2015—2020年间海南热带雨林国家公园景观格局变化

海南热带雨林国家公园森林资源富集，探究该地区景观格局时空演变特征，对维护海南岛生态安全屏障具有重要意义。该研究依托2015年和2020年海南热带雨林国家公园地表覆盖数据，建立景观分布格局体系，采用景观格局指数、单一景观动态度和景观转移矩阵的方法，分析海南热带雨林国家公园10类土地覆盖类型的景观格局变化特征，探究其变化的影响因素。结果表明：(1)2015—2020年，海南热带雨林国家公园整体景观破碎度呈现降低趋势，空间集聚性增加，综合动态度较小，景观类型整体较稳定。(2)雨林优势种常绿阔叶林面积不断增加，破碎度减小，呈正向增长态势；针叶林与灌木林面积减少；部分水体转化为湿地等，面积减小；其余景观类型面积占比较小，按自然演替方向发展变化。(3)景观格局演变主要以雨林自然演替为主，其次受政策、气候等因素综合影响。综上所述，自开展海南热带雨林国家公园体制试点以来，其景观格局趋于稳定。政策引导发挥着重要的正向作用，有针对性地开展热带雨林景观保护及修复工作，有助于海南热带雨林国家公园可持续发展。     

呼伦贝尔森林-草原交错区景观格局时空动态

基于遥感（RS）与地理信息系统（GIS）相结合的方法,解译并提取了1988年、1995年、2000年和2004年四期呼伦贝尔森林．草原交错区的景观格局空间分布信息,并在Fragstats3．3软件中,分别从景观级别和类型级别出发,分析了该区景观格局的时空动态变化。结果表明：（1）16年来,呼伦贝尔森林-草原交错区各景观类型转换频繁。其中,林地面积减少量最多,达7858．15km^2,主要转换为草地;未利用土地面积增加量最多,净增4087．25km^2,增加的面积主要来源于草地和林地。（2）景观格局整体波动较大,景观破碎度、景观多样性指数逐年增大,优势度指数降低。（3）受人为干扰的影响,研究区内各主要景观类型均表现出景观斑块由大到小,由少到多,斑块形状复杂化程度增加的特点。（4）主要景观类型质心向东偏移,其中,林地景观的质心向东南方向偏移了50．22°大约4．48km;草地景观整体向东北方向偏移了79．96°大约29．93km。     

亚热带人工和天然马尾松、杉木林生长对干旱的生态弹性差异

选取福建中西部地区相似气候条件下马尾松和杉木的天然林和人工林进行研究,利用年轮宽度、年轮宽度指数和断面积增量重建了4种林型共109株松树20年(1993—2012年)的年生长量,计算其对连续两次极端干旱事件(2003—2004年和2011年)的抵抗力、恢复力和弹性指数,分析人工林和天然林在抵抗力和弹性方面的差异。结果表明:马尾松和杉木对水分的需求在时间上存在差异,这解释了其对2003—2004年干旱事件的响应不一致。干旱压力极大地降低了马尾松和杉木的生长,但树木生长并未表现出干旱遗留效应。受干旱强度的影响,4种林型径向生长对2003—2004年干旱的响应强于2011年。干旱事件后马尾松比杉木具有更强的恢复能力;天然林比人工林对干旱的敏感性更高,同时弹性也更大。杉木人工林更容易受到频发的极端干旱事件的影响,在人工林抚育管理中应选择抗旱能力较强的遗传种源,以应对气候变暖导致的干旱频发。     

基于遥感影像的丹霞山国家级自然保护区森林景观格局分析

森林景观格局分析是景观格局优化、森林资源的可持续性经营与保护的重要基础。以无人机遥感影像和DEM为基础数据,利用ArcGIS和Fragstats软件对所选取的不同景观指数进行计算,分析了丹霞山森林景观的类型、格局特征及其地形分异规律。结果表明:1)从类型水平指数来看,丹霞山森林景观类型以天然林为主,占总面积的78.42%,表现出较高的集中连片性;2)从景观水平指数来看,丹霞山景观多样性和均匀度指数均较低,而蔓延度指数和连通度指数则较高,分别为77.85和99.97,表明景观以少数大面积的斑块为主,斑块间连接密切,自然连通度高; 3)从功能分区景观格局和地形分异规律来看,与人类活动密切相关的农田、人工林、裸地、居民地、人工水体和自然水体六类森林景观主要集中分布于海拔较低(60—150 m)、坡度平缓(0—5°)、无坡向的实验区内;灌木、草地、天然林和裸岩四类森林景观则较均衡的分布于海拔60—350m的各级坡度和坡向的核心区和缓冲区内。综上所述,丹霞山森林景观保持完好,破碎化程度较低,人为活动干扰较少,斑块之间物质、能量和物种交换的潜力较大。应建立无人机遥感监测系统,长期、准确的跟踪森林景...     

格氏栲天然林与人工林凋落物数量、养分归还及凋落叶分解(英文

通过对中亚热带格氏栲天然林(natural forest of Castanopsis kawakamii。约150年生)、格氏挎和杉木人工林(monoculture plantations of C．kawakamii and Cunninghamia lanceolata,33年生)凋落物数量与季节动态、养分归还及凋落叶分解与其质量的关系为期3a的研究表明。林分年均凋落量及叶所占比例分别为：格氏栲天然林11．01t／hm^1。59．70t／hm^2;格氏栲人工林9．54％。71．98％;杉木人工林5．47t／hm^2。58．29％。格氏栲天然林与人工林凋落量每年只出现1次峰值(4月份)。而杉木林的则出现3次(4或5月份、8月份和11月份)。除杉木林的Ca和格氏栲人工林的Mg年归还量最大外。N、P、K及养分总归还量均以格氏栲天然林的为最大。杉木人工林的最小。分解la后格氏栲天然林中格氏栲叶的干重损失最大(98．16％)。杉木叶的最小(60．78％)。C／N及木质素／N比值与凋落叶分解速率呈显著负相关。而N、水溶性化合物初始浓度与分解速率呈显著正相关。与针叶树人工林相比,天然林的凋落物数量大、养分归还量高、分解快。具有良好自我培肥地力的能力。因此。保护和扩大常绿阔叶林资源已成为南方林区实现森林可持续经营的重要措施之一。     

人工林与天然林破碎化过程差异对比——以美国华盛顿州和密西西比州为例

森林损失和破碎化一直是国际社会普遍关注的重大环境问题之一。根据Forman景观变化包括穿孔、分割、破碎化、收缩和消失5种空间过程的理论,利用ArcGIS Modeler建立森林破碎化过程模型用以明确描述森林景观破碎化的空间过程和生态进程。基于NLCD2001、2006、2011 3期数据,以美国华盛顿州和密西西比州为研究区,利用森林破碎化过程模型,将森林损失斑块分为4种破碎化过程(分割类型因其线状特征被归入破碎化类型),对比分析天然林和人工林的破碎化过程在时空上的差异性。研究表明天然林破碎化斑块多分布于城市/森林、耕地/森林、以及灌木/森林的交界处,而人工林破碎化斑块分布格局较为零散;天然林中破碎化斑块和收缩斑块大多发生在上阶段收缩、破碎化以及穿孔斑块的边缘,而人工林中4种空间过程的承接关系不像天然林那么明显,但两者整体上都呈现相似的"收缩-消失-穿孔/破碎化"变化规律,主要表现为收缩类型占主导然后慢慢消退,穿孔和破碎化逐渐增多占据新的主导。     

格氏栲天然林与人工林根际土壤微生物及其生化特性的研究

通过对格氏栲天然林（约１２０年生）和人工林（２８年生）根际土壤和全土微生物、生化活性、土壤养分的研究,结果表明：格氏栲天然林根际和全土土壤养分、土壤微生物区系、生理类群数量、土壤酶活性和生化作用强度均比相应人工林的大,格氏栲天然林根际土壤速效性养分相对富集,而人工林的则存在亏缺现象。格氏栲人工林的根际效应（Ｒ／Ｓ值）比天然林的明显。     

黑龙江省森林景观多样性动态

讨论了1949—1981年黑龙江省森林景观多样性的动态。利用1949年和1981年森林资源分布图,选取7个有代表性的度量景观多样性的定量指标：斑块密度、周长-面积分数维、聚集度、斑块散布与毗连指数、Shannon多样性指数、优势度、均匀度,在ESRI’S ARCGIS 8和FRAGSTATS 3．3软件支持下,系统研究了景观元素空间格局的变化。结果表明在近32年的时间进程中,区域森林景观破碎化现象加剧,其中以红松(Pinus koraiensis)林的破碎化最为严重。从斑块多样性、格局多样性和类型多样性的动态变化分析看出,原生的景观斑块类型在数量上不断减少或被异类景观所代替,即景观类型所占景观表面的百分比发生了变化,从而引起景观内部空间格局的改变。整个森林的景观多样性和景观类型分布的均匀性降低,优势度增加。人类不合理的经济活动,如毁林开荒、乱砍滥伐等,改变了景观异质性,从而造成景观多样性的变化。现在应该把对森林的保护和经营提到日程上来。天然林保护工程的实施对于促进林业部门休养生息、培育与保护森林资源,保护生物多样性和改善生态环境等具有重要意义。保护现有森林资源,实行采育结合,实施天然林保护工程,使森林的经营走可持续发展的道路是切实可行的解决办法．     

石家庄西部太行山区景观格局时空变化

基于1987、2000年两期TM、ETM＋遥感数据资料，利用ArcGIS提取石家庄西部太行山区的景观类型转移矩阵，并结合重心模型，从时间和空间上对景观格局动态变化进行分析。结果表明：（1）1987～2000年，景观基质均为耕地，林地、草地、水域、建设用地和未利用土地作为斑块单元镶嵌其中；耕地、草地和水域的面积均为减少，其中草地面积减少量最大，主要向林地转化；林地、建设用地和未利用土地的面积均为增加，其中建设用地面积增加量最大，主要由未利用土地转化而来。（2）1987～2000年间，水域重心迁移距离最大；耕地、水域和建设用地的重心偏移方向为北偏西；林地和草地的重心偏移方向为北偏东；未利用土地的重心偏移方向为南偏西。     

西双版纳地区森林变化碳效应与生态效益评估

减少发展中国家因森林砍伐与森林退化导致的碳排放和保持碳储量(REDD+),不仅能减少因森林砍伐和森林退化造成的碳排放,而且还可以带来其它生态效益,如减缓森林破碎化、保护生物多样性和增强水土保持功能等。以中国的西双版纳地区为研究区域,以毁林最严重的1976—2007年为REDD+基线,基于卫星影像,并结合植被指数,提取了研究区的土地利用变化信息。基于IPCC温室气体清单方法,计算了研究区的森林碳储量变化。在此基础上,对REDD+的碳汇效益和生态效益进行了系统综合评估。结果显示：(1)1976—2007年间天然林碳储量从占总碳储量的78.24%减少至50.52%,这是造成西双版纳地区碳储量减少的主要原因。(2)1976—2007年,天然林的斑块数量和平均最近邻距离分别增加了120.00%和25.21%,平均斑块面积下降了71.98%,说明天然林的破碎化程度加剧。从研究区整体景观格局来看,斑块数量、Shannon多样性指数和Shannon均一性指数分别增加了8.16%、51.39%和34.07%;与此同时,平均斑块面积和景观内聚力指数分别下降了26.26%和2.13%,表明研究区整体景观格局...     

Distribution of N,P, K,Ca, Mg,S, Zn,Fe, Mn and Cu in groundnut

Summary Concentration of N, P, K, Ca, Mg and S in summer groundnut crop was higher than in kharif while Zn, Fe, Mn and Cu contents were higher in summer crop. Kernel's N, P and Zn; Leaflet's Ca and Mn; Stem's K and Fe; Root's S and Cu and Petiole's Mg contents were highest. Shell's N, P, K, Mg, S, Zn and Cu; Kernel's Ca, Fe and Mn contents were the least. N, P, K, S, Zn and Cu concentrations decreased linearly as the crop grew. Ca, Mg, Fe and Mn concentrations did not display any distinct pattern. Ca concentration was positively correlated with pod yield in both the seasons.     

Simultaneous measurement of the trace elements Al, As, B, Be, Cd, Co, Cu, Fe, Li, Mn, Mo, Ni, Rb, Se, Sr, and Zn in human serum and their reference ranges by ICP-MS

The goal of this article was to establish reference ranges of the concentration of trace elements in human serum and to compare these results with those reported by other authors. We describe the sample preparation and measurement conditions that allow the rapid, precise, and accurate determination of Al, As, B, Be, Cd, Co, Cu, Fe, Li, Mn, Mo, Ni, Rb, Se, Sr, and Zn in human serum samples (n=110) by inductively coupled plasma-mass spectrometry (ICP-MS). Accuracy and precision were determined by analyzing three reconstituted reference serum samples by comparison with other methods and by the standard addition procedure. The advantages of the ICP-MS method include short time of analysis of the elements mentioned, low detection limit, high precision, and high accuracy. Disadventages include a high risk of contamination due to the presence of some of the elements of interest in the environment, the relatively delicate sample handling, and the high cost of the equipment.     

Reference values for the concentrations of As,Cd, Co,Cr, Cu,Fe, I,Hg, Mn,Mo, Ni,Pb, Se,and Zn in selected human tissues and body fluids

This report attempts to formulate reference ranges of elemental concentrations for 15 trace elements in selected human tissues and body fluids. A set of samples consisting of whole blood, blood serum, urine, milk, liver, and hair were chosen and considered for 15 elements of biological significance: As, Cd, Co, Cr, Cu, F, Fe, I, Hg, Mn, Mo, Ni, Pb, Se, and Zn. The results represent wholly or partially data received from 40 countries of the global regions of Africa, Asia, Europe, North, South, and Central America, Australia, and New Zealand. This survey, even if qualitative, has been useful in demonstrating certain trends of trace-element scenarios around the world. It is of course recognized that both diet and environment exert a strong influence on the distribution pattern of several elements, such as As, Cd, Mn, Pb, Se, and Zn. A limited comparison of the available information on soil status of different countries reflected some interesting associations for elements, such as Mn and Zn. Importantly, this study revealed that only a few countries were in a position to identify a reasonable amount of data on samples requested for this project. Regretably, for a number of countries, any dependable data for even such essential elements as Cu, Fe, and Zn were not available. In view of the nutritional importance of many elements, the time is ripe for concerted efforts by intergovernmental agencies to initiate investigations or commission task forces/projects to generate reliable reference data for selected global regions, which sadly lack data of any kind at present.     

Crystal structure, detonation performance, and thermal stability of a new polynitro cage compound: 2, 4, 6, 8, 10, 12, 13, 14, 15-nonanitro-2, 4, 6, 8, 10, 12, 13, 14, 15-nonaazaheptacyclo [5.5.1.13, 11. 15, 9] pentadecane

A new polynitro cage compound 2, 4, 6, 8, 10, 12, 13, 14, 15-nonanitro-2, 4, 6, 8, 10, 12, 13, 14, 15-nonaazaheptcyclo [5.5.1.1(3,11).1(5,9)] pentadecane (NNNAHP) was designed in the present work. Its molecular structure was optimized at the B3LYP/6-31 G(d,p) level of density functional theory (DFT) and crystal structure was predicted using the Compass and Dreiding force fields and refined by DFT GGA-RPBE method. The obtained crystal structure of NNNAHP belongs to the P-1 space group and the lattice parameters are a = 9.99 ?, b = 10.78 ?, c = 9.99 ?, α = 90.01°, β = 120.01°, γ = 90.00°, and Z = 2, respectively. Based on the optimized crystal structure, the band gap, density of state, thermodynamic properties, infrared spectrum, strain energy, detonation characteristics, and thermal stability were predicted. Calculation results show that NNNAHP has detonation properties close to those of CL-20 and is a high energy density compound with moderate stability.     

Monovalent Cation Permeation through the Connexin40 Gap Junction Channel : Cs,Rb, K,Na, Li,TEA, TMA,TBA, and Effects of Anions Br,Cl, F,Acetate, Aspartate,Glutamate, and NO3

The unitary conductances and permeability sequences of the rat connexin40 (rCx40) gap junction channels to seven monovalent cations and anions were studied in rCx40-transfected neuroblastoma 2A (N2A) cell pairs using the dual whole cell recording technique. Chloride salt cation substitutions (115 mM principal salt) resulted in the following junctional maximal single channel current-voltage relationship slope conductances (γ_j in pS): CsCl (153), RbCl (148), KCl (142), NaCl (115), LiCl (86), TMACl (71), TEACl (63). Reversible block of the rCx40 channel was observed with TBA. Potassium anion salt γ_j are: Kglutamate (160), Kacetate (160), Kaspartate (158), KNO₃ (157), KF (148), KCl (142), and KBr (132). Ion selectivity was verified by measuring reversal potentials for current in rCx40 gap junction channels with asymmetric salt solutions in the two electrodes and using the Goldman-Hodgkin-Katz equation to calculate relative permeabilities. The permeabilities relative to Li⁺ are: Cs⁺ (1.38), Rb⁺ (1.32), K⁺ (1.31), Na⁺ (1.16), TMA⁺ (0.53), TEA⁺ (0.45), TBA⁺ (0.03), Cl⁻ (0.19), glutamate⁻ (0.04), and NO₃− (0.14), assuming that the monovalent anions permeate the channel by forming ion pairs with permeant monovalent cations within the pore thereby causing proportionate decreases in the channel conductance. This hypothesis can account for why the predicted increasing conductances with increasing ion mobilities in an essentially aqueous channel were not observed for anions in the rCx40 channel. The rCx40 effective channel radius is estimated to be 6.6 Å from a theoretical fit of the relationship of relative permeability and cation radius.     

Relations of the Al,B, Ba,Br, Ca,Cl, Cu,Fe, K,Li, Mg,Mn, Na,P, S,Si, Sr,and Zn mass fractions to morphometric parameters in pediatric and nonhyperplastic young adult prostate glands

The variation with age of the 18 trace element mass fractions and some histological characteristics of intact prostate glands of 50 subjects aged 0–30 years was investigated by instrumental neutron activation analysis, inductively coupled plasma atomic emission spectrometry, and a quantitative morphometric analysis. Mean values ± standard error of the mean (M ± SΕΜ) for the mass fractions (in milligrams per kilogram wet tissue) of these trace elements in pre-puberty were: Al 28.5 ± 9.0, B 0.40 ± 0.11, Ba 1.48 ± 0.44, Br 10.5 ± 1.5, Ca 241 ± 30, Cl 3,203 ± 278, Cu 3.51 ± 0.89, Fe 33.7 ± 4.1, K 2,364 ± 145, Li 0.020 ± 0.004, Mg 153 ± 23, Mn 0.46 ± 0.06, Na 2,286 ± 130, P 1,391 ± 100, S 1,698 ± 132, Si 62 ± 11, Sr 0.38 ± 0.08, and Zn 27.6 ± 2.3. During puberty and postpuberty, when there is a significant increase in circulating androgens, the mean values were: Al 7.2 ± 1.4, B 0.21 ± 0.05, Ba 0.25 ± 0.06, Br 5.8 ± 1.0, Ca 433 ± 81, Cl 2,314 ± 201, Cu 1.77 ± 0.13, Fe 20.9 ± 1.6, K 2,585 ± 118, Li 0.0088 ± 0.0014, Mg 232 ± 27, Mn 0.34 ± 0.04, Na 1,875 ± 107, P 1,403 ± 98, S 1,673 ± 73, Si 22.2 ± 3.1, Sr 0.22 ± 0.03, and Zn 93.3 ± 8.9. Mean values (M ± SΕΜ) of percent volumes (%) of the stroma, epithelium and lumen in the prostate before puberty were 73.4 ± 2.6, 20.4 ± 1.7, and 4.45 ± 0.94, respectively, versus 46.5 ± 2.5, 38.5 ± 1.9, and 14.9 ± 1.2 during puberty and postpuberty. This work’s results confirm that the Zn mass fraction in prostate tissue is an androgen-dependent parameter. For the first time it has been demonstrated that the glandular lumen is a main pool of Ca, Mg, and Zn accumulation and that the stroma is a main pool of Al, B, Ba, Br, Cl, Cu, Fe, Mn, Na, and Si accumulation in the normal human prostate, for the age range 0–30 years. It was concluded that the Ca, Mg, and Zn binds tightly within the prostatic fluid, because the volume of glandular lumen reflects the volume of prostatic fluid.     

Competitive inhibition and selectivity enhancement by Ca in the uptake of inorganic elements (Be, Na, Mg, K, Ca, Sc, Mn, Co, Zn, Se, Rb, Sr, Y, Zr, Ce, Pm, Gd, Hf) by carrot (Daucus carota cv. U.S. harumakigosun)

We investigated the uptake of inorganic elements (Be, Na, Mg, K, Ca, Sc, Mn, Co, Zn, Se, Rb, Sr, Y, Zr, Ce, Pm, Gd, and Hf) and the effect of Ca on their uptake in carrots (Daucus carota cv. U.S. harumakigosun) by the radioactive multitracer technique. The experimental results suggested that Na, Mg, K, and Rb competed for the functional groups outside the cells in roots with Ca but not for the transporter-binding sites on the plasma membrrane of the root cortex cells. In contrast, Y, Ce, Pm, and Gd competed with Ca for the transporters on the plasma membrane. The selectivity, which was defined as the value obtained by dividing the concentration ratio of an elemental pair, K/Na, Rb/Na, Be/Sr, and Mg/Sr, in the presence of 0.2 and 2 ppm Ca by that of the corresponding elemental pair in the absence of Ca in the solution was estimated. The selectivity of K and Rb in roots was increased in the presence of Ca. The selectivity of Be in roots was not affected, whereas the selectivity of Mg was increased by Ca. These observations suggest that the presence of Ca in the uptake solution enhances the selectivity in the uptake of metabolically important elements against unwanted elements.     

The Effect of Age and Gender on Al, B, Ba, Ca, Cu, Fe, K, Li, Mg, Mn, Na, P, S, Sr, V, and Zn Contents in Rib Bone of Healthy Humans

The effect of age and gender on major, minor, and trace element contents in the intact rib bone of 80 relatively healthy 15–55-year-old women and men was investigated. Contents or upper limit of contents of 16 chemical elements in the rib bone were determined by inductively coupled plasma atomic emission spectrometry (ICP-AES). Mean values (M?±?SΕΜ) for the mass fraction of Ba, Ca, Cu, Fe, K, Li, Mg, Na, P, S, Sr, and Zn (milligram per kilogram of dry bone) were as follows: 2.54?±?0.16, 171,400?±?4,050, 1.35?±?0.22, 140?±?11, 1,874?±?71, 0.049?±?0.011, 2,139?±?38, 5,378?±?88, 75,140?±?1,660, 1,881?±?51, 291?±?20, and 92.8?±?1.5, respectively. The upper limits of contents of Al, B, Mn, and V were <7.20, <0.65, <0.36, and <0.03, respectively. Statistically significant tendency for the Ca, Mg, and P content to decrease with age was found in the human rib bone, regardless of gender. The mass fraction of Fe in the male rib bone increases with age. It was shown that higher Ca, Mg, Na, P, and Sr mass fractions as well as lower Fe content were typical of female ribs as compared to those in male ribs.