城市污泥堆肥温度的空间变异性研究

利用半变异函数对城市污泥堆肥温度的空间变异特性进行了研究 ,对堆体温度进行了克里格法 ( KRIGING)插值。采用通风静态垛堆肥工艺 ,试验了 0 .79、2 .0 3m3 / ( min·m3 )两种通风量。沿着堆肥池长度方向设定 2个纵剖面 ,每个纵剖面的面积为 6 .0 m× 1 .0 m,按 0 .5 m× 0 .1 m布设网格。结果表明 ,在水平方向上堆肥温度的半变异函数用球状模型进行拟合效果较好 ,而在垂直方向上的半变异函数用线性模型进行拟合效果较好 ;在水平方向上两个剖面的温度变程 ( range)分别为 0 .90 m、1 .2 5 m,在垂直方向上的变程分别为 0 .75 m、1 .0 0 m;利用克里格法进行最优内插估值得到的温度等值线图表明 ,高温区域一般位于堆体中层 0 .4～ 0 .6 m,低温区域一般位于堆体下层 0～ 0 .4 m;从温度剖面等值线图判断 ,中试规模的城市污泥堆肥 ,其合理通风量小于 0 .79m3 / min· m3 。     

五年填埋龄准好氧和厌氧填埋体及陈垃圾的理化特性

研究了5年填埋龄准好氧和厌氧填埋体的沉降量、温度和填埋气产生特性,并分析了填埋处理陈腐垃圾的理化性质.结果表明：5年填埋龄准好氧填埋体的表面沉降量和减容率均显著高于厌氧填埋体,同时渗滤液回灌比清水回灌更容易引起垃圾填埋体表面的不均匀沉降.厌氧填埋体的平均温度（25.6 ℃）略高于准好氧填埋体（24.8 ℃）,但差异不显著.准好氧填埋体不同时期的O₂浓度分别高于厌氧填埋体,而CH₄浓度则显著低于厌氧填埋体.5年填埋龄准好氧和厌氧填埋体陈垃圾中厨余物和纸类等易降解有机物含量显著降低,塑料、玻璃、砖瓦和竹木等含量则升高.其中,陈垃圾中有机质与营养元素含量均高于典型南方土壤;除厌氧填埋体陈垃圾中Cr含量超标外,其余重金属含量均未超出《土壤环境质量标准（GB 15618—1995）》的三级标准要求.     

准好氧填埋渗滤液水质变化特性研究

在大型模拟填埋试验装置(21 m×3.8 m×6.0 m)上,研究了准好氧填埋渗滤液水质的主要指标COD_Cr、BOD、NH₃⁺-N和pH的变化特性.结果表明,准好氧填埋结构下渗滤液COD_Cr、BOD浓度下降很快,没有出现在传统填埋场累积的现象,并且封场后39周分别降为173和30 mg·L^-1;NH₃⁺-N浓度下降更为显著,第39周降为1 mg·L^-1,下降率达到99.6%,为渗滤液后续处理解决了NH₃⁺-N浓度过高的难题;pH值在前2周略低于7,第3周后一直呈弱碱性.根据实验数据,拟合了准好氧填埋结构渗滤液污染物的衰减方程.     

不同填埋工艺对填埋气产生动态变化的影响

依据厌氧、准好氧填埋原理构建了填埋试验装置,对准好氧填埋CH₄、O₂浓度的动态变化进行了监测,并与厌氧填埋结构CH₄的浓度变化进行了比较.结果表明,准好氧填埋方式下、厌氧填埋方式下CH₄的平均浓度变化范围分别为7%～13%、35%～50%;准好氧填埋结构有利于减少CH₄气体的产生;CH₄浓度在准好氧填埋、厌氧填埋方式下都表现出明显的空间层次效应,呈现出下层>中层>上层的规律性;准好氧填埋结构的O₂浓度呈现上层>中层>下层的规律性.     

地统计学方法在长白落叶松人工林凋落物现存量估测中的应用

采用地统计学的变异函数分析方法定量研究了15年生落叶松(Larix olgensis)人工纯林凋落物层重量的空间异质性特征,利用地统计学的克里格内插法结合定积分,对凋落物层的重量进行了估测.结果表明1)不同分解层次的凋落物重量的变异函数曲线理论模型均为球状模型,空间变异主要是由结构性因素引起,且空间自相关程度均属中等以上(空间结构比＞25%).2)非参数统计的成对样本符号检验结果表明,变异函数分析结果基础上的克里格内插法适用于凋落物重量的估计.利用此估计值,拟合其与位置坐标值之间的多元回归关系均为二元十次余弦级数多项式.利用此多项式,通过定积分的方法(积分区间为整块样地的大小),估计出15年生落叶松人工纯林中凋落物层的未分解、半分解、完全分解和腐殖质层的重量分别为4.7753、5.4129、8.0742、10.9269t hm-2.3)采用地统计学的克里格空间插值,结合多元回归和定积分的方法,可以实现落叶松人工林凋落物层重量的准确估计.     

采用地统计学方法对水曲柳人工纯林表层根量的估计

采用地统计学的变异函数分析方法定量研究了水曲柳纯林表层根量的空间异质性特征,利用地统计学的克里格内插法结合定积分,对水曲柳纯林表层(0～10 cm)各类型根量进行了估测。结果表明:1)水曲柳细根(<2 mm)、粗根(≥2 mm)、活根和土壤总根变异函数曲线的理论模型符合球状模型,其它植物活根符合指数模型,水曲柳及其它植物死根符合线性模型。水曲柳及其它植物死根的空间变异主要是由随机性因素引起;水曲柳细根、粗根、活根、其它植物活根和土壤总根的空间变异主要是由结构性因素引起,且空间自相关程度均属中等(空间结构比在2 5 %和75 %之间)。水曲柳粗根的空间变异尺度为13.2 m,水曲柳细根、水曲柳活根、土壤总根和其它植物活根的空间变异尺度均大于33.9m。根据理论模型的拟合参数估计,水曲柳细根、水曲柳活根和土壤总根的空间变异尺度为6 1m,其它植物活根为183m。(2 )平均值成对二样本t检验结果表明,变异函数分析结果基础上的克里格内插法适用于水曲柳样地各空间位置处各类型根量的估计。利用此估计值,拟合其与位置坐标值之间的多元回归关系均为二元十次余弦级数多项式。利用此多项式,通过定积分的方法(积分区间为整块样地的大小) ,估计出水曲柳纯林表层根量为1.5 92 6 t/ hm2 ,水曲柳细根为0 .6 86 5 t/     

长白山岳桦种群格局的地统计学分析

应用地统计学的原理和方法研究了长白山岳桦种群空间分布格局及其空间相关关系,首先通过样方调查数据计算岳桦材积的半变异函数,拟合半变异函数模型,然后根据拟合的最优半变异函数模型,进行空间数据插值、绘制岳桦材积的克立拉图,最后对所得到的不同海拔质海拔岳桦材积的半变异函数图和克立格图进行分析。结果表明,在海拔1650－1700m岳桦材积的半变异函数曲线为球形,其空间分布格局为聚集型,种群呈衰退趋势;海拔1750－2000m岳桦材积的半变异函数曲线为直线形,其空间分布格局为随机型,种群较稳定;在海拔2000－2150m岳桦材积的半变异函数曲线为球形,其空间分布格局为聚集型,种群呈增长趋势,这说明长白山桦整体上有一种向上迁移的趋势,尤其是过渡带中的岳桦表现则为更为明显。     

基于地统计学的南沙海域鸢乌贼渔场分析

根据2013年南沙海域4个季度渔业资源声学走航调查数据,以声学探测生物量作为表征渔场分布的指标,对南沙海域鸢乌贼渔场进行分析。结果表明:4个季度鸢乌贼渔场均具有极强的空间相关性,其变异函数的块金效应C0值均小于0.25;通过变异函数,对不同季节分别采用不同理论模型进行拟合,夏季和秋季指数模型为最优拟合模型,春季和冬季分别为球型模型和高斯模型,夏季和冬季模型拟合较好,空间相关性较春秋季强烈;采用克里格法分季度对鸢乌贼渔场进行空间插值分析,各季度渔场生物量较高的区域大部分集中于靠近陆地的区域,表现出明显的斑块状和片状分布特点,且鸢乌贼渔场随时间变化,有逐渐向南转移的趋势。根据变异函数的理论模型和空间插值分析,对插值结果的理论值和实际值进行交叉验证发现,各季度的模型选择恰当。     

桂西北喀斯特洼地土壤有机碳和速效磷的空间变异

空间变异性的研究有助于认识土壤养分的空间分布特征与生态过程之间的关系。采用网格取样(20m×20m),利用地统计学方法分析了典型喀斯特洼地土壤有机碳(SOC)和速效磷(AP)的空间变异特征。结果表明SOC和AP的半变异函数分别用球状模型和指数模型拟合的效果较好。块金效应对SOC和AP总变异的贡献分别为37.9%和49.8%,说明SOC主要受结构性因素控制,而AP受结构性因素和随机因素双重控制。SOC的分布呈明显的带状各向异性特征,在洼地的长轴方向具有较大的变程和较小的基台值,其全向半变异函数的相关距离为135.5m,与洼地不同种植类型地块的覆盖尺度基本相当。AP的分布特征与SOC存在明显差异,具有较大的漂移趋势,其相关距离为413.4m;但在分离漂移趋势后,其相关距离为167.4m,反映了不同地块间的施肥差异对AP的影响较大。喀斯特洼地SOC的空间分布主要受地形和土地利用结构控制,而AP的分布的规律性不明显,可能与施肥等因素的随机性较强有关。     

黄土高原年均降水量空间插值及其方法比较

采用不同空间插值方法(普通克里格法OK、反距离权重法IDW和径向基函数法RBF),对黄土高原地区85个气象站点1957—2013年逐日降水数据进行年均降水量空间插值分析,采用平均绝对误差(MAE)、均方根误差(RMSE)、Pearson相关系数(R)以及准确度(AC)对插值结果进行对比,研究不同方法对该地区年均降水量插值结果的影响.结果表明:研究期间,黄土高原地区年均降水量的Moran I值为0.67,各站点年均降水量存在较强的空间自相关性.63个预测站点和22个检验站点的验证结果显示,3种方法的实测值和预测值均显著相关,但反距离权重法和径向基函数法的平均绝对误差(MAEIDW=38.98,MAERBF=34.61)和均方根误差(RMSEIDW=51.49,RMSERBF=43.79)均高于普通克里格法.通过普通克里格法的不同半变异函数模型(环形模型、球体模型、指数模型、高斯模型)对比发现,环形模型的平均绝对误差最小(MAE=32.34),准确度最高(AC=0.976),指数模型平均绝对误差最大(MAE=33.24).综合对比不同插值方法实测值与估算值的验证结果表明,采用半变异函数为环形模型的普通克里格法是进行黄土高原年均降水量插值较好的方法.     

Patterns in the vertical structure of the tropical lowland rain forest of Los Tuxtlas,Mexico

The vertical structure of one hectare of tropical rain forest was studied at Los Tuxtlas, State of Veracruz, Mexico. The structure was analysed at various scales of analysis, using different methodologies e.g. profile diagrams (0.1 ha) and vertical structure diagrams (1 ha). All profile diagrams suggested presence of stratification to some extent. However, simultaneous evaluation of several adjacent profile diagrams showed that the use of one profile diagram only can be very misleading: gaps or layers apparent in a diagram did usually not reflect gaps or layers that could be recognized in the field.Structure diagrams of abundance, basal area and crown cover showed that this forest community is not stratified, with the exception of an understorey layer below 7.5 m dominated by palms. The vertical structure was described using arbitrarily chosen height intervals. From the forest floor to the canopy top basal area, percentage of deciduous species (and individuals), and percentage of compound-leaved species (and individuals), increased, but total number of individuals and number of species decreased. Leaf sizes tended to decrease in the same direction, and crown cover was approximately evenly distributed. Species from different families dominated different parts along the vertical plane. It is concluded that the vertical structure of tropical rain forest can best be described as a complex gradient, involving many community features. Stratification can best be emphasized as a special case of such a gradient.     

Influence of soil depth on the decomposition of Bouteloua gracilis roots in the shortgrass steppe

The distribution and turnover of plant litter contribute to soil structure, the availability of plant nutrients, and regional budgets of greenhouse gasses. Traditionally, studies of decomposition have focused on the upper soil profile. Other work has shown that temperature, precipitation, and soil texture are important determinates of patterns of decomposition. Since these factors all vary through a soil profile, it has been suggested that decomposition rates may vary with depth in a soil profile. In this work, we examine patterns of root decomposition through a shortgrass steppe soil profile. We buried fresh root litter from Bouteloua gracilis plants in litterbags at 10, 40, 70, and 100 cm. Litterbags were retrieved six times between July 1996 and May 1999. We found that the decomposition rate for fresh root litter was approximately 50% slower at 1 m than it was at 10 cm. After 33 months, 55% of the root mass buried at 10 cm remained, while 72% of the root mass buried at 1 m was still present. This corresponds to a 19-year residence time for roots at 10 cm and a 36-year residence time for roots at 1 m. Mass loss rates decreased linearly from 10 cm to 1 m. Patterns of total carbon and cellulose loss rates followed those of mass loss rates. Roots at 1 m tended to accumulate lignin-like compounds over the course of the experiment. Differences in the stabilization of lignin may be a consequence of differences in microbial community through a shortgrass steppe soil profile.     

Effect of Mg2+ concentration on Ca2+ uptake kinetics and structure of the sarcoplasmic reticulum membrane.

Direct measurements of phosphorylation of the Ca2+ ATPase of the sarcoplasmic reticulum (SR) have shown that the lifetime of the first phosphorylated intermediate in the Ca2+ transport cycle, E1 approximately P, increases with decreasing [Mg2+] (Dupont, Y. 1980. Eur. J. Biochem. 109:231-238). Previous x-ray diffraction work (Pascolini, D., and J.K. Blasie. 1988. Biophys. J. 54:669-678) under high [Mg2+] conditions (25 mM) indicated that changes in the profile structure of the SR membrane could be responsible for the low-temperature transient trapping of E1 approximately P that occurs at temperatures below 2-3 degrees C, the upper characteristic temperature th for lipid lateral phase separation in the membrane. We now present results of our study of the Ca2+ uptake kinetics and of the structure of the SR membrane at low [Mg2+] (less than or equal to 100 microM). Our results show a slowing in the kinetics of both phases of the Ca2+ uptake process and an increase in the duration of the plateau of the fast phase before the onset of the slow phase, indicating an increase in the lifetime (transient trapping) of E1 approximately P. Calcium uptake kinetics at low [Mg2+] and moderately low temperature (approximately 0 degree C) are similar to those observed at much lower temperatures (approximately -10 degrees C) at high [Mg2+]. The temperature-induced structural changes that we observed at low [Mg2+] are much more pronounced than those found to occur at higher [Mg2+]. Also, at the lower [Mg2+] the upper characteristic temperature th for lipid lateral phase separation was found to be higher, at approximately 8-10 degrees C. Our studies indicate that both temperature and [Mg2+] affect the structure and the functionality (as measured by changes in the kinetics of Ca2+ uptake) of the SR membrane. Membrane lipid phase behavior and changes in the Ca2+ ATPase profile structure seem to be related, and we have found that structural changes are responsible for the slowing of the kinetics of the fast phase of Ca2+ uptake, and could also mediate the effect that [Mg2+] has on E1 approximately P lifetime.     

Calorimetric investigations of the structural stability and interactions of colicin B domains in aqueous solution and in the presence of phospholipid bilayers

The effects of pH and temperature on the stability of interdomain interactions of colicin B have been studied by differential-scanning calorimetry, circular dichroism, and fluorescence spectroscopy. The calorimetric properties were compared with those of the isolated pore-forming fragment. The unfolding profile of the full-length toxin is consistent with two endothermic transitions. Whereas peak A (T(m) = 55 degrees C) most likely corresponds to the receptor/translocation domain, peak B (T(m) = 59 degrees C) is associated with the pore-forming domain. By lowering the pH from 7 to 3.5, the transition temperature of peaks A and B are reduced by 25 and 18 degrees C, respectively, due to proton exchange upon denaturation. The isolated pore-forming fragment unfolds at much higher temperatures (T(m) = 65 degrees C) and is stable throughout a wide pH range, indicating that intramolecular interactions between the different colicin B domains result in a less stable protein conformation. In aqueous solution circular dichroism spectra have been used to estimate the content of helical secondary structure of colicin B ( approximately 40%) or its pore-forming fragment ( approximately 80%). Upon heating, the ellipticities at 222 nm strongly decrease at the transition temperature. In the presence of lipid vesicles the differential-scanning calorimetry profiles of the pore-forming fragment exhibit a low heat of transition multicomponent structure. The heat of transition of membrane-associated colicin B (T(m) = 54 degrees C at pH 3.5) is reduced and its secondary structure is conserved even at intermediate temperatures indicating incomplete unfolding due to strong protein-lipid interactions.     

MIS 21 and the Mid-Pleistocene climate transition: Climate and sea-level variation from a sediment core in Osaka Bay,Japan

We report climate and sea-level variation for the marine oxygen isotope stage (MIS) 21, encompassing the end of the Mid-Pleistocene climate transition (MPT), based on pollen, diatom, and sulfur records from a 50-m thick sequence in a core from Osaka Bay. An extremely warm climate coincided with the sea level highstand of substage 21.5, when the warm-temperate element Quercus (Cyclobalanopsis) exceeds 40% of total arboreal pollen. This was followed by a warm-temperate to temperate and humid climate that continued until the end of MIS 21. A linear age model shows that climate was dominated by precessional cyclicity, with an inverse correlation between temperature and precipitation. The postglacial sea-level rise reached its highest peak in substage 21.5, when paleo-Osaka Bay reached its maximum extent including Kyoto and Nara Basins. At this time pelagic diatoms were dominant in the central part of the bay. Sea level dropped below the Osaka Bay sill (about ? 60 m at present) during substage 21.4, followed by a rise above the sill in substage 21.3, and a drop at 21.2. Sea level remained below the sill during substage 21.1. The thermal maximum and sea level peak occurred just after the rapid postglacial sea level rise, after which there was a gradual decline in temperature and sea level accompanied by precession-related oscillations; these features are typical of the post-MPT interglacials dominated by 100-ka cyclicity. These features may be a sign of termination of the MPT.     

不同尺度下低山茶园土壤有机质含量的空间变异

南方低山丘陵区是我国茶园集中分布的区域,研究其土壤特性的空间变异性,尤其是有机质的空间分布特性,可以为实施低山丘陵茶园土壤养分精准管理提供依据。以四川蒙顶山茶园为研究对象,利用地统计学方法,在两个尺度下对其土壤有机质含量的空间变异性进行了研究。结果表明:(1)小尺度下,蒙顶山茶园土壤有机质含量具有中等空间相关性(C0与C0 C的比值为49.9%),空间相关距离达到了894m,随机性和结构性因子对有机质含量空间变异的影响各占一半;茶园土壤有机质含量在坡体垂直方向的变异性较强,在坡体水平方向上的变异较弱;普通Kriging插值分析说明有机质含量从东北至西南呈明显的带状分布,垂直方向上随海拔升高而增加。(2)微尺度下,代表性茶园土壤有机质含量具有强烈的空间相关性(C0与C0 C的比值为4.1%),空间相关距离达到了311m,结构性因子是影响其空间变异的主要因素;各向异性分析,茶园土壤有机质含量也在坡面垂直方向变异较强,且在坡面倾斜45°方向也存在一定变异;普通Kriging分析,坡面由上到下有机质含量逐渐增加。     

Tidal transport of planktonic copepods across the sill of a British Columbia fjord

Estimates of plankton transport into and out of semi-enclosedbodies of water could be of value in long-term ecological monitoring.The study reported here examined the problems associated withthe estimates of tidal transport of four species of planktoniccopepods across the sill of a British Columbia fjord. Transportwas estimated by applying calculated tidal volume exchange toplankton field data collected over a 13-month period. Hydrographicdata during the period indicated that tidal exchange was thedominant mechanism for the transport of water Differences indepth distribution and behaviour resulted in a species-specificeffect of tidal exchange. The diel vertical migration of Metridialucens and the ontogenetic migration of Eucalanus bungi resultedin transport only during those periods when organisms were presentin water near or above sill depth. Corycaeus anglicus was presentabove sill depth at all times and transport occurred throughoutthe study period. Euchaeta japonica, although present in waterabove sill depth throughout the year, was transported acrossthe sill only during the winter months. Transport estimatescould be related to estimates of fjord concentrations for C.anglicus and E. bungii. For M. lucens and E. japonica, it issuggested that natality and mortality within the inlet was sufficientto mask the effect of tidal transport on the species concentration.     

低温小麦种质叶片结构及某些生理特性

通过对小麦冠层温度的长期观测,发现自然界存在冠层温度持续偏低的低温种质和冠层温度持续偏高的高温种质.在扬花结实期,低温种质冠层温度比高温种质低1～4 ℃.低温种质功能叶片叶肉细胞小,排列紧密,层数较多,通常比高温种质多1～2层叶肉细胞.低温种质陕229、901和小偃6号3片功能叶的平均厚度分别为166、192和165 μm,平均比高温种质薄26 μm;3片功能叶叶脉的平均间距分别为257、231和245 μm,平均比高温种质小31 μm;3片功能叶大叶脉平均横截面积分别为5 961、6 580和5 603 μm²,平均比高温种质大837 μm²;小叶脉平均横截面积分别为1 624、1 521和1 472 μm²,平均比高温种质大246 μm².在扬花结实期,低温种质陕229、901和小偃6号3片功能叶平均叶绿素含量分别为2.8749、2.8162和2.4129 g·100 g^-1 FW;净光合速率分别为10.8640、10.8003和10.1939 μmol·m^-2·s^-1;蒸腾速率分别为0.0076、0.0074和0.0067 mol·m^-2·s^-1,均明显高于高温种质.结果表明,植物的冠层温度与植物本身的器官结构和生理功能联系密切.