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1.
对黑龙江省东部山地白桦人工林生态系统的大气降水、穿透水、树干茎流和地表径流中的pH值、溶解氧、浊度、总溶解固体、电导率、氧化还原电位、K、Na、Ca、Mg、Cu、Zn、Mn和Fe等水质指标进行了测定.结果表明:大气降水经过白桦人工林生态系统后,浊度和总溶解固体值逐渐升高.穿透水除Ca元素外,其他化学元素含量均有不同程度的增加,化学元素含量排序为:K＞ Ca＞ Na＞ Mg＞ Mn＞ Fe ＞Zn＞ Cu.树干茎流中各化学元素含量排序为:K＞Ca＞Mg ＞Na＞Fe ＞Mn ＞Zn ＞Cu.地表径流中各化学元素含量为:K＞ Ca＞ Na＞ Mg＞ Fe＞ Mn＞ Zn＞ Cu.除Na、Ca元素外,大气降水中其他元素的变异系数均较大.穿透水和树干茎流中Cu元素的变异系数大于其他元素,地表径流中Zn元素的变异系数最大.根据淋溶系数的大小排列,穿透水中各化学元素的淋溶序列是:Mn＞K＞Mg＞Fe＞Cu ＞Zn＞ Na＞ Ca.树干茎流中各化学元素的淋溶序列是:K ＞Mn＞ Mg＞ Fe ＞Cu ＞Zn＞ Ca＞ Na.经过淋洗后,穿透水和树干茎流中K和Mg元素增加较多,Ca元素出现负淋溶. 相似文献
2.
在2001年森林生长季(6-9月),通过测量降雨各分量,分析了中国吉林省长白山北坡红松阔叶林冠层对降水分配各分量的影响。结果表明:干流量(37.39 mm),透流量(326.02 mm)和截留量(105.67 mm),分别占同期降雨量(469.08 mm) 的7.97%、69.50%和22.53%。林冠对降雨的月份分配规律是:树干茎流率的月变化为七、八月份大于其它月份,穿透率从6-9月份有逐渐减少的趋势,而截留率的变化正好与穿透率相反,从19.43%增加到31.02%。林内降雨中的养分元素浓度发生显著变化,除Ca、Mg外,其它元素的浓度都有所增加。经分析得出,大气降雨中养分元素的浓度序列为:Ca> Mg> N> K> Fe > P> Cu > Mn;而穿透雨中养分元素的浓度序列为:K>N>Mg>Ca>P>Fe>Mn>Cu;在林冠淋溶中各养分元素的浓度序列为:Mn> P>K>Cu>Fe>N>Mg>Ca。图1表5参13。 相似文献
3.
The effect of forest type on atmospheric nutrient inputs to the forest ecosystem was measured for individual storm events for 1 year in three East Texas forest types: beechmagnolia, pine-mixed hardwoods and loblolly pine plantation. Total annual bulk precipitation inputs (kg/ha) for Ca, Mg, N, K and Na were, respectively: 5.0, 1.1, 4.1, 3.3 and 9.9. Total througfall inputs were increased by forest type, but the magnitude differed with each nutrient. Over of the total K and the total Mg throughfall input were due to the forest canopy. However of the Ca and most of the Na throughfall input resulted from bulk precipitation. Although stemflow nutrient concentrations (ppm) were higher than throughfall and bulk precipitation, total annual stemflow nutrient inputs were only a minor component of the loblolly pine plantation ecosystem. 相似文献
4.
《Scandinavian Journal of Forest Research》2012,27(1-4):446-456
The dynamics of three major mineral nutrients (K, Ca, Mg) and six heavy metals (Fe, Mn, Zn, Cu, Pb and Cd) were studied in decomposing natural, unpolluted litter in two forest types: Scots pine needle litter in a pure Scots pine forest and oak‐hornbeam leaf litter in a mixed oak‐hornbeam stand. Of the mineral nutrients, only K in the oak‐hornbeam system showed a significant decrease in concentration during the course of litter decomposition. For Ca and Mg in both systems and for K in the Scots pine system no clear relation between concentration and accumulated litter‐mass loss was observed. On the other hand, for Fe, Zn, Pb and Cd at both sites, as well as for Mn in the oak‐hornbeam stand and Cu in the Scots pine stand highly significant positive relations were found between heavy metal concentrations and accumulated mass loss. A decrease in concentration was noted only in the case of Mn in the Scots pine system. No clear pattern was found for Cu in the oak‐hornbeam stand. Concentrations of heavy metals in the decomposing litter reached levels at or above those reported to retard decomposition in other studies. At the oak‐hornbeam stand increased also the absolute amounts of Fe, Zn, Pb and Cd. 相似文献
5.
Retranslocation of N, P, K, Ca, Mg, Mn, Fe, Zn, Cu and Ni within the foliage of Scots pine (Pinus sylvestris L.) was studied during autumnal needle senescence along a heavy-metal pollution gradient in western Finland. The stands were located at distances of 0.5 (Har 0.5), 4 (Har 4) and 8 km (Har 8) to the southeast of a copper-nickel smelter at Harjavalta. A background study stand was located at H?meenkangas (H?m), 60 km northeast of the smelter. During needle senescence, the mobile nutrients N, P and K decreased by 67-88% and needle dry mass decreased by 31-43%. Retranslocation of P and K was less efficient in the stand nearest the smelter (Har 0.5) than in the other stands. During needle senescence at stand Har 0.5, heavy metal content either decreased slightly (Zn, Ni) or increased (Fe, Cu), whereas in the background study stand, retranslocation efficiency of Cu was 75%. Net throughfall (the amount of a nutrient in throughfall minus the amount in open precipitation) was higher in stand Har 0.5 than in stand Har 8 for all of the elements measured, except N and P which were intercepted by the canopy. In stand Har 8, deposition of S, Cu and Ni was intercepted by the canopy, and net throughfall of Fe and Zn was very low. In contrast, S and heavy metal contents of net throughfall in stand Har 0.5 were greater than the decrease in these elements in the needles indicating that accumulation on needle surfaces and subsequent wash-off accounted for a major part of the fluxes. Furthermore, the Cu content in net throughfall during the senescence period was higher than the original Cu content of the needles in July, providing additional evidence that much of the needle Cu content was comprised of dry deposits of Cu on the needle surface. 相似文献
6.
A. M. O''Connell 《Forest Ecology and Management》1985,10(4):283-296
Nutrient accessions to the forest floor in rainfall, throughfall and stemflow from the understorey and tree strata were measured in karri (Eucalyptus diversicolor F. Muell.) forest of south-west Western Australia. These data, for stands aged 2, 6, 9, and 40 years and for mature forest, were compared with annual accessions of nutrients in litterfall.
With increasing age of the stands, the concentration and amounts of Ca, K, Mg, Na and Cl in throughfall increased. The amounts of Mg, Na and Cl in stemflow from the overstorey were also greatest in the older stands. Although concentrations of nutrients in stemflow from the tree stratum were higher than from the understorey, the quantities of nutrients transported to the forest floor in stemflow from the understorey were greater because of its greater volume.
Rainfall is the major source of Na (64–91%) and Cl (51–79%) and it also contributes significantly to Mg (19–50%) accessions. Of the nutrient pathways between canopy and forest floor, litterfall accounts for the largest proportion of N (89–93%), Ca (80–87%) and P (67–79%) recycled in the karri forest. About equal amounts of K are transferred in litterfall, throughfall and stemflow with approximately 80% of stemflow K originating from the understorey strata. 相似文献
7.
Throughfall and stemflow measurements in a 60-year-old white oak stand (Quercus serrata Thunb.) were carried out during two periods totalling eleven months, from August to November 1993 and from May to November
1994, in order to clarify the rainfall partitioning of this forest. Troughs and spiral-type stemflow gauges connected to tipping
bucket-gauges were used for throughfall and stemflow measurements. Seventy-five storms were analyzed individually. Coefficients
of variation for throughfall and stemflow ranged between 5–25% and 20–70% respectively. Partitioning of net rainfall in throughfall
and stemflow represent 72% and 10% of the gross rainfall respectively. Multiple regression analyses were carried out to determine
the stemflow variability. In was determined that maximum rain intensity was highly correlated with stemflow and this variable
explained a further 5.5% of the stemflow variation. Estimates of averaged lag time and drainage after rain cease for stemflow
were 290 and 164 min, while estimates for throughfall were 60 and 104 min. respectively. The canopy saturation was estimated
from continuous storms and showed a value of 0.6 mm. The trunk storage capacity was estimated at a value of 0.2 mm. The interception
loss from the forest canopy was estimated in 18%. Interception loss was heighly correlated with rainfall characteristics such
as duration and intensity. 相似文献
8.
《林业研究》2017,(3)
Stemflow is a focused point source input of precipitation and nutrients at the base of a tree or plant and can have a significant impact on site hydrology. To date, no known studies have modelled stemflow production for juvenile lodgepole pine(Pinus contorta var. latifolia).Meteorological conditions, tree characteristics, and stemflow were sampled for two juvenile lodgepole pine stands over the course of the 2009 growing season. Step-wise multiple regression was used to assess which meteorological and tree architecture variables influenced stemflow production for each research plot. Once predictor variables were identified, models were produced for each stand and a generic model was produced that applied to both plots. A model employing precipitation depth and crown projection area successfully explained 71.3% of the variation in stemflow production from sampled trees. Stemflow was found to represent 1.8% of the study period rainfall and,although not a large component of the plot-scale canopy water balance, it is an order of magnitude greater than the fractioning of stemflow from mature lodgepole and lodgepole pine dominated forest. Additionally, stemflow funnelling ratios were found to average 22.2 and 24.3 from the two sample plots over the study period with a single tree, single event maximum of 111.7 recorded for a tree with a 3.3 cm bole diameter and a rain depth of 17.4 mm. 相似文献
9.
Roger F. Walker Robert M. Fecko Dale W. Johnson Watkins W. Miller 《Journal of Sustainable Forestry》2013,32(5):482-541
An investigation of wildfire effects on mineral nutrition of Jeffrey pine (Pinus jeffreyi Grev. & Balf.) along with species comparisons of the nutrition of unburned specimens of this pine to those of unburned California white fir (Abies concolor var. lowiana [Gord.] Lemm.) were conducted in an eastern Sierran mixed conifer stand. Foliar Fe and Mn concentrations were frequently higher and Al was consistently so in burned than in the unburned pine as assessed in six sampling periods distributed over more than two postfire growing seasons while base cation/metallic element molar ratios consisting of Ca/Al, K/Al, K/Mn, Ca/Fe, Mg/Fe, K/Fe, and Ca/Zn were often lower in the former. Foliar N, P, Fe, Zn, and Cu were frequently higher in unburned pine than unburned fir while the reverse proved true concerning K, Ca, Mn, B, and Al; and likewise several molar ratios involving Al and Mn were higher in the former while several involving Fe, Zn, and Cu were higher in the latter. At midstudy, mineral soil in the burned stand portion had lower K but higher S, Mn, and Zn than that in the unburned portion, and the former had several molar ratios that were lower as well. 相似文献
10.
11.
Interception loss was measured indirectly for 3 years in adjacentunthinned 25-year-old stands of Sitka spruce and lodgepole pineand for 2 years in a 63-year-old selectively thinned stand ofSitka spruce. For each stand measurements were made of grossprecipitation, throughfall and stemflow. Interception loss wasderived by subtracting the sum of throughfall and stemflow (netprecipitation) from gross precipitation. For the years 1977–78, 1978–79 and 1979–80,interception losses in the pole-stage Sitka spruce were 32,28 and 27 per cent of gross precipitation respectively whilethose in the lodgepole pine were 33, 29 and 26 per cent. For1979–80 and 1980–81 interception losses in the matureSitka spruce were 44 and 53 per cent of gross precipitation.The average interception loss was 29 per cent for both pole-stagecrops and 49 per cent for mature Sitka spruce. The proportions of net precipitation reaching the ground asstemflow and throughfall were 0.18 and 0.82 respectively forthe pole-stage Sitka spruce, 0.14 and 0.86 for the pole-stagelodepole pine and 0.02 and 0.98 for the mature Sitka spruce. 相似文献
12.
Stemflow is a focused point source input of precipitation and nutrients at the base of a tree or plant and can have a significant impact on site hydrology. To date, no known studies have modelled stemflow production for juvenile lodgepole pine (Pinus contorta var. latifolia). Meteorological conditions, tree characteristics, and stemflow were sampled for two juvenile lodgepole pine stands over the course of the 2009 growing season. Step-wise multiple regression was used to assess which meteorological and tree architecture variables influenced stemflow production for each research plot. Once predictor variables were identified, models were produced for each stand and a generic model was produced that applied to both plots. A model employing precipitation depth and crown projection area successfully explained 71.3% of the variation in stemflow production from sampled trees. Stemflow was found to represent 1.8% of the study period rainfall and, although not a large component of the plot-scale canopy water balance, it is an order of magnitude greater than the fractioning of stemflow from mature lodgepole and lodgepole pine dominated forest. Additionally, stemflow funnelling ratios were found to average 22.2 and 24.3 from the two sample plots over the study period with a single tree, single event maximum of 111.7 recorded for a tree with a 3.3 cm bole diameter and a rain depth of 17.4 mm. 相似文献
13.
贵州都匀马尾松种子园针叶DRIS营养诊断分析 总被引：1，自引：0，他引：1
通过对都匀1．5代无性系种子园20年生马尾松针叶中N、P、K、Ca、Mg、Cu、Zn、Fe、Mn、B等营养元素含量变化的测定和分析,初步筛选出N／P、K／N、Ca／N、Mg／N、N／Cu、zn／N、N／Fe、K／P、Ca／P、P／Mg、P／Cu、P／Zn、Fe／P、K／Ca、K／Mg、K／Cu、K／Zn、Fe／K、Ca／Mg、Ca／Cu、Ca／Zn、Fe／Ca、MgJCu、Zn／Mg、Fe／Mg、Zn／Cu、Fe／Cu、Fe／Zn共28对元素比值为重要参数,对贵州都匀马尾松种子园针叶作DRIS营养诊断分析。结果表明,该地区马尾松针叶内Mn含量过高,平均值为767．01mg／kg,而B含量较低,仅为12．95mg／kg,马尾松的需肥顺序为Cu〉P〉Zn〉Mg〉Ca〉N〉K〉Fe。 相似文献
14.
百山祖冷杉枝叶主要营养元素特征分析 总被引：1，自引：1，他引：0
应用原子吸收光谱法测定了百山祖冷杉枝和针叶中K、Na、Cu、Ca、Zn、Fe、Mg、Mn 8种营养元素的含量,结果表明,百山祖冷杉枝和针叶中均含有所测的K、Cu、Ca、Zn、Fe、Mg、Mn等元素,但未检出Na元素;其含量为CaKMgZnFeMnCuNa。与大多数植物体正常生长发育的元素含量范围值相比较,百山祖冷杉枝和针叶中K含量分别为2 967.68~5 585.95、4 036.13~5 194.30 mg/kg,均低于临界值,针叶中Cu含量2.58~4.70 mg/kg,略低于一般植物水平,枝部Zn、Mn含量及针叶Mn含量则均处于较高水平。 相似文献
15.
紫金山麻栎林降水分配格局研究 总被引：1，自引：0，他引：1
对紫金山栎林林冠截留、树干茎流与降水量之间的关系进行了研究。在观测的46场降水中,降水量达823.8 mm,林冠总截留量、树干茎流量和穿透雨量分别为207.95 mm、33.30 mm、582.55 mm,林冠截留率、树干茎流率和穿透率分别为25.24%、4.04%、70.71%。随着降水量的增大,林冠截留量、树干茎流量、穿透雨量及穿透率都有所增加,林冠截留率降低,树干茎流率在2～50 mm降水量级中逐渐增大,在>50 mm降水量级有所降低。林冠截留量与降水量之间呈幂函数关系,而树干茎流量、穿透雨与降水量之间呈线性相关。 相似文献
16.
微波消解-ICP-OES法测定麻竹中12种矿质元素含量的实验 总被引：1，自引：0，他引：1
利用微波消解对麻竹叶进行前期处理,采用电感耦合等离子体发射光谱(ICP-OES)法测定竹叶中的12种元素含量。结果表明,该测定方法快速、准确、分析精度高;麻竹叶中所含的12种元素从高到低的排序为K、Ca、Mg、P、Mn、Al、Si、Na、Fe、Zn、Cr和Cu,其中,富含人体必需的Fe、Ca、Si等常量元素和Mn、Cu等微量元素,且K、Ca、Mg、P等元素的含量较高。本项实验建立了微波消解-ICP-OES法测定麻竹竹叶中的矿质元素的检测方法,麻竹叶中微量元素含量丰富。 相似文献
17.
18.
Genetic variation in branchlet nutrient (N, P, K, Na, Ca, Mg, Mn and Fe) concentrations and mineral concentration (sum of branchlet P, K, Na, Ca, Mg, Mn and Fe concentrations) of 8-9-year-old hoop pine (Araucaria cunninghamii Ait. ex D. Don) half-sib families was assessed for four canopy positions at a wet site (23 families) and two canopy positions at an N- and water-limiting dry site (22 families) in relation to tree growth and associated branchlet carbon (delta13C) and oxygen (delta18O) isotope composition in southeast Queensland, Australia. Branchlet nutrient and mineral concentrations varied significantly among families and with canopy position and site. Depending on the canopy position sampled, the hoop pine family effect accounted for 0 to 13.8% of the total variation in branchlet N concentration, and for 0 to 30.3% of the total variation in branchlet mineral concentration at the wet site. The corresponding values for the family effect at the dry site were 0-13.3% for branchlet N concentration and 0-25.7% for branchlet mineral concentration. There were significant variations in branchlet P, K, Ca and Mg concentrations at both sites, and these variations differed with canopy position. Relationships between family means of branchlet N concentration and tree growth or delta13C or delta18O varied with canopy position at both sites. At the wet site, there were significant positive correlations between branchlet mineral concentration in the upper-outer or upper-inner canopy and tree height (r = 0.26 and 0.37, P < 0.01) and between branchlet mineral concentration and delta13C (r = 0.24, P < 0.01) in the upper-inner canopy, and a significant negative correlation between branchlet mineral concentration and delta13C (r = -0.21, P < 0.05) in the upper-outer canopy. At the dry site, branchlet mineral concentrations in the upper-inner and upper-outer canopy were significantly correlated with branchlet delta13C (r = -0.28 and -0.51, P < 0.01), and branchlet N concentration in the upper-inner canopy was significantly correlated with tree growth (r = 0.29, P < 0.01). A significant correlation between branchlet delta18O (an index of stomatal conductance) and branchlet mineral concentration at the dry site (r = 0.39, P = 0.020) indicated that stomatal conductance might be a factor regulating the variation in branchlet mineral concentration of the hoop pine families. Both branchlet N concentration and mineral concentration at particular canopy positions assist in selecting hoop pine families with improved tree growth and N- and water-use efficiency in environments where both N deficiency and a limited water supply are major factors affecting plantation productivity. 相似文献
19.
对长宁竹海楠竹林、黄竹林、苦竹林、杉木林和栎林5种林分林冠降雨分配格局进行了对比。回归结果表明:穿透雨量和干流与林外降雨量呈线性关系,并都达到极显著水平(p-0.01)。在降雨量为1204.7 mm时,5种林分穿透雨的最小响应雨量分别为:斑苦竹(Pleioblastus amarus Kengf)林为3.0 mm,硬头黄竹(Bambusa rigida Keng et Kengf)林为1.0 mm、白栎(Quercus fabri Hance)林为0.9 mm、楠竹(Phyllostachy spubescen)林为0.8 mm、杉木(Cunninghamia lanceolata Hook)林为0.7 mm。干流量随树干胸径的增加而增大,两者关系可用Q=B0 B1D B2D2 B3D3进行描述。与其它的林种相比,竹林干流量远高于栎林和杉木林。苦竹林干流量达105.3 mm,干流率为8.74%,黄竹和楠竹干流量均为82.4 mm,干流率为6.84%,栎林分别为42.4 mm和3.49%,杉木林最小,仅为8.8 mm和0.73%。截留量和截留率从大至小的排序为:苦竹林为384.3 mm和31.9%,栎林355.5 mm和29.51%,黄竹280.7 mm和23.3%,楠竹274.1 mm和22.75%,杉木林254.8 mm和21.15%。 相似文献
20.
《Scandinavian Journal of Forest Research》2012,27(1-4):177-193
Temporal variation in nutrient concentrations of Scots pine (Pinus sylvestris L.) needles was studied during a three‐year period in three stands of differing stages of development. Concentrations of N, P and K varied significantly between years; this variation was related to differences in needle dry weight. Concentrations of all measured nutrients (N, P, K, Ca, Mg, Mn, Cu, Zn, Fe, B) and Al varied between seasons; this variation was related to nutrient mobility and the annual physiological cycle. Concentrations of the mobile nutrients N, P and K decreased in spring and early summer during shoot and needle elongation and increased in late summer and autumn during needle senescence and litterfall. Concentrations of Mg, Cu, Zn and B followed somewhat similar patterns. The poorly mobile nutrients Ca, Mn and Fe accumulated gradually in needles during each growing season. Needle nutrient concentrations were stable during the nonactive period. 相似文献