期的水溶性盐溶解量。该研究表明, 极端干旱区凋落物分解的驱动机制具有独特性, 由于降水稀少, 土壤微生物的活性较低, 掩埋深度不是驱动凋落物分解的主要因素, 极端干旱区凋落物的分解主要受其他非生物过程如太阳光辐射的影响。     

Comparative analysis of leaf angle and sclerophylly of Aspidosperma quebracho‐blanco on a water deficit gradient

Abstract Aspidosperma quebracho‐blanco is found throughout the Chaco (17°?33°S) in Argentina, and it is the dominant tree species in the arid Chaco. Under the hypothesis that morpho‐physiological features of A. quebracho‐blanco change as a function of its geographical position on a water deficit gradient, it was predicted that with increasing water stress, leaf angles (specifically horizontal) would be greater and mean values of the leaf mass per area would increase. These leaf characteristics were compared at three points on a water deficit gradient extending from the humid Chaco through semi‐arid Chaco to the arid Chaco of Argentina (south‐west to north‐east rainfall gradient, from 350 to 1200 mm annual mean precipitation). Twig and leaf positions were modified and water potentials were measured at the highest heating hour of the day at a site of the arid Chaco. Daily and seasonal water potential variations of untreated twigs were also observed. Leaf angle modification towards horizontal produced more negative twig water potentials with respect to those of leaves in non‐horizontal positions. The comparison of the three sites along the gradient showed contrasting patterns of leaf‐angle frequency distribution of adults. In Chancaní (mean annual temperature: 18–24°C, mean annual precipitation: 450 mm, arid) there was a higher frequency of angles near 90° for non‐pendulous and about 270° for pendulous trees. Leaf angles in Copo (semi‐arid) and Chaco National Park (mean annual temperature: 20–23°C, mean annual precipitation: 1300 mm humid) were widely distributed with higher frequency towards the angles near 0° and 180°. This sclerophyllous tree species showed plasticity in its leaf traits along the precipitation gradient. Plasticity in leaf mass per area and leaf position enables plants to develop efficiently in contrasting environmental conditions of humidity and aridity.     

不同水分条件下毛果苔草枯落物分解及营养动态

于2009年5月至2010年5月采用分解袋法,研究了三江平原典型湿地植物毛果苔草枯落物分解对水分条件变化的响应,探讨了典型碟形洼地不同水位下枯落物分解1a时间内的分解速率与N、P等营养元素动态。分解1a内,无积水环境下枯落物失重率为34.99%,季节性积水环境下为27.28%,常年积水环境下随水位增加枯落物失重率分别为26.99%与30.67%,表明积水条件抑制了枯落物的分解。枯落物的分解随环境变化表现出阶段性特征,分解0—122 d内随水位增加枯落物失重率分别为16.09%、24.25%、23.53%与26.60%,即生长季内积水条件促进了枯落物有机质的分解及重量损失。而随实验进行,分解122—360 d内随水位增加毛果苔草枯落物的失重率分别为18.90%、3.02%、3.46%、4.03%,即在非生长季土壤冻融期积水条件抑制了枯落物分解(P<0.05)。水分条件对毛果苔草枯落物N元素的影响表现为积水条件促进生长季内枯落物的N固定,水位最高处毛果苔草N浓度显著高于无积水环境(P<0.05)。但进入冻融期后积水环境下枯落物N浓度与含量降低;其中季节性积水限制了枯落物的N积累能力,至分解360d时与初始值相比表现出明显的N释放(P=0.01)。毛果苔草枯落物分解61d时P出现富集,其中积水条件下P的富集作用增强,但与水位不相关。分解1a后毛果苔草枯落物表现为P的净释放,不同水分条件下枯落物P元素损失没有明显差异(P>0.05)。     

Large Rainfall Pulses Control Litter Decomposition in a Tropical Dry Forest: Evidence from an 8-Year Study

We investigated the influence of rainfall attributes on litter decomposition over an 8-year period in a well-preserved tropical dry forest ecosystem in western Mexico. We examined the relationship between the size and number of rainfall events and rainy-season litter decomposition rates and determined if this relationship varied along a landscape gradient. A mass balance approach was used to estimate decomposition rate in four permanent 2,400 m² plots located in two small watersheds. Watershed I included three plots in different landscape positions (upper, middle, and lower) in the elevation gradient, whereas Watershed IV included one plot in the middle position. Surface litter C mass was lower in the rainy than in the dry season in all plots in response to seasonal fluctuations in rainfall. The frequency of small (≤5 mm) and medium (5.1–9.9 mm) size rainfall events largely did not correlate with litter decomposition, but the frequency of large events (≥10 mm) had a positive correlation with decomposition rates (P < 0.05), except in plot IV (P < 0.1). Decomposition rates were similar among plots at the different landscape positions within Watershed I (P > 0.05). The relevance of large rainfall events (≥10 mm) in rainy-season litter decomposition suggests that changes in the precipitation regime which alter the frequency of these rainfall pulses or increase their variability would affect the vulnerability of the litter C and nutrient pools to extreme events.     

Intraspecific variation in resistance to desiccation in the land snailTheba pisana

Theba pisana is a bush-dwelling snail with a circum-Mediterranean distribution. In Israel it is limited to a narrow coastal strip, along which there is a north-to-south gradient in mean annual rainfall (700–300 mm per year). In this study we found significant intraspecific differences among populations ofT. pisana in resistance to desiccation along this gradient, and in a population from Greece, which may be grossly correlated with the climatic gradient. The Greek population was the least resistant to desiccation with an extremely high rate of water loss. The differences in total mass loss were mainly determined by the rate of water loss during the first 4 days of desiccation. A general phenomenon during desiccation was the close regulation of the soft body water content at the expense of the extra-pallial fluid compartment.     

氮沉降与降雨变化下中小型土壤动物对凋落物分解的影响

土壤动物是凋落物分解、养分转化过程的重要调节者,全球变化驱动的氮沉降与降雨变化通过改变其分解环境和土壤动物群落结构,进而影响凋落物分解进程。为了探究中小型土壤动物对凋落物分解的贡献受氮沉降和降雨变化的影响,本研究利用不同网孔(2 mm和0.01 mm)的凋落物分解网袋法,以建群种短花针茅为研究对象进行野外分解试验。试验采用裂区设计,主区为自然降雨(CK)、增雨30%(W)和减雨30%(R)3个水分处理,副区为0(N₀)、30(N₃₀)、50(N₅₀)和100(N₁₀₀) kg·hm^-2·a^-1 4个氮素处理。结果表明: 1)降雨变化显著影响了凋落物的分解速率,增雨处理中凋落物的分解速率加快,且随着氮添加浓度的升高,凋落物重量残留率逐渐降低,100 kg·hm^-2·a^-1时分解速度最快;在减雨处理与对自然降雨处理中凋落物的分解速率则呈先降低后升高的趋势,在50 kg·hm^-2·a^-1时分解速度最快。氮沉降和降雨变化对凋落物分解无显著的交互作用。2)在整个分解过程中,共捕获中小型土壤动物1577只,隶属于1门3纲13目(含亚目)49科,优势类群为蜱螨目、鞘翅目幼虫和弹尾目;增雨施氮提升了中小型土壤动物群落的类群数和个体数。3)凋落物重量残留率与中小型土壤动物类群数、个体数均呈极显著负相关,增雨处理整体提高了中小型土壤动物对凋落物分解的贡献率。综上,荒漠草原上中小型土壤动物对凋落物的分解具有积极作用,且水分和氮素输入的增加提高了中小型土壤动物的类群数及个体数,增加了其对凋落物分解的贡献;在水分不足时,过量的氮素会抑制中小型土壤动物群落的发展,导致中小型土壤动物对凋落物分解的贡献降低。     

不同水分条件下杨树-玉米复合系统凋落物分解特性

为探讨水分变化对农林复合生态系统凋落物分解特性的影响,以河西走廊杨树（Populus）-玉米（Zea mays）凋落物为研究对象,设置正常水分（9200 m³/hm²,对照）,轻度干旱胁迫（减少15%,7800 m³/hm²）,中度干旱胁迫（减少30%,6400 m³/hm²）3种不同水分处理条件,采用分解袋法研究了不同水分条件下杨树叶和玉米秸秆的质量残留率、分解速率和养分含量变化特征。结果表明：（1）随着干旱胁迫的加剧,两种凋落物的质量残留率均增加,而分解速率降低。经过164 d的分解后,杨树叶和玉米秸秆的质量残留率分别为70.43%-77.49%、63.55%-68.29%。分析表明：水分和时间对各类型凋落物的质量残留率均有极显著的影响（P<0.001）,但二者的交互作用不显著（P>0.05）;干旱胁迫显著降低了玉米秸秆的分解速率,但杨树叶的分解速率却只是在中度干旱胁迫下显著降低（P<0.05）。对于不同类型凋落物而言,分解速率表现为玉米秸秆>杨树叶。（2）两种类型凋落物的氮（N）残留率在分解过程中表现为降低的趋势,但随着干旱程度的加大,N的残留率增加,表明水分抑制了N的释放过程。分解164d后,同一类型凋落物不同水分条件下的N残留率均存在显著差异。对于同一水分条件下不同凋落物而言,玉米秸秆的N残留率最低,而杨树叶最高。总的来说,水分降低对干旱区农林复合系统内凋落物的分解和氮元素含量具有显著的抑制作用。     

荒漠草原中间锦鸡儿冠层截留特征

以荒漠草原人工中间锦鸡儿（Caragana intermedia）为研究对象,利用2016-2017年监测获取的26次降雨事件,对比分析了两组灌丛（自然组和人工组）的冠层截留特征。结果表明：（1）试验期间共观测到有效降雨33次,总降雨量为251 mm,次平均降雨量和降雨强度分别为7.6 mm和1.14 mm/h,以雨量<2 mm,雨强<1 mm/h和降雨历时2-5 h的降雨出现次数最多;（2）自然组和人工组中间锦鸡儿平均截留量分别为1.11 mm和0.72 mm,平均截留率分别为24.81%和15.95%,两组灌丛截留存在极显著差异（P < 0.01）;（3）在雨量级>15 mm时,自然组（4.57%,CV=73.38%）和人工组（5.25%,CV=51.96%）平均截留率变异性相差最大;（4）自然组和人工组截留量与降雨量,降雨历时和降雨强度之间的关系可以用幂函数描述,截留率与三者的关系均用指数函数描述较好。在降雨特征相同的情况下,灌丛形态特征是影响中间锦鸡儿冠层截留的关键因素。     

砾石对红壤工程堆积体边坡径流产沙的影响

为探究砾石对红壤工程堆积体边坡降雨侵蚀的影响,基于室内模拟降雨试验,在1.0、1.5、2.0、2.5 mm/min雨强条件下,以土质边坡为对照,研究了10%、20%和30%的砾石质量分数红壤工程堆积体边坡的径流特征、产沙过程及侵蚀动力机制。结果表明：1）砾石质量分数对稳定径流强度的影响存在阈值,在雨强 > 1.0 mm/min时稳定径流强度随砾石质量分数的增加先减小后增大,在1.0 mm/min雨强时则表现为先增大后减小,且均在10%砾石质量分数下达到极值;2）雨强1.0 mm/min时,径流为缓流,砾石促进径流流动,使弗汝德数增大24.5%-87.8%,雨强2.0、2.5 mm/min时,径流为急流,砾石延缓径流流动,使弗汝德数降低4.2%-13.0%;3）侵蚀速率随产流历时变化过程受砾石质量分数和雨强的影响,雨强越大,砾石质量分数越低,边坡越易发生细沟侵蚀且伴随重力崩塌现象,侵蚀速率呈多峰多谷变化趋势;4）1.0 mm/min雨强时,砾石存在加剧了土壤侵蚀,产沙增幅达28.7%-50.5%;雨强 > 1.0 mm/min时,砾石减沙效益为5.0%-64.4%;5）径流功率是描述红壤工程堆积体侵蚀动力机制最优参数,其可蚀性参数及发生侵蚀临界径流功率从大到小对应的砾石质量分数均为10%、0、20%和30%。研究成果可为红壤区开发建设项目水土流失治理及侵蚀预测模型提供科学依据。     

Hypolithic Cyanobacteria, Dry Limit of Photosynthesis, and Microbial Ecology in the Hyperarid Atacama Desert

The occurrence of hypolithic cyanobacteria colonizing translucent stones was quantified along the aridity gradient in the Atacama Desert in Chile, from less arid areas to the hyperarid core where photosynthetic life and thus primary production reach their limits. As mean rainfall declines from 21 to ≤2 mm year⁻¹, the abundance of hypolithic cyanobacteria drops from 28 to <0.1%, molecular diversity declines threefold, and organic carbon residence times increase by three orders of magnitude. Communities contained a single Chroococcidiopsis morphospecies with heterotrophic associates, yet molecular analysis revealed that each stone supported a number of unique 16S rRNA gene-defined genotypes. A fivefold increase in steady-state residence times for organic carbon within communities in the hyperarid core (3200 years turnover time) indicates a significant decline in biological carbon cycling. Six years of microclimate data suggest that the dry limit corresponds to ≤5 mm year⁻¹ rainfall and/or decadal periods of no rain, with <75 h year⁻¹ of liquid water available to cyanobacteria under light conditions suitable for photosynthesis. In the hyperarid core, hypolithic cyanobacteria are rare and exist in small spatially isolated islands amidst a microbially depauperate bare soil. These findings suggest that photosynthetic life is extremely unlikely on the present-day surface of Mars, but may have existed in the past. If so, such microhabitats would probably be widely dispersed, difficult to detect, and millimeters away from virtually lifeless surroundings.     

模拟降水对古尔班通古特沙漠生物结皮表观土壤碳通量的影响

水分是控制干旱区生态过程的重要环境因素,在水分受限制的生态系统中,降水通过改变土壤的干湿状态直接控制地下生物过程。生物结皮作为干旱区主要的地表覆盖物,能利用空气中有限的水分进行光合作用,其自身的碳交换是干旱区土壤碳通量的重要组成部分。通过模拟0(对照)、2、5 mm和15 mm 4个降水梯度,利用红外气体分析仪,对古尔班通古特沙漠中部生物结皮以及裸地表观土壤碳通量进行测量,探讨不同强度降水条件下生物结皮对表观土壤碳通量的影响,结果表明:(1)降水增加了生物结皮表观土壤碳释放量,2、5 mm和15 mm 3种降水处理累积碳释放量分别是对照的151.48%、274.97%、306.44%,并且随着降水后时间的延长,表观土壤碳通量逐渐减小直至达到降水前的水平;(2)生物结皮与裸地的表观土壤碳通量对降水的响应不同,对照和最大降水量下,生物结皮表观土壤碳通量大于裸地,但是2 mm和5 mm降水后,生物结皮表观土壤碳通量小于裸地,并且二者在2 mm降水时差异显著(P<0.05),而在其它降水处理下无显著差异;(3)连续两次降水事件,活性碳在初级降水后的大量释放使得二次降水后释放量下降,其中裸地碳释放量下降速率与降水强度正相关。本研究说明,在探求荒漠地区土壤碳交换对降水的响应规律时,应该考虑生物结皮的影响以及连续降水事件的差异。     

西藏紫花针茅叶功能性状沿降水梯度的变化

植物叶功能性状与环境因子的关系是近10年来植物生态学的研究热点。该文以广泛分布于青藏高原干旱、半干旱草地的优势植物种紫花针茅(Stipa purpurea)为研究对象, 沿降水梯度(69-479 mm)系统测定了日土、改则、珠峰、当雄和纳木错5个调查地点紫花针茅比叶面积(SLA)、单位重量和单位面积叶氮含量(N_mass, N_area)、叶密度和厚度等叶功能性状以及土壤全氮含量等因子, 试图验证干旱胁迫地区同一物种内SLA-N_mass关系沿降水梯度的策略位移现象是否具有普遍性, 并对是否出现策略位移现象提出可能的解释。研究结果表明: 1) SLA和N_mass与生长季温度和降水以及土壤全氮含量均没有显著关系, SLA与N_mass的关系在干旱半干旱区(年降水/蒸发比< 0.11)与半湿润区(年降水/蒸发比> 0.11)之间并没有出现典型的位移现象; 2)叶密度是决定半湿润区SLA变化的主导因子, 而叶厚度则是干旱半干旱区SLA变化的控制因子, 两者与SLA均呈负相关, 随着温度增加或降水减少, 叶厚度增加而叶密度降低, 导致SLA随温度和降水变化不明显; 3)半湿润区的叶密度增加引起N_area增加, 而干旱半干旱区的叶厚度增加并没有造成N_area的显著变化, 导致N_area沿降水梯度没有显著变化; 4)紫花针茅地上生物量与N_area具有显著正相关关系, 表明N_area的增加有助于提高植被生产力。结果表明, 在干旱胁迫下, 植物通过增加叶厚度来维持不变的N_area可能有助于保持与较湿润地区相似的光合生产和水分利用效率。叶厚度和叶密度对比叶面积的相对影响在干旱半干旱区与半湿润区之间发生转变, 这为进一步检测高寒草地植被的水分限制阈值提供了新思路。     

Rapid Development of Adaptive,Climate-Driven Clinal Variation in Seed Mass in the Invasive Annual Forb Echium plantagineum L.

We examined adaptive clinal variation in seed mass among populations of an invasive annual species, Echium plantagineum, in response to climatic selection. We collected seeds from 34 field populations from a 1,000 km long temperature and rainfall gradient across the species'' introduced range in south-eastern Australia. Seeds were germinated, grown to reproductive age under common glasshouse conditions, and progeny seeds were harvested and weighed. Analyses showed that seed mass was significantly related to climatic factors, with populations sourced from hotter, more arid sites producing heavier seeds than populations from cooler and wetter sites. Seed mass was not related to edaphic factors. We also found that seed mass was significantly related to both longitude and latitude with each degree of longitude west and latitude north increasing seed mass by around 2.5% and 4% on average. There was little evidence that within-population or between-population variation in seed mass varied in a systematic manner across the study region. Our findings provide compelling evidence for development of a strong cline in seed mass across the geographic range of a widespread and highly successful invasive annual forb. Since large seed mass is known to provide reproductive assurance for plants in arid environments, our results support the hypothesis that the fitness and range potential of invasive species can increase as a result of genetic divergence of populations along broad climatic gradients. In E. plantagineum population-level differentiation has occurred in 150 years or less, indicating that the adaptation process can be rapid.     

Low rainfall-induced shift in leaf trait relationship within species along a semi-arid sandy land transect in northern China

It is unclear whether the shift in leaf traits between species of high- and low-rainfall sites is caused by low rainfall or by species replacement, because leaf traits vary substantially among species and sites. Our objective was to test if the within-species relationship between specific leaf area (SLA) and leaf N concentration (N(mass) ) shifts across a rainfall gradient in the semi-arid sandy lands of northern China. Data for SLA and N(mass) of dominant species and related canopy and soil variables were collected from 33 plots along a rainfall transect (270-390 mm) having similar temperatures in the Mu Us, Inner Mongolia. We further investigated the generality of Mu Us data using 12 additional plots in the southeastern Qaidam Basin, Qinghai. Artemisia ordosica is a widespread species in both regions. Across and within species, the positive SLA-N(mass) relationship shifted between two plant groups in the lowest rainfall plots (270 mm) and other higher rainfall plots (320-390 mm), which was confirmed by additional data from Qinghai. For A. ordosica populations, leaf area index (LAI) decreased and N(mass) increased with decreasing rainfall, while the foliage N pool and SLA varied little. Rainfall was the limiting factor that determined variations in N(mass) and LAI. Accordingly, N(mass) /SLA ratios continually increased with decreasing LAI along the rainfall gradient (r = -0.76, P < 0.001). Results indicate a low rainfall-induced shift in the SLA-N(mass) relationship associated with changes in LAI and foliage N pool, suggesting a link between leaf characteristics and ecosystem function.     

The Effect of Water on Decomposition Dynamics in Mesic to Wet Hawaiian Montane Forests

I used a mesic to wet precipitation gradient on Maui, Hawaii, to test whether variation in rainfall regulates decomposition in tropical wet forest. Decomposition rates of leaves and roots from the dominant tree species, Metrosideros polymorpha, were measured at six sites similar in temperature regime, parent material, ecosystem age, vegetation, and topographical relief, whereas mean annual precipitation (MAP) at these six sites varied from 2200 to over 5000 mm/y. In situ decomposition rates of leaves placed on the soil surface declined by a factor of 6.4 with increased precipitation, whereas the decomposition rate of roots placed below ground declined by a factor of 2.3 across the gradient. Leaves collected from the 2200-mm site and placed at all sites on the gradient decomposed faster on the soil surface than they did below ground, whereas both above- and belowground decomposition rates of the common leaves decreased by a factor of 2.5 with increased precipitation. Of the environmental variables that changed with MAP, soil oxygen availability appeared to be the proximal factor that limited decomposition rates across the gradient, both above and below ground. When plant tissue collected from all sites across the gradient was decomposed at a common site, leaves from the wettest sites decomposed almost three times more slowly than leaves from the mesic sites. In contrast, roots from across the gradient all decomposed at a similar rate in a common site. Of tissue chemistry variables, high lignin concentration was correlated consistently with slow decomposition for roots and leaves. These results suggest that soil oxygen limitation combined with poorly decomposable leaves caused slower rates of decomposition and nutrient release with increased rainfall in these upland forests. Received 14 April 2000; Accepted 11 December 2000.     

Atmospheric water vapor as driver of litter decomposition in Mediterranean shrubland and grassland during rainless seasons

Litter production in many drought‐affected ecosystems coincides with the beginning of an extended season of no or limited rainfall. Because of lack of moisture litter decomposition during such periods has been largely ignored so far, despite potential importance for the overall decay process in such ecosystems. To determine drivers and extent of litter decay in rainless periods, a litterbag study was conducted in Mediterranean shrublands, dwarf shrublands and grasslands. Heterogeneous local and common straw litter was left to decompose in open and shaded patches of various field sites in two study regions. Fresh local litter lost 4–18% of its initial mass over about 4 months without rainfall, which amounted to 15–50% of total annual decomposition. Lab incubations and changes in chemical composition suggested that litter was degraded by microbial activity, enabled by absorption of water vapor from the atmosphere. High mean relative humidity of 85% was measured during 8–9 h of most nights, but the possibility of fog deposition or dew formation at the soil surface was excluded. Over 95% of the variation in mass loss and changes in litter nitrogen were explained by characteristics of water‐vapor uptake by litter. Photodegradation induced by the intense solar radiation was an additional mechanism of litter decomposition as indicated by lignin dynamics. Lignin loss from litter increased with exposure to ultraviolet radiation and with initial lignin concentration, together explaining 90%–97% of the variation in lignin mass change. Our results indicate that water vapor, solar radiation and litter quality controlled decomposition and changes in litter chemistry during rainless seasons. Many regions worldwide experience transient periods without rainfall, and more land area is expected to undergo reductions in rainfall as a consequence of climate change. Therefore, absorption of water vapor might play a role in decomposition and nutrient cycling in an increasing number of ecosystems.     

叶片毛尖对齿肋赤藓结皮凝结水形成及蒸发的影响

凝结水(隐匿降水)和降水是荒漠地区两种不同形式的水分来源,对荒漠生态系统极为重要。叶片毛尖(leaf hair points, LHPs)是很多荒漠藓类的重要外部形态结构特征,但它在藓类植物利用凝结水和降水中的作用尚不清楚。齿肋赤藓(Syntrichia caninervis)是古尔班通古特沙漠藓类结皮的优势种,其叶片顶端具有较长的白色毛尖。本文采用自制微渗计(h=3.5 cm, d=5.7 cm)研究了正常有毛尖和人工去除毛尖的齿肋赤藓结皮的凝结水特征及其在3种模拟降水梯度(1 mm, 3 mm, 6 mm)下的短期蒸发特征,结果表明：(1) 在凝结阶段,有毛尖结皮每时段的凝结水量均大于无毛尖结皮,但日出后有毛尖结皮凝结水下降速度稍快;有毛尖结皮的日凝结水量均大于无毛尖结皮,且前者的总凝结水量比后者多10.26%,即毛尖能增加10.26%的凝结水量。(2) 3种模拟降水梯度下,有毛尖结皮在各时段的累积蒸发率始终小于无毛尖结皮,以蒸发前期阶段最为明显,表明毛尖能显著减少和延缓结皮内的水分蒸发、延长植株水合时间,而且降水量越大减缓效果越明显。毛尖对这2种不同形式水分利用的差异是因为利用方式不同：对凝结水的利用主要归因于毛尖增大了结皮表面粗糙度,而减少对降水的蒸发主要是毛尖能反射阳光、形成内部毛细管及减小植株间隙的缘故。因此,毛尖的存在有利于齿肋赤藓结皮对凝结水和降水的利用,增强了藓类结皮对干旱环境的适应能力。     

Use of differential water sources by Prosopis flexuosa DC: a dendroecological study

In central-western Argentina, there is a pronounced water deficit gradient, from semiarid climate conditions with 500-mm rainfall/year to arid climate conditions with 80-mm rainfall/year. This climatic transition, governed by the rainfall gradient, occurs between the Arid Chaco and Monte phytogeographic regions and is evidenced by differences in vegetation type, structure, dynamics and tree growth. In turn, the availability of soil moisture, particularly access to the water table, modifies water use strategies by trees along this gradient. We analyzed how water availability, expressed as differences in accessibility to the water table, influences Prosopis flexuosa tree rings along a precipitation gradient. In this manner, we try to interpret the growth of species according to the use of differential water sources. P. flexuosa showed highly varying growth reactions (tree-ring width and hydraulic anatomic parameters) with climate, depending on the ecology of the site. Along the Arid Chaco-Monte gradient, the growth of P. flexuosa is more dependent on variations in rainfall in those areas where water depth is greater than root spread. The climate signal was hidden in those regions where the water table is accessible to the root system.     

黄土丘陵沟壑区黄土坡面侵蚀过程及其影响因素

降雨强度、坡长、坡度是影响坡面产流产沙的重要因素。为定量分析降雨强度、坡长、坡度对黄土丘陵沟壑区安塞黄土坡面侵蚀过程的影响,本研究基于室内人工模拟降雨试验,分析2个坡长(5、10 m)、3个坡度(5°、10°、15°)、2个降雨强度(60、90 mm·h^-1)下安塞黄土坡面产流产沙规律。结果表明: 初始产流时间随坡长增加呈减小趋势,但总体变化不大;初始产流时间随降雨强度增加而减小,与60 mm·h^-1相比,90 mm·h^-1下缩短5.7～18 min;10°坡度上的径流起始时间最快。随降雨历时延长,产流率先快速增加,最终逐渐稳定在某一产流率值上下波动;产沙率在产流初期短时间内突然升高,达到最大值后减小,再逐渐达到稳定。产流率和产沙率随坡长和降雨强度的增加而增加,但随坡度变化规律不明显。随着降雨强度、坡长和坡度的增加,总产沙量相应增加。在降雨强度90 mm·h^-1时,坡长和坡度分别为10 m和15°的坡面产生了细沟,导致总侵蚀量最大(11885.66 g)。降雨强度为60 mm·h^-1时,随着坡长增加单位面积侵蚀量减小,在5～10 m坡段存在临界侵蚀坡长。坡长、坡度和降雨强度对坡面径流过程均有促进作用,降雨强度、坡长和两者之间交互作用对产流率和总侵蚀量的贡献率较大,其中,对产流率贡献最大的影响因素是降雨强度,贡献率为49.8%;坡长对总侵蚀的贡献率最大,为37.8%。     

Life history variation in an annual plant under two opposing environmental constraints along an aridity gradient

Environmental gradients represent an ideal framework for studying adaptive variation in the life history of plant species. However, on very steep gradients, largely contrasting conditions at the two gradient ends often limit the distribution of the same species across the whole range of environmental conditions. Here, we study phenotypic variation in a winter annual crucifer Biscutella didyma persisting along a steep gradient of increasing rainfall in Israel. In particular, we explored whether the life history at the arid end of the gradient indicates adaptations to drought and unpredictable conditions, while adaptations to the highly competitive environment prevail at the mesic Mediterranean end. We examined several morphological and reproductive traits in four natural populations and in populations cultivated in standard common environment. Plants from arid environments were faster in phenological development, more branched in architecture and tended to maximize reproduction, while the Mediterranean plants invested mainly in vertical vegetative growth. Differences between cultivation and field in diaspore production were very large for arid populations as opposed to Mediterranean ones, indicating a larger potential to increase reproduction under favorable conditions. Our overall findings indicate two strongly opposing selective forces at the two extremes of the aridity gradient, which result in contrasting strategies within the studied annual plant species.