998 resultados para 23-229


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1. Systematic list of birds (pp. 23-31) 2. Observations on the Galapagos fur seal, Arctocephalus australis galapagoensis Heller, 1904 (pp. 31-33) 3. Cetaceans observed (pp. 33-34)

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东灵山地区年均降水量659.7mm,单次降水以雨量小、雨强低的降水为主。水汽压(年均17.7mb)、相对湿度(年均66%)的季节变化呈现生长季高、冬季低的趋势。年均蒸发量1019.5mm;气温、风速、日照时间和水压与月蒸发量和日蒸量相关显著;气温、日照时间和水压分别在11-6月、7-8月和9-10月为决定蒸发量的首要因子。枯枝落叶层、土壤层湿度主要受前十日降水量和坡向影响。 植物体含水量生长季节较高,冬季较低;含水量随径级的增大而降低。六个灌木树种的平均含水量大小顺序为:毛榛(48.62%)最高荆条(36.32%)最低;七个乔木树种水分含量为油松,56.14%;蒙椴,54.19%;华北落叶松,52.91%;五角枫,43.64%;辽东栎,41.87%;棘皮桦,41.13%;大叶白腊,37.79%。几种植被类型的储水量为:辽东栎林,82.08mm;华北落叶松林,47.35mm;混交林,34.60mm;油松林,31.33mm;灌丛,12.40mm。各树种叶片日最低水势的季节均值为:辽东栎,-16.1bar;五角枫,-15.8bar;大叶白腊,-15.1bar;糠椴,-13.4bar;棘皮桦,-12.3bar;蒙椴,-12.2bar。叶片水势的日间变化均呈一“V”形曲线;光照在叶片水势的日间变化中起着决定性作用。 96年各树种平均单株树干茎流量为辽东栎,30.3mm(4.19%);华北落叶松,16.1mm(2.22%);油松,8.9mm(1.23%);棘皮桦,2.9mm(0.40%)。两个生长季各林分冠层的水量平衡为:辽东栎林,树干流茎量101.87mm(9.18%),穿透降水量823.08mm(74.15%),截留量185.05mm(16.67%);华北落叶松林,树干径流量66.88mm(6.03%),穿透降水量836.92mm(75.40%),截留量206.20mm(18.58);混交林,树干径流量50.13(4.52%),穿透降水量846.78mm(76.29%),截留量212.20mm(19.12%);油松林,树干径流量33.90mm(3.05%),穿透降水量934.88mm(84.22%),截留量141.22mm(12.72%)。多元回归分析表明,树干流茎量S与降水量P和前24小时降水量P_1呈显著正相关关系;穿透降水量T与降水量P和最大雨强M正相关显著。附加截留量与降水时间成正比。 枯枝落叶层的生物量为:油松林,25.56t/hm~2;华北落叶松林20.01t/hm~2;辽东栎林,8.31t/hm~2;混交林,7.98t/hm~2。枯枝落叶层的平均实际持水量和有效持水量均以油松林最大,其次是华北落叶松林,而混交林和辽东栎林较低;枯枝落叶层的实际持水量和有效持水量的季节变化分别与前十日降水量P10成正相关和负相关关系。枯枝落叶层的截留量为油松林>华北落叶松林>辽东栎林>混交林;油松林(145.632mm和90.800mm)混交林(61.816mm和54.504mm)。油松林、辽东栎林、混交林和华北落叶松林去除枯枝落叶层后,土壤入渗量比对照平均降低100mm以上;表层土壤含水量分别比对照土壤下降了6.26、18.26、15.06和15.07个百分点。地表径流量分别增加了,辽东栎林34.299mm(603%)和15.816mm(525%);油松林14.593mm(732%)和10.584mm(1321%);混交林12.004mm(181%)和7.275mm(364%);华北落叶松林3.555mm(118%),3.275mm(229%)。96年生长季,各土壤流失量分别增加了:油松林172.751t/hm~2(124倍);辽东栎林836.500t/hm~2(119倍);混交林172.499t/hm~2(47倍);华北落叶松林11.557t/hm~2(11倍)。表层土壤容重分别增加了:油松林15.0%和20.6%,辽东栎林18.4%和28.2%,混交林11.5%和38.5%,华北落叶松林4.3%和17.1%。 0-60cm深度土壤容重平均值的大小顺序为:草地>灌丛>辽东栎林>油松林>混交林>华北落叶松林;而土壤孔隙度的大小顺序为华北落叶松林>混交林>油松林>辽东栎林>灌丛>草地。两个生长季为土壤实际储水量的均值:油松林,124.45mm,78.62mm;辽东栎林,131.23mm,87.72mm;混交林,180.41mm,113.90mm;华北落叶松林,165.53mm,127.95mm;灌丛,172.50mm,89.81mm;草地,152.92mm,89.59 mm分别比干旱年份97年高出45.83mm、43.51mm、51.63mm、37.58mm、82.69mm和63.33mm。两个生长季的地表径流量为草地,30.930mm(2.79%);灌丛,16.321mm(147%);油松林,2.911mm(0.26%);辽东栎林,8.703mm(0.78%);混交林,8.625mm(0.78%);华北落叶松林,4.447mm(0.40%)。油松林、混交林和华北落叶松林地表径流量与降水量P(mm)和最大雨强(mm/h)正相关显著;而辽东栎林、灌丛和草地的地表径流量则与降水量P(mm)、平均雨强Q(mm/hr)和最大雨强M(mm/hr)三者之间呈显著正相关关系。与草地相比(1220.093kg/hm~2,100%),灌丛、辽东栎林、混交林、油松林和华北落叶松林96年生长季的土壤流失量分别降低了85.05%、94.26%、96.99%、98.86和99.14%。 降水量是影响小流域径流量时间变化的主要因素;南沟和马牙石沟96年的径流量分别是97年的8.19倍和7.87倍,而径流深(46.25mm,52.75mm)分别比97年(5.65mm,6.70mm)高出40.60mm和46.05mm。两个小流域由于面积的差异而使南沟两年的径流量分别比马牙石沟高出2773.136m~3(13.15%)和235.434m~3(8.79%)。96年和97年马牙石沟径流深比南沟高出6.5mm(14.05%)和1.05mm(18.58%)。在地处大陆性季风气候区的东灵山地区,用0.010m~3/min/km~2/hr能较好地分割小流域的洪峰和基流。在五次暴雨水文曲线中,马牙石沟的快速径流量分别比南沟高出25.00%到143.33%。五次洪水水文响应R的平均值南沟为0.218%,马牙石沟为0.404%;与海洋性气候地区相比,东灵山地区小流域的R值要低一到两个数量级。马牙石沟洪峰流量Qp的平均值为418.772L/min要比南沟(281.191L/min)大48.9%。东灵山地区小流域的洪水径流过程可分为三种类型。

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This report of the cruise along the Sofala Bank (Mozambique) describes the catch composition and catch distributions of the shallow water shrimp. Biological data are given for Penaeus indicus and Metapenaeus monoceros which represent 77% of the total catch.

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Catch composition and bathymetric distribution of demersal fish caught along the coast of Mozambique between parallels 16 degree 20' and 19 degree 30' S at depths of 11 to 180 metres are given. The shrimp by-catch was also studied.

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This report of the research cruise (7 to 23 June 1981) surveying pelagic marine resources of the Sofala Bank (Mozambique) describes the size composition, distribution, length-weight relationships and sex-ratio of the fish captured. Decapterus russellii, D. macrosoma, Selar crumenophthalmus and Rastrelliger kanagurta represented 21.7% of the total catch. The by-catch was also studied.

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Three short-chain neurotoxins named NT-I, NT-II, and NT-III were purified from the venom of Naja kaouthia, a snake distributed throughout the south of Yunnan province, China, by a series of chromatographic steps, including an FPLC Resource S column. Their molecular weights, determined by matrix-assisted laser desorption ionization time-of-flight (MALDI-TOF) MS, were 6952.19 Da, 6854.92 Da, and 6828.80 Da, respectively. NT-I consisted of 62 amino acid residues, and the other two consisted of 61 amino acid residues, including 8 cysteines. After hydrolysis by endoproteinase Glu-C, their primary sequences were determined. A test of their activities demonstrated that they effectively inhibited muscle contractions induced by electric stimulation. Furthermore, the extent of inhibition caused by NT-II and NT-III was less than that of NT-I. The IC(50)s were 0.04 mug/ml, 0.20 mug/ml, and 0.23 mug/ml for NT-I, NT-II, and NT-III, respectively. Compared with NT-II and NT-III, the higher activity of NT-I may be a result of the amino acid residue substitution Ile36 to Arg36.

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