闽江河口湿地土壤全磷高光谱遥感估算

磷是湿地生态系统必需和限制性元素,利用高光谱遥感数据对其进行估算对实现湿地土壤磷素快速和准确定量具有重要意义。选取闽江河口湿地作为研究区,于2013年5月,采集16个土壤剖面80个样本作为估算与验证模型样本;基于光谱指数建立土壤全磷(TP)含量估算模型,其中光谱指数包括原始光谱反射率(R)、比值土壤指数(RSI)、归一化土壤指数(NDSI)和有机质诊断指数(OII)。此外进一步分析反射光谱与不同形态磷,TP与有机质之间关系,以期初步揭示河口湿地土壤TP估算的机理。研究结果表明,闽江河口湿地土壤TP含量与R相关系数较高的区域分布在360-560 nm,并在406 nm处达到最大值-0.816;光谱指数RSI(R_(430),R_(830))、RSI(R_(460),R_(810))、RSI(R_(560),R_(580))、NDSI(R_(430),R_(830))、NDSI(R_(460),R_(830))、NDSI(R_(560),R_(580))和OII(R_(446))与土壤TP含量均有较高的相关系数,能较好的用于TP含量的估算;各估算模型决定系数(r~2)和均方根误差(RMSE)分别在0.657-0.805和0.052-0.067之间;验证模型r~2和RMSE分别在0.606-0.893和0.037-0.044之间。分潮滩建立TP含量估算模型是可行的,并且能提高部分光谱指数的估算精度。土壤TP含量的估算精度与磷素的组成有关,其中与铁吸附态磷关系较为密切,钙吸附态和铝吸附态磷关系较弱。土壤TP与有机质和氧化还原环境的存在密切关系可能是湿地土壤TP含量估算的重要机理。     

冠层水平互花米草叶片光合色素含量的高光谱遥感估算模型

以闽江河口鳝鱼滩湿地互花米草(Spartina alterniflora)的实测冠层高光谱反射率和叶片光合色素含量(LPPC)为数据源,在分析LPPC与原始光谱反射率、一阶导数光谱反射率、22种已报道光谱指数和14种新构建的植被指数相关性的基础上,利用直线回归、指数回归、对数回归以及乘幂回归方法,系统地比较了36种植被指数在估算互花米草LPPC中的表现。研究表明:(1)一阶导数光谱反射率组合的植被指数用于估算互花米草的LPPC优于原始光谱反射率;(2)红边区域一阶导数光谱是估测互花米草LPPC的最佳波段;(3)对于单一色素含量的估算,叶绿素a(Chla)的最佳估算指数为FDNDVI[723,703];叶绿素b(Chlb)的最佳估算指数为FDRVI[723,525];类胡萝卜素(Cars)的最佳估算指数为FDNDVI[723,703];(4)对于使用统一参量同时估算Chla、Chlb、Cars,由FDRVI[723,703]建立的对数估算模型效果最佳。研究成果可为湿地植物生化参量反演提供参考,也可为闽江河口湿地入侵种互花米草的动态监测和生态评估管理提供有力的科学依据。     

闽江河口湿地土壤速效磷时空分布与来源

选取闽江河口潮滩湿地作为研究区,于2013年5、8和11月沿水文梯度采集不同深度土壤,测定其速效磷含量,研究闽江河口潮滩湿地土壤速效磷沿水文梯度的时空分布特征;并进一步测定土壤全磷(TP)、有机磷(Org-P)和无机磷(IP)分级,利用通径分析揭示土壤速效磷来源。结果表明:5月和8月土壤平均速效磷含量分别为3.53±1.15和3.23±1.15 mg·kg-1,显著高于11月(1.96±1.07 mg·kg-1)(P0.05);5、8和11月土壤速效磷空间分布格局相似,从高潮滩到中潮滩,其含量呈波动降低,并且表现为芦苇群落土壤速效磷含量显著高于短叶茳芏群落(P0.05);在垂直方向上,高潮滩土壤速效磷含量大都随深度增加而降低,中潮滩其垂直变化不显著;在植物生长初期(5月),土壤Org-P和闭蓄态磷(O-P)是速效磷的主要来源;在植物生长旺盛期(8月)和生长末期(11月),土壤Org-P和铁磷(Fe-P)是速效磷的主要来源。     

秋茄类胡萝卜素含量高光谱反演

类胡萝卜素(Car)作为植物主要色素,对诊断植被生理状态有重要作用。于2013年4月和7月采集闽江口秋茄(Kandelia candel)叶片,室内测定其叶片正面和背面反射光谱,同时测定其Car含量\[单位面积(μg·cm-2)和单位质量(mg·g-1)\]。选取常见Car含量估算的光谱参数,同时分析确定最佳比值植被指数(SR),基于回归分析,建立秋茄叶片Car含量估算与验证模型。结果表明,叶片光谱反射率表现为叶片背面大于正面(350~2350 nm);基于叶面背面光谱计算的SR与叶片Car含量(μg·cm-2)的相关系数优于其他组合,相关系数较高的区域分布在520~540 nm与1000~1100 nm波段组合,700~720 nm与800~1100 nm波段组合;基于背面光谱计算的大部分光谱参数与Car含量(μg·cm-2)的相关系数要高于基于正面光谱计算的。因此,以叶片背面光谱作为Car含量估算的光谱数据,以单位面积Car含量为估算量纲建立反演模型。本研究表明,光谱指数LCI、DD、NDVI(770,713)、NDVI(773,562)、SR(723,770)和SR(1000,700)均可实现Car含量的反演,估算与检验模型的R2均0.65,RMSE均1.52;并且新构建的SR(1000,700)估算精度最好,模型和检验R2分别为0.77和0.87,模型和检验RMSE分别为1.08和1.11。这些预味着基于高光谱遥感对闽江河口湿地秋茄Car含量进行估算是可行的。     

闽江河口湿地植物与土壤灰分及其影响因子分析

以闽江河口鳝鱼滩湿地生长的芦苇(Phragmitesaustralis)和互花米草(Spartina alterniflora)为研究对象,并对相应的36个土壤剖面进行取样分析,揭示它们的(厂火)分含量分布特征,并对其影响因子进行分析。研究结果表明:闽江河口鳝鱼滩湿地芦苇和互花米草各个器官(厂火)分含量的差异性明显,芦苇各部位(厂火)分含量的平均值大于互花米草;芦苇和互花米草湿地土壤(厂火)分含量的垂直分布较为类似,芦苇湿地土壤(厂火)分合量略高于互花米草湿地土壤(厂火)分含量,但两种植物土壤(厂火)分含量的差异并不显著;芦苇和互花米草湿地土壤(厂火)分含量与土壤有机碳有极其显著的负相关关系,与土壤含水量的相关性也较明显;从单一的植物类型来看,互花米草湿地土壤(厂火)分含量与容重、碳含量、含水量和盐度呈显著的相关关系,芦苇湿地土壤(厂火)分含量与土壤pH值有明显的正相关关系。     

滨海盐土土壤水分的高光谱参数及估测模型

基于滨海盐土5个试验点的土壤含水量和室内土壤表面高光谱反射率,综合分析了350~2500 nm波段范围内土壤含水量与土壤光谱之间的关系,并基于比值光谱指数(RSI)、归一化光谱指数(NDSI)和差值光谱指数(DI)确定了光谱参数,进而构建土壤含水量估测定量模型.结果表明:滨海盐土原始光谱反射率与土壤含水量呈显著负相关关系,且最大负相关出现在1930 nm(r=0.86)附近.对RSI、NDSI和DI的直线回归方程、幂函数回归方程进行对比,以RSI(R_(1407),R_(1459))为自变量构建的土壤含水量指数函数线性回归方程决定系数最大(0.780),标准误较小(0.016),拟合方程为y=0.00001e~(9.72053 x).估测模型能够更好地监测滨海盐土土壤水分状况.基于RSI(R_(1407),R_(1459))构建的模型可实现对江苏省滨海盐土土壤水分的精确监测.     

闽江口典型芦苇湿地与短叶茳芏湿地土壤碳氮含量的空间分布特征

以闽江河口鳝鱼滩湿地的芦苇湿地、短叶茳芏湿地以及二者交错带湿地为对象,研究了不同类型湿地土壤碳氮含量的空间分布特征。结果表明:土壤总氮(TN)和有机碳(SOC)含量在水平方向上整体表现为交错带湿地芦苇湿地短叶茳芏湿地,而在垂直方向上其在不同类型湿地土壤中的含量均随深度增加而降低;与芦苇湿地和短叶茳芏湿地相比,交错带湿地表层土壤的无机氮含量分别降低了15.78%、0.84%(NH4+-N)和13.04%、44.00%(NO3--N),而在下层土壤分别增加了30.00%、6.06%(NH4+-N)和43.75%、23.91%(NO3--N);芦苇湿地土壤NH4+-N含量主要受到有机质含量控制,短叶茳芏湿地土壤TN含量受到土壤盐分的重要影响,而土壤颗粒组成和水分是影响交错带湿地土壤的NH4+-N和NO3--N关键因子。研究发现,芦苇与短叶茳芏种群的竞争作用不但明显增加了交错带湿地土壤SOC和TN含量,而且也深刻改变了NH4+-N和NO3--N含量的空间分布特征,其可能通过改变土壤的细颗粒组成、氮矿化与硝化作用来影响土壤碳氮的空间分布。     

一种估测土壤有机质含量的近红外光谱参数

通过系统分析我国中、东部地区5种不同类型土壤风干样本的有机质含量与近红外(1000～2500 nm)光谱反射率和一阶导数两波段构成的比值、差值及归一化指数之间的关系,构建了适合土壤有机质含量估测的光谱参数及定量反演模型.结果表明：用多元散射校正及Savitzky-Golay平滑方法对原始光谱反射率进行预处理后,其两波段组成的光谱参数与土壤有机质含量的相关性明显优于原始光谱反射率组成的光谱参数,而由上述预处理后的反射率一阶导数的两波段构成的光谱参数介于二者之间;不同类型光谱参数构成形式中,以差值指数的预测性最好,其次为比值和归一化指数;与土壤有机质含量相关程度最高的光谱参数,是以近红外合频区1883和2065 nm 2个波段的反射率经多元散射校正和Savitzky-Golay平滑后构建而成的差值指数DI(CR₁₈₈₃, CR₂₀₆₅),两者呈极显著的直线相关.经不同类型土壤的观测资料检验,模型的决定系数为0.837,均方根误差为4.06;与偏最小二乘法的全谱建模结果相比,尽管DI(CR₁₈₈₃, CR₂₀₆₅)的预测精度略低于后者,但该指数只使用了2个波段的反射率,且所建模型比较简单,能为便携式监测仪的研制提供更有效的信息,可作为一种良好的土壤有机质估测光谱参数.     

滨海盐土土壤水分的高光谱参数及估测模型

基于滨海盐土5个试验点的土壤含水量和室内土壤表面高光谱反射率,综合分析了350～2500 nm波段范围内土壤含水量与土壤光谱之间的关系,并基于比值光谱指数(RSI)、归一化光谱指数(NDSI)和差值光谱指数(DI)确定了光谱参数,进而构建土壤含水量估测定量模型.结果表明： 滨海盐土原始光谱反射率与土壤含水量呈显著负相关关系,且最大负相关出现在1930 nm(r=0.86)附近.对RSI、NDSI和DI的直线回归方程、幂函数回归方程进行对比,以RSI(R₁₄₀₇,R₁₄₅₉)为自变量构建的土壤含水量指数函数线性回归方程决定系数最大(0.780),标准误较小(0.016),拟合方程为y=0.00001e^9.72053x.估测模型能够更好地监测滨海盐土土壤水分状况.基于RSI(R₁₄₀₇,R₁₄₅₉)构建的模型可实现对江苏省滨海盐土土壤水分的精确监测.     

互花米草入侵影响下闽江河口湿地土壤有效硅的时空变化特征

2016年1—12月,选择闽江河口鳝鱼滩的短叶茳芏湿地、互花米草湿地以及二者的交错带湿地为研究对象,采用定位研究方法探讨了互花米草入侵影响下湿地土壤有效硅含量的时空变化特征。结果表明:互花米草入侵影响下3块湿地土壤有效硅含量随时间推移整体呈波动上升趋势;互花米草入侵显著提高了鳝鱼滩湿地30—60 cm土层土壤有效硅含量(P0.01),与短叶茳芏湿地相比,交错带湿地和互花米草湿地30—60 cm土层土壤有效硅含量分别增加了8.56%和19.97%,逐步线性回归分析表明土温和电导是影响其变化的重要因素(P0.01)。研究互花米草入侵影响下湿地土壤有效硅含量的变化特征,对于揭示湿地生态系统生源要素硅生物地球化学循环过程以及互花米草入侵及其扩张机制具有重要意义。     

流域水碳过程耦合模拟——WaSSI-C模型的率定与检验

在复杂的气候变化条件下, 利用水碳耦合模型进行生态水文学研究成为主要的研究手段和途径。该文以杂谷脑河上游流域为例, 在确定生态水文模型WaSSI-C模拟尺度的基础上, 探讨水碳耦合模型在中国西南湿润地区的适用性。杂古脑河上游流域位于岷江上游, 隶属于长江流域。在分析和讨论了模型结构和机理的基础上, 分别对模型蒸散和融雪计算进行了补充改进, 以提高模型的适用性。将1988-1996年作为模型的率定期, 1997-2006年作为模型的验证期, 分别在率定期和验证期利用实测的径流数据和中分辨率成像光谱仪数据的总初级生产力、蒸散(ET)数据, 对模拟结果进行对比验证。并利用决定系数(R²)和Nash-Sutcliffe效率系数(NS)两个指标对模拟效果进行评价。流域总径流率定期和验证期对比验证的R²分别为0.86和0.78; NS分别为0.82和0.67。总生态系统生产力和ET验证期的R²分别为0.89和0.78。可见模型模拟结果的两个评价指标都处于较为理想的区间内, 说明WaSSI-C模型在研究区内具有较好的适用性。并对模型的蒸散计算方法进行了讨论, 在此基础上提出了模型中存在的问题和改进的方向。     

生理房室药动学模型

生理药动学模型较ｎ房室模型能更准确地描述药物在体内的处置过程,但在实际应用中由于其计算结果有较大的误差而限制其应用和推广．在生理模型中,某一组织器官中血液分布容积相对于单位时间的血流量来说,如果太大,就去给计算结果带来较大的误差．本文提出的生理房室模型可以减小这种误差,从而更准确地模拟药物在体内的处置过程．文中对一组模拟的生理和生化参数分别求出了生理房室模型和生理模型的数值解．通过两组解的比较,说明生理房室模型可以描述药物在体内处置过程中的细微变化．     

Maintenance requirements: energy supply from simultaneous endogenous respiration and substrate consumption

Abstract A model is presented that describes energy for maintenance purposes (ATP) as being obtained simultaneously from biomass degradation as well as from substrate degradation in excess of growth requirements. The ratio between both catabolic processes was taken to be growth rate dependent. As such, this approach is intermediate between established models; its significant features are negative growth and the absence of substrate consumption at zero substrate concentration, and the attainability of the maximum specific growth rate (the model parameter μ _max) at elevated substrate concentrations. As a simple case, the amounts of ATP obtained from direct substrate catabolism or from the degradation of an equivalent amount of biomass were taken as identical. Also, the maintenance demand in terms of ATP per unit time and biomass was taken to be constant. True growth rate dependency of maintenance can be implemented by relaxing either of these assumptions.     

An EMG-driven model applied for predicting metabolic energy consumption during movement

The relationship between mechanical work and metabolic energy cost during movement is not yet clear. Many studies demonstrated the utility of forward-dynamic musculoskeletal models combined with experimental data to address such question. The aim of this study was to evaluate the applicability of a muscle energy expenditure model at whole body level, using an EMG-driven approach.Four participants performed a 5-min squat exercise on unilateral leg press at two different frequencies and two load levels. Data collected were kinematics, EMG, forces and moments under the foot and gas-exchange data. This same task was simulated using a musculoskeletal model, which took EMG and kinematics as inputs and gave muscle forces and muscle energetics as outputs. Model parameters were taken from literature, but maximal isometric muscle force was optimized in order to match predicted joint moments with measured ones. Energy rates predicted by the model were compared with energy consumption measured by the gas-exchange data.Model results on metabolic energy consumption were close to the values obtained through indirect calorimetry. At the higher frequency level, the model underestimated measured energy consumption. This underestimation can be explained with an increase in energy consumption of the non-muscular mass with movement velocity.In conclusion, results obtained in comparing model predictions with experimental data were promising. More research is needed to evaluate this way of computing mechanical and metabolic work.     

Numerical model (switchable/dual model) of the human head for rigid body and finite elements applications

In this paper, a methodology for the development and validation of a numerical model of the human head using generic procedures is presented. All steps required, starting with the model generation, model validation and applications will be discussed. The proposed model may be considered as a dual one due to its capabilities to switch from deformable to a rigid body according to the application's requirements. The first step is to generate the numerical model of the human head using geometry files or medical images. The required stiffness and damping for the elastic connection used for the rigid body model are identified by performing a natural frequency analysis. The presented applications for model validation are related to impact analysis. The first case is related to Nahum's (Nahum and Smith 1970) experiments pressure data being evaluated and a pressure map generated using the results from discrete elements. For the second case, the relative displacement between the brain and the skull is evaluated according to Hardy's (Hardy WH, Foster CD, Mason, MJ, Yang KH, King A, Tashman S. 2001.Investigation of head injury mechanisms using neutral density technology and high-speed biplanar X-ray. Stapp Car Crash J. 45:337–368, SAE Paper 2001-22-0016) experiments. The main objective is to validate the rigid model as a quick and versatile tool for acquiring the input data for specific brain analyses.     

On the mechanistic underpinning of discrete-time population models with Allee effect

The Allee effect means reduction in individual fitness at low population densities. There are many discrete-time population models with an Allee effect in the literature, but most of them are phenomenological. Recently, Geritz and Kisdi [2004. On the mechanistic underpinning of discrete-time population models with complex dynamics. J. Theor. Biol. 228, 261-269] presented a mechanistic underpinning of various discrete-time population models without an Allee effect. Their work was based on a continuous-time resource-consumer model for the dynamics within a year, from which they derived a discrete-time model for the between-year dynamics. In this article, we obtain the Allee effect by adding different mate finding mechanisms to the within-year dynamics. Further, by adding cannibalism we obtain a higher variety of models. We thus present a generator of relatively realistic, discrete-time Allee effect models that also covers some currently used phenomenological models driven more by mathematical convenience.     

Conventional and newly developed bioheat transport models in vascularized tissues: A review

Heat transfer in a biological system is a complex process and its analysis is difficult. Heterogeneous vascular architecture, blood flow in the complex network of arteries and veins, varying metabolic heat generation rates and dependence of tissue properties on its physiological condition contribute to this complexity. The understanding of heat transfer in human body is important for better insight of thermoregulatory mechanism and physiological conditions. Its understanding is also important for accurate prediction of thermal transport and temperature distribution during biomedical applications. During the last three decades, many attempts have been made by researchers to model the complex thermal behavior of the human body. These models, viz., blood perfusion, countercurrent, thermal phase-lag, porous-media, perturbation, radiation, etc. have their corresponding strengths and limitations. Along with their biomedical applications, this article reviews various contextual issues associated with these models. After brief discussion of early bioheat models, the newly developed bioheat models are discussed in detail. Dependence of these models on biological properties, viz., thermophysical and optical properties are also discussed.     

物种分布模型在海洋潜在生境预测的应用研究进展

海洋生物的栖息分布与环境要素的关联性一直是海洋生态学研究的热点之一.近年来,物种分布模型被广泛应用于预测海洋物种分布、潜在适宜性生境评价等研究,为保护海洋生物多样性、防治外来物种入侵及制定渔业管理措施等提供了一条有效途径.物种分布模型主要包括生境适宜性指数模型、机理模型和统计模型.本文对物种分布模型的理论基础进行了归纳和总结,回顾了物种分布模型在预测海洋物种潜在地理分布研究中的开发与应用,重点介绍了不同类型统计模型在海洋物种潜在分布预测中的研究实例.比较各种选取变量和模型验证方法,认为赤池信息准则对于选取模型变量具有优势,Kappa系数和受试者操作特征曲线下面积在验证模型精度中应用最广泛.阐述了物种分布模型存在的问题及未来发展趋势,随着海洋生物生理机制研究的进一步深入,机理模型将是今后物种分布模型发展的重点.     

On the mechanistic underpinning of discrete-time population models with complex dynamics

We present a mechanistic underpinning for various discrete-time population models that can produce limit cycles and chaotic dynamics. Specific examples include the discrete-time logistic model and the Hassell model, which for a long time eluded convincing mechanistic interpretations, and also the Ricker- and Beverton-Holt models. We first formulate a continuous-time resource consumption model for the dynamics within a year, and from that we derive a discrete-time model for the between-year dynamics. Without influx of resources from the outside into the system, the resulting between-year dynamics is always overcompensating and hence may produce complex dynamics as well as extinction in finite time. We recover a connection between various standard types of continuous-time models for the resource dynamics within a year on the one hand and various standard types of discrete-time models for the population dynamics between years on the other. The model readily generalizes to several resource and consumer species as well as to more than two trophic levels for the within-year dynamics.     

土壤-植物-大气连续体水热、CO2通量估算模型研究进展

土壤-植物-大气连续体(SPAC)水热、CO2通量的准确估算对理解陆地和大气的物质和能量交换过程有着重要意义.重点阐述了基于过程的土壤-植物-大气连续体水热、CO2通量模型,综述了统计模型、综合模型及基于遥感的模型的发展过程.其中水热通量统计模型包括基于温度和湿度以及基于温度和辐射的方法;CO2通量统计模型包括基于气候因子或蒸散因子以及基于光能利用率的方法.水热通量过程模型包括大叶、双源、多源和多层的水热传输物理模型;CO2通量过程模型包括叶片尺度及由大叶、双叶和多层方法扩展到冠层尺度的生理生态模型以及光合-蒸腾耦合模型.综合模型包括生物物理模型、生物化学模型和生物地理模型.统计模型形式简单,资料易得,对大范围的水热通量模拟具有指导意义;过程模型准确的揭示了水热和CO2通量传输的物理和生理过程,是大尺度综合模型的基础.未来生态系统水热、CO2通量估算模型将集成各种技术手段进行多尺度网络观测和大尺度机理模拟.