967 resultados para Canopy


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辐射传输研究是贯穿森林生态系统的纽带,太阳辐射为植物的生长发育提供光合能量、适宜的环境温度以及发育信息。一方面,气候变化使到达地面辐射能的质和量发生变化,影响到植被的生长发育,改变森林的结构,而森林结构的变化又会影响林冠内辐射能的分配和质量,这些变化会进一步影响到林下土壤温度,改变森林根系活性以及土壤营养转化的效率;连锁反应的结果有可能会使森林生态系统的生产力发生变化,改变碳素和氮素源库的调节方向,从而反馈影响地球气候系统。另一方面,人类作为生态系统的成员,必然需要森林生态系统为其提供更多的原材料和更好的生态服务功能,如何实现这些目标,就需要人类适度调整干预方式和频度,达到预期的目的。本文在建立适合于川西亚高山森林的叶面积测量技术、光照辐射模型和土壤温度变化模型的基础上,对川西亚高山地带森林生态系统的辐射传输特征进行了分析,并从森林结构的角度探讨了林分内的辐射分布以及对土壤温度的影响。主要成果如下: 1. 提出了一种照相法测量叶面积的方法。通过对摆放在平面上的叶片照相,利用投影变化,把非正射图像转化为正射图像,然后经过计算机图像处理得到每一片叶片的面积、周长、长度、宽度等信息。这种方法可使用户以任意方向和距离拍摄处于平面上的叶片,能同时处理大量的叶片,适于野外离体或活体叶片测量。叶片面积分辨率可调,分辨率可以与常用的激光叶面积仪相近甚至更高,而且叶片图像可以存档查询。 2. 提出一种模拟林内光照变化的模型。利用林冠半球照片,记录视点以上半球内的林冠构件空间分布,作为林冠子模型;天空辐射子模型采用国际照明委员会(CIE)的标准晴天和阴天以及插值模型。该模型能够模拟林下某一位点处的实时光斑变化。 3. 提出一种土壤温度变化模型。把土壤视为具有容量和阻力性质的结构,利用电阻和电容器件构建土壤能量分布模型。外界太阳辐射能经过植被以及其它一些能量分配器后进入土壤,其中有一部分转化为土壤势能,即土壤温度。土壤温度的变化类似于电池的充放电过程。在已知模型参数的情况下,可以从太阳辐射计算土壤温度的变化。在模型参数未知的情况下,通过输入和输出值推算模型的参数,而模型参数中的时间常数与土壤组成和含水量有关,这样就可以知道土壤水分的变化情况。 4. 从王朗亚高山森林典型样地林分结构的测量获得林地三维结构图、树冠形态、叶面积密度等参数,这些参数输入到Brunner (1998)开发的tRAYci 模型中计算出一段时间内林分任意位置处的光照值。与林下辐射计测量值以及半球照片计算结果的比较,该模型基本上能够满足对林分光环境了解的要求。 5. 从川西亚高山森林生产力的角度,探讨了森林生产力研究的方法以及川西地区的研究历史和成果,发现了其中的一些规律和问题,特别是在叶面积测量上,还没有使用标准的叶面积指数定义。综合来看,川西地区针叶林叶面积指数(单位土地面积上植物冠层总叶面积的一半) 应在4-5 之间。降雨丰富的华西雨屏带是川西地区森林生产力最高的地区,而向西北森林生产力逐渐降低。川西地区云冷杉林森林生产力平均约为600 gDM m-2 a-1,但是根据辐射能计算的潜在生产力则达到1800 gDM m-2 a-1。实际与潜在森林生产力的巨大差异说明其它因子对生产力的影响。 6. 王朗亚高山3 个典型森林林分中,白桦林样地(BF) 林下草本以糙野青茅、牛至、紫菀等喜阳性物种为主,林下透光度较高;冷杉林样地(FF) 林下透光度最低,以喜阴性物种水金凤、蟹甲草、囊瓣芹等为主;而云杉林样地(SF)林分林龄最大,林下透光度介于冷杉林和白桦林之间,草本层仍然以喜阴性物种东方草莓、紫花碎米芥、酢浆草等为主。冷杉林和云杉林的灌木层也很丰富,卫矛属、五加属、茶藨子属、忍冬属植物很丰富,而在白桦林则以栒摘要子属、榛子属、鹅耳枥属等植物为主。藓类植物在云杉林中最丰富,并且形成毯状层,其它两个林分则很稀少。3 个样地林分结构与林下光环境有很强的相关性,从光环境特征可以在一定程度上推测林分的结构。各样地单纯从乔木层材积推算的NPP 排列顺序为BF>FF>SF,与林下辐射透射率和林分年龄的顺序相同,暗示辐射对群落演替过程的驱动作用。 7. 用半球照相法测得BF、FF 和SF 3 个样地的有效叶面积指数以SF 样地最高,BF 最低。如果考虑针叶树叶片在小枝上的丛聚分布,利用北方针叶林的数值进行校正,则SF 样地LAI 显著增加(达到89%),其它样地的LAI 基本不变甚至有所下降。校正后的数值与文献中地面测量的结果较相近,说明在使用半球照相法测量川西亚高山针叶林LAI 时必须加以校正。 8. 在3 个样地中,白桦、岷江冷杉和方枝柏种群为丛聚分布,紫果云杉在FF和SF 样地中基本上为随机分布。3 个物种出现丛聚分布的最短距离约为2m,在最短距离以内则为随机分布。最短距离可能与树冠大小有关,种子传播特征以及对光照的需求状况可能是造成这种分布格局类型的原因。 Radiative transfer plays a key role in forest ecosystems. Solar radiation providesenergy for photosynthesis, appropriate ambient temperature and development informationfor plants. However, quality and quantity of radiation reaching land surface are affected byweather and subsequently influence the growth and development of plants, which in turnchanges the budget of radiation in forest. Soil temperature changes with the variation ofradiation under forest canopy and influences the activity of roots and rate of nutrientturnover. Thus, any changes of radiation will induce chain reactions in the entireecosystem and display in the value of net primary productivity which will possibly shiftthe relationship between carbon source and sink at local or regional scale and feed back tothe global climate system. On the other hand, as a component of ecosystems, humanbeings of course need to demand more materials and better service from ecosystems. Forthese purpose, man must adapt their pattern and frequency of interference to ecosystems.This paper aims to research on the canopy structure, the radiation distribution and theirinfluence on soil temperature from the process of radiative transfer in subalpine forestecosystem of western Sichuan. The main results are: 1 Present a new photogrammetric method for leaf area. The main idea is to convertnon-vertically taken images of planar leaves to orthoimages through projectivetransformation. The resultant images are used to get leaf morphological parametersthrough image processing. This method enables users to take photos at almost anyorientation and distance if only the leaves are placed on same plane, and to processlarge quantity of leaves in a short time, which is suitable for field measurement. Theresolution of leaf area is adjustable to fit for special requirement. 2 A model using hemispherical photos combining with solar tracks and radiation courseis provided to simulate light variation in forest. The hemispherical photos of canopyrecord the real spatial distribution of each element of plants viewed from a point. Skyradiance is simulated with CIE standard clear sky or cloudy sky model. This modelcan be used to simulate real time light variation under canopy. 3 Present a soil temperature model. Soil could be regarded as a body of resistor andcapacitor. Some of the budget of solar radiation in soil body is transformed into soilpotential energy, the soil temperature. Variation of soil temperature is driven by solarradiation, vegetation, soil properties, etc. This model has two parameters, one of whichis time constant and is related to soil water content. The inversed model can be used tosimulate the variation of soil water. 4 By using model tRAYci developed by Brunner (1998), the 3-D distribution of light inthree subalpine forest stands of Wanglang Nature Reserve has been simulated andvalidated with value of radiometers in these stands. This model can basically satisfythe need for understanding light regimes of these stands. 5 Present some principles and questions of NPP (net primary of productivity) researchesin western Sichuan. The standard leaf area index (LAI) defined by Chen and Black(1997) has not been used in this region. Total leaf area and projected leaf area indexare still used in NPP researches which may differ around 1-fold in magnitude. Thestandard LAI which is a half of total leaf area above unit land area should be between4 and 5 for typical subalpine coniferous forest of western Sichuan concluded fromliteratures. The maximum forest NPP occurs in West China rain belt and decreasesnorthwestwards. Average NPP of spruce-fir forest in western Sichuan is about600gDM m-2 a-1, which is below the potential NPP of 1800gDM m-2 a-1 based onmeasured radiation in this region. The significant difference between potential and realNPP suggests that other factors influence the growth of stands. 6 In the three subalpine forest stands of Wanglang Nature Reserve, herbage layer ofAbstractbirch stand (BF) with age of 40 is dominated by heliophytes of Deyeuxia scabrescens,Origanum vulgare, Aster tongoloa etc.. However, both of the other two stands aredominated by shade tolerent species, such as Impatiens noli-tangere, Impatiensdicentra, Cacalia deltophylla and Pternopetalum tanakae etc. in fir stand (FF) withage of 180 and Fragaria orientalis, Cardamine tangutorum and Oxalis corniculata etc.in spruce stand (SF) with age of 330. Shrub species in the latter two stands arerelatively rich, typical dominant genera being Euonymus, Acanthopanax, Ribes andLonicera. Birch stand has relatively sparse shrubs dominated by genera of Cotoneaster,Corylus and Carpinus. Mosses are significant only in spruce stand. The canopystructure controls the light regime of stand, which influence the composition of herblayers beneath the canopy. This light regime-community structure relationship can beused to infer the herb community from canopy structure. The NPP derived from timbervolume of arbor layer of the three stands decreases from BF to SF, which is in thesame order of transmitted total radiation under canopy and age of these stands,suggesting the driving effect of radiation in the succession of community. 7 The highest effective LAI of the three stands obtained by hemispherical photos is inplot SF and lowest in plot BF. After rectification of the clumping effect of leaves onshoot, the real LAI in plot SF increases significantly (89%) and approximate to theaverage LAI of coniferous forest in western Sichuan. Therefore, the LAI obtainedfrom hemispherical photos needs rectification for clumping effect. 8 Spatial distribution pattern for Betula platyphylla, Abies faxoniana and Sabinasaltuaria is clumpy, but Picea purpurea almost random in plot FF and SF. The shortestdistance for clumpy distribution for Betula platyphylla and Sabina saltuaria is 1.5m,and 2m for Abies faxoniana. And random pattern for these trees is exhibited within thisrange which almost coincides with the diameter of crown. Seed dispersalcharacteristics and light requirement may be the reason for different spatial pattern.

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The relationships of eight moss species of Dicranum in 31 sites in main ecological systems in the Changbai Mountain with environmental factors were studied by canonical correspondence analysis (CCA). The results showed that altitude, soil sand percentage, water percentage, acidity and canopy density were important environmental factors influencing the distribution of the species of Dicranum . The relationships between Dicranum elongatum Schleich. ex Schwaegr ., D.groenlandicum Brid. and altitude,between D.japonicum Mitt., D.scoparium Hedw. and canopy density,between D.polysetum Sw., D. undulatum Schrad. ex Brid. and soil acidity and water percentage,were positively correlative. The niche overlaps among the eight species of Dicranum were calculated. The minimal spanning tree of the eight species on the two-dimensional scatter plot were also drawn based on their niche overlaps, which clearly revealed the ecological similarities of eight species.

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植物冠层在养分循环及改变养分流量方面的作用,是当前国内、外研究的重点和热点课题。本文在综合评述前人研究的基础上,对植物冠层氮素淋失及其影响因素进行了分析,指出现有研究中存在的不足,提出了下一步应重点研究的问题:(1)进一步完善测定方法,开展对农田植物冠层氮素淋失的研究;(2)如果确定农田植物存在冠层氮素淋洗,需明确冠层氮素淋洗形态,并与不同氮效率基因型联系起来进行研究;(3)开展揭示植物冠层氮素淋失途径与过程的机理研究,特别是应该将不同生育期叶面积、气孔密度、气孔导度、叶片自由空间和自由空间中可溶性氮素等可能影响冠层氮素淋洗的指标与冠层氮素淋洗相联系进行研究,有利于揭示冠层氮素淋失机理,对冠层氮素淋失赋予理论支持。

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试验研究了冬小麦在不同土壤水分条件下拔节~抽穗期冠层温度-气温差变化规律及其随作物生长发育期的变化状况。结果表明,作物在充分供水条件下冠层温度-气温差变化较平缓;缺水时变化较大。冠层温度-气温差随作物生长发育期的变化趋势为低水分处理高于高水分处理。冠层温度-气温差可较合理反映土壤水分变化状况和作物水分亏缺程度。

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黄土高原半干旱区土壤蒸发强烈,准确地掌握土壤水分动态对于旱地农业水分管理至关重要。应用基于物理基础的一维水热耦合SHAW(The Simultaneous Heat and Water)模型,模拟了陕西子洲岔巴沟流域1964~1967年土壤水分和土壤蒸发的动态特征,以及神木六道沟流域2006年坡地和梯田土壤水分变化。结果表明,除表层土壤水分模拟结果偏差较大,其他土层模拟值与实测值基本吻合,模拟期土壤水分模拟的相对平均绝对误差(Relatively Mean Absolutely Error,RMAE)为5.2%~11.4%。1964~1967年土壤累积蒸发量模拟值与实测值平均相对偏差为0.8%~6.1%,土壤蒸发的模拟值与实测值较为一致。因此,SHAW模型可以用于黄土高原半干旱区农田土壤水分动态规律研究。

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以3种不同株型夏玉米为供试材料,采用盆栽试验研究了不同生育期及冠层不同叶位叶片表观自由空间的大小差异和变化规律。结果表明,在相同施肥水平下,随生育期推进,各株型夏玉米叶片表观自由空间逐渐降低;不同玉米品种冠层叶片表观自由空间在全生育期内存在极显著差异(P<0.01)。从不同株型品种叶片表观自由空间看,以紧密型品种陕单902叶片表观自由空间最大,中间型品种农大108与平展型品种陕单9号间较小,二者差异不显著;平展型品种各生育时期间叶片表观自由空间的差异较小,而紧密型品种的差异最大。全生育期内不同株型品种不同叶位间叶片表观自由空间存在明显差异,但缺乏普遍规律性;比较不同生育期内不同叶位,以拔节期不同叶位间差异较大;比较同株型品种不同叶位,以中间型品种农大108不同叶位间差异较大。以上结果说明了在研究和评价植物叶片表观自由空间时,不仅要考虑植物遗传特征,而且还需考虑植物生育期及叶位。

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在遮雨棚控水条件下,采用盆栽的方式研究了不同秸秆覆盖量对玉米根、冠生长的影响。试验按对照(CK)和秸秆覆盖量0.3 kg/m2(SM0.3)、0.6 kg/m2(SM0.6)、0.9 kg/m2(SM0.9)、1.2 kg/m2(SM1.2)共设5个处理,水分按高水(占田间持水量的90%)和低水(占田间持水量的60%)设两个水平。分别测定了玉米根、茎、叶、穗干重,根系垂直空间分布及叶片叶绿素相对含量等指标。结果表明:秸秆覆盖明显改变了玉米根系和地上部分的生长;高水条件下SM0.6处理玉米根系、茎秆、叶和穗干重均高于其它处理;低水条件下,地上部分干重SM1.2最大,SM0.6次之;根系的垂直空间分布与水分和覆盖条件都有密切的关系,覆盖措施主要影响下层根系的生长和发育。

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通过喷灌玉米田间试验,研究了喷灌水经玉米冠层再分配后的分布状况。结果表明:在玉米全生育期,茎秆下流水量占灌水量的均值为44%左右,棵间穿透水量占灌水量的均值为48%左右,冠层截留量在0.8 ̄2.9mm之间变化。一次灌水中,喷灌水在地表的分布很不均匀,43.2%的灌水量经茎秆下流到根区,在距离茎秆7cm,15cm,25cm和32.5cm处,地表接收的水量占总灌水量的比例分别为18.9%、43.5%、66.9%和84.5%。灌水量、种植密度、株高和叶面积指数等都影响着喷灌水在地表的分布。

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研究表明 ,5~ 7年生沙棘林冠层可截留降水 8 5%~ 4 9 0 % ,并降低雨滴动能 ;枯枝落叶层重5 4 6t·hm- 2 ,其最大持水量可达 15 31t·hm- 2 ,有 1cm厚枯枝落叶层覆盖地表 ,即可基本控制水土流失 ;根系可以提高土壤的抗冲性和抗蚀性 ,与无根系土壤相比 ,可减少土壤冲刷量 55%~ 88% .据1988~ 1994年雨季径流小区测定 ,沙棘林在栽植后 4~ 5年可充分发挥水土保持作用 ,与农地相比 ,可减少地表径流量 87 1% ,减少土壤流失量 99 0 % .此外 ,它还可以每 4~ 5年提供薪材 10~ 30t·hm- 2 ,提高土壤中有机质和氮素含量 115%和 90 % ,生产沙棘果实 50 0kg·hm- 2 .所有这些表明了沙棘在治理黄土高原水土流失和改善人民生活条件 ,在实现由“恶性循环”向“良性循环”转变等方面 ,具有十分重要的作用 .目前 ,黄土地区已建立起若干利用沙棘固坡、防洪、解决燃料短缺和综合治理小流域的成功典型

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作物蒸腾量的计算是水资源开发利用和农业生产运筹的关键参数之一 .本文以彭曼 -蒙特斯方程为基础 ,通过引入临界阻力 ,根据实测资料建立冠层阻力和空气动力学阻力比值与临界阻力和空气动力学阻力比值二者之间的函数关系 ,得到一个只需气象参数就能计算作物蒸腾量的简单方法 .文章对该方法进行了理论分析 ,并用实例给予验证 .结果表明 ,该方法在理论上和实践上都是可行的 ,是一个值得研究和发展的新方法 .作物蒸腾量的日变化表明 ,炎热夏季晴天中午遮光处理后作物蒸腾量的增大是可能的

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在黄土高原南部半湿润易旱区土垫旱耕人为土上进行大田试验,研究氮肥、品种和栽培模式对冬小麦叶面积指数(LAI)和透光率(DIFN)及产量的影响。结果表明,小麦生长过程中LAI先增大后减小,在开花期最大,成熟期最小,施氮能够显著增加LAI;DIFN的变化规律与LAI相反。不同品种间LAI和DIFN差异显著。全程覆膜和覆膜150 d的LAI极显著大于常规栽培、集雨面栽培和三密一稀栽培模式,DIFN与此相反;施氮后籽粒产量极显著增加。在不同栽培模式下,以全程覆膜、覆膜150 d和集雨面栽培模式的产量较高,但从维持土壤质量角度考虑,则覆膜150 d和集雨面2种栽培模式优于其它几种栽培模式;从冠层结构特征分析,这2种栽培模式更有利于增加群体光合能力。

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Reducing uncertainties in the estimation of land surface evapotranspiration (ET) from remote-sensing data is essential to better understand earth-atmosphere interactions. This paper demonstrates the applicability of temperature-vegetation index triangle (T-s-VI) method in estimating regional ET and evaporative fraction (EF, defined as the ratio of latent heat flux to surface available energy) from MODIS/Terra and MODIS/Aqua products in a semiarid region. We have compared the satellite-based estimates of ET and EF with eddy covariance measurements made over 4 years at two semiarid grassland sites: Audubon Ranch (AR) and Kendall Grassland (KG). The lack of closure in the eddy covariance measured surface energy components is shown to be more serious at MODIS/Aqua overpass time than that at MODIS/Terra overpass time for both AR and KG sites. The T-s-VI-derived EF could reproduce in situ EF reasonably well with BIAS and root-mean-square difference (RMSD) of less than 0.07 and 0.13, respectively. Surface net radiation has been shown to be systematically overestimated by as large as about 60 W/m(2). Satisfactory validation results of the T-s-VI-derived sensible and latent heat fluxes have been obtained with RMSD within 54 W/m(2). The simplicity and yet easy use of the T-s-VI triangle method show a great potential in estimating regional ET with highly acceptable accuracy that is of critical significance in better understanding water and energy budgets on the Earth. Nevertheless, more validation work should be carried out over various climatic regions and under other different land use/land cover conditions in the future.

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For maximizing the effective applications of remote sensing in crop recognition, crop performance assessment and canopy variables estimation at large areas, it is essential to fully understand the spectral response of canopy to crop development and varying growing conditions. In this paper, the spectral properties of winter wheat canopy under different growth stages and different agronomic conditions were investigated at the field level based on reflectance measurements. It was proved that crop growth and development, nitrogen fertilization rates, nutrient deficit (e.g. lacking any kind of nitrogen, phosphorus and kalium fertilizer or lacking all of them), irrigation frequency and plant density had direct influence on canopy reflectance in 400-900 nm which including the visible/near infrared bands, and resulted in great changes of spectral curves. It was suggested that spectral reflectance of crop canopy can well reflect the growth and development of crop and the impacts from various factors, and was feasible to provide vital information for crop monitoring and assessment. ©2010 IEEE.

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The remote sensing based Production Efficiency Models (PEMs), springs from the concept of "Light Use Efficiency" and has been applied more and more in estimating terrestrial Net Primary Productivity (NPP) regionally and globally. However, global NPP estimates vary greatly among different models in different data sources and handling methods. Because direct observation or measurement of NPP is unavailable at global scale, the precision and reliability of the models cannot be guaranteed. Though, there are ways to improve the accuracy of the models from input parameters. In this study, five remote sensing based PEMs have been compared: CASA, GLO-PEM, TURC, SDBM and VPM. We divided input parameters into three categories, and analyzed the uncertainty of (1) vegetation distribution, (2) fraction of photosynthetically active radiation absorbed by the canopy (fPAR) and (3) light use efficiency (e). Ground measurements of Hulunbeier typical grassland and meteorology measurements were introduced for accuracy evaluation. Results show that a real-time, more accurate vegetation distribution could significantly affect the accuracy of the models, since it's applied directly or indirectly in all models and affects other parameters simultaneously. Higher spatial and spectral resolution remote sensing data may reduce uncertainty of fPAR up to 51.3%, which is essential to improve model accuracy.