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1.
潮棕壤不同利用方式下植物线虫垂直分布研究(英文) 总被引：4，自引：0，他引：4
2003 年11 月,在中国科学院沈阳生态实验站潮棕壤经过不同利用方式后对水稻田、玉米地、撂荒地和林地开展了植物线虫垂直分布(0–15 cm 各土层)特征研究。研究结果表明:不同土地利用方式下的某些优势属线虫随着土壤深度增加而呈下降趋势。螺旋属(Helicotylenchus)线虫是4 种土地利用方式中最优势的属。水田丝尾属(Filenchus)、平滑属(Psilenchus)和垫刃属(Tylenchus)线虫主要分布在上层(0–20 cm),而撂荒地、林地中的针属(Paratylenchus)线虫及玉米地中的短体属(Pratylenchus)线虫能够分布在更深的土层(0–80 cm)。本研究揭示,植物线虫优势属数量与土壤化学特性指标存在显著相关关系。不同利用方式螺旋属线虫数量与土壤C/N 比、全碳、全氮、全磷、碱解氮及Olsen-P含量呈显著正相关;水田丝尾属和平滑属线虫、玉米地短体属线虫、撂荒地针属线虫与土壤pH 程显著负相关,与土壤全碳、全氮及碱解氮呈显著正相关。为了更正确地评价植物线虫种群数量,有必要根据植物线虫优势属的垂直分布特征来确定取样深度。图1 表1 参21。 相似文献
2.
Vertical variation and storage of nitrogen in an aquic brown soil under different land uses 总被引：3，自引：0，他引：3
The vertical variation and storage of nitrogen in the depth of 0–150 cm of an aquic brown soil were studied under 14 years
of four land use patterns, i.e., paddy field, maize field, fallow field and woodland in Shenyang Experimental Station of Ecology,
Chinese Academy of Sciences in November of 2003. The results showed that different land uses had different profile distributions
of soil total nitrogen (STN), alkali N, ammonium (NH4
+-N) and nitrate (NO3
−-N). The sequence of STN storage was woodland>maize field>fallow field>paddy field, while that of NO3
−-N content was maize field>paddy field>woodland>fallow field, suggesting the different root biomass and biological N cycling
under various land uses. The STN storage in the depth of 0–100 cm of woodland averaged to 11.41 t·hm−1, being 1.65 and 1.25 times as much as that in paddy and maize fields, respectively, while there was no significant difference
between maize and fallow fields. The comparatively higher amount NO3
−-N in maize and paddy fields may be due to nitrogen fertilization and anthropogenic disturbance. Soil alkali N was significantly
related with STN, and the correlation could be expressed by a linear regression model under each land use (R
2≥0.929,p<0.001). Such a correlation was slightly closer in nature (woodland and fallow field) than in agro ecosystems (paddy and maize
fields). Heavy N fertilization induced an excess of crop need, and led to a comparatively higher amount of soil NO3
−-N in cultivated fields than in fallow field and woodland. It is suggested that agroforestry practices have the potential
to make a significant contribution to both crop production and environment protection.
Foundation item: The project was supported by the Knowledge Innovation Program of Chinese Academy of Sciences (KZCX2-413-9) and Fund of Shenyang
Experimental Station of Ecology, CAS (STZ0204)
Biography: ZHANG Yu-ge, (1968-), female, Ph.D. candidate, associate research fellow in Institute of Applied Ecology, Chinese Academy
of Sciences, Shenyang 110016, P.R. China.
Responsible editor: Song Funan 相似文献
3.
The impacts of elevated atmospheric CO2 concentrations (500 μmol·mol−1 and 700 μmol·mol−1) on total soil respiration and the contribution of root respiration ofPinus koraiensis seedlings were investigated from May to October in 2003 at the Research Station of Changbai Mountain Forest Ecosystems, Chinese
Academy of Sciences, Jilin Province, China. After four growing seasons in top-open chambers exposed to elevated CO2, the total soil respiration and roots respiration ofPinus koraiensis seedlings were measured by a Li-6400-09 soil CO2 flux chamber. Three PVC cylinders in each chamber were inserted about 30 cm into the soil instantaneously to terminate the
supply of current photosynthates from the tree canopy to roots for separating the root respiration from total soil respiration.
Soil respirations both inside and outside of the cylinders were measured on June 16, August 20 and October 8, respectively.
The results indicated that: there was a marked diurnal change in air temperature and soil temperature at depth of 5 cm on
June 16, the maximum of soil temperature at depth of 5 cm lagged behind that of air temperature, no differences in temperature
between treatments were found (P>0.05). The total soil respiration and soil respiration with roots severed showed strong diurnal and seasonal patterns. There
was marked difference in total soil respiration and soil respiration with roots severed between treatments (P<0.01); Mean total soil respiration and contribution of root under different treatments were 3.26, 4.78 and 1.47 μmol·m−2·s−1, 11.5%, 43.1% and 27.9% on June 16, August 20 and October 8, respectively.
Foundation item: This study was supported by the Knowledge Innovation Project of the Chinese Academy of Sciences (KZCX1-SW-01) and the National
Natural Science Foundation of China (30070158).
Biography: LIU Ying (1976-), female, Ph. D. Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, P. R. China.
Responsible editor: Song Funan 相似文献
4.
杉木纯林、混交林土壤微生物特性和土壤养分的比较研究 总被引：6，自引：0，他引：6
本文于2005年5月份,在中国科学院会同森林生态实验站选择了一块15年生的杉木纯林和两块15年生杉阔混交林作为研究对象,调查了林地土壤有机碳、全氮、全磷、硝态氮、有效磷和土壤微生物碳、氮、磷、基础呼吸以及呼吸熵,比较了纯林和混交林土壤微生物特性和土壤养分.结果表明,杉阔混交林的土壤有机碳、全氮、全磷硝态氮和有效磷含量高于杉木纯林;在混交林中,土壤微生物学特性得到改善.在0(10 cm和10(20 cm两层土壤中,杉阔混交林土壤微生物氮含量分别比杉木纯林高69%和61%.在0(10 cm土层,杉阔混交林土壤微生物碳、磷和基础呼吸分别比杉木纯林高11%、14%和4%;在10(20 cm土层,分别高6%、3%和3%.但是,杉阔混交林土壤微生物碳:氮比和呼吸熵较杉木纯林低34%和4%.另外,土壤微生物与土壤养分的相关性高于土壤呼吸、微生物碳:氮比和呼吸熵与土壤养分的相关性.由此可知,在针叶纯林中引入阔叶树后,土壤肥力得以改善,并有利于退化森林土壤的恢复. 相似文献
5.
为评价我国北方大规模人工造林对土壤磷素转化及磷素有效性的影响,对半干旱沙地樟子松人工林和天然植被(疏林草地)不同层次(0～5 cm, 5～20 cm)土壤中不同形态磷组分和磷酸单酯酶活性进行了比较.结果表明:除人工林土壤中活性有机磷不受土壤深度影响外,各样地表层土壤中各种磷素含量和酶活性均显著高于低层土壤,但分层效应在人工林中低于疏林草地;与疏林草地土壤相比,除Al-P外,人工林土壤中各种磷素绝对含量和酶活性均显著降低,总有机磷和Ca-P在全磷中的比例显著下降,而活性磷,Al-P和Fe-P占全磷的比例增加.可见表层土壤是磷素转化最活跃的区域,凋落物分解是土壤磷的主要来源;用樟子松进行人工造林促进了有机磷的矿化和Ca-P的溶解,提高了土壤磷素的有效性,同时导致土壤总磷库逐渐耗竭.要维持该人工防护林功能和稳定性,必须对地被物予以保护,并进行适当施肥.表3参38. 相似文献
6.
Soil samples were taken from depth of 0–12 cm in the virgin broad-leaved/Korean pine mixed forest in Changbai Mountain in
April, 2000. 20 μL·L−1 and 200 μL·L−1 CH4 and N2O concentration were supplied for analysis. Laboratory study on CH4 oxidation and N2O emission in forest soil showed that fresh soil sample could oxidize atmospheric methane and product N2O. Air-dried soil sample could not oxidize atmospheric methane, but could product N2O. However, it could oxidize the supplied methane quickly when its concentration was higher than 20 μL·L−1. The oxidation rate of methane was increased with its initial concentration. An addition of water to dry soil caused large
pulse of N2O emissions within 2 hours. There were curvilinear correlations between N2O emission and temperature (r2=0.706, p<0.05), and between N2O emission and water content (r2=0.2968, p <0.05). These suggested temperature and water content were important factors controlling N2O emission. The correlation between CH4 oxidization and temperature was also found while CH4 was supplied 200 μL·L−1 (r2=0.3573, p<0.05). Temperature was an important factor controlling CH4 oxidation. However, when 20 μL·L−1 CH4 was supplied, there was no correlation among CH4 oxidization, N2O emission, temperature and water content.
Foundation item: This paper was supported by Chinese Academy of Sciences.
Biography: ZHANG Xiu-jun (1960-), female, Ph. Doctor, lecture in Laboratory of Ecological Process of Trace Substance in Terrestrial
Ecosystem, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110015, P.R. China.
Responsible editor: Song Funan 相似文献
7.
土壤温度和水分对长白山3种温带森林土壤呼吸的影响 总被引：7，自引：0，他引：7
为了研究土壤温度和土壤含水量对阔叶红松林(山地暗棕壤)、云冷杉暗针叶林(山地棕针叶林土壤)和岳桦林(生草森林土)的土壤呼吸的影响,于2001年9月在长白山进行了土壤实验。利用增加土壤样柱的含水量,将土壤含水量分为9%,、21%、30%、37%和43%5个等级,土壤样品分别在0、5、15、25和35 的温度下保持24小时。阔叶红松林土壤在0~35 范围内,土壤呼吸速率与温度呈正相关。在一定的含水量范围内(21%~37%),土壤呼吸随含水量的增加而升高,当含水量超出该范围,土壤呼吸速率则随含水量的变化而降低。土壤温度和水分对土壤呼吸作用存在明显的交互作用。不同森林类型土壤呼吸作用强弱存在显著差异,大小顺序为阔叶红松林>岳桦林>云冷杉暗针叶林.红松阔叶林土壤呼吸作用的最佳条件是土壤温度35 ,含水量37%;云冷杉暗针叶林下的山地棕色针叶土壤呼吸作用的最佳条件是25 ,21%;岳桦林土壤呼吸作用的最佳条件是35 ,含水量37%。但是,由于长白山阔叶红松林,云冷杉林和岳桦林处在不同的海拔带上,同期不同森林类型土壤温度各不相同,相差4~5 ,所以野外所测的同期的山地棕色针叶林土呼吸速率应低于暗棕色森林土呼吸速率,山地生草森林土呼吸速率应高于山地棕色针叶林土的呼吸速率。图2表1参25。 相似文献
8.
Responses of soil microbial activities to elevated CO2 in experiment sites ofPinus sylvestriformis andPinus koraiensis seedlings were studied in summer in 2003. The results indicated the number of bacteria decreased significantly (p<0.05) under elevated CO2 forPinus sylvestriformis andPinus koraiensis. Amylase and invertase activities in soil increased forPinus sylvestriformis and decreased forPinus koraiensis with CO2 enrichment compared with those at ambient (350 μmol·mol−1). The size of microbial biomass C also decreased significantly at 700 μmol·mol−1 CO2. Bacterial community structure had some evident changes under elevated CO2 by DGGE (Denaturing Gradient Gel Electrophoresis) analysis of bacterial 16S rDNA gene fragments amplified by PCR from DNA
extracted directly from soil. The results suggested that responses of soil microorganisms to elevated CO2 would be related to plant species exposed to elevated CO2.
Foundation item: The study was supported by Major State Basic Research Development Program of China (2002CB412502) and the Knowledge Innovation
Project from Chinese Academy of Sciences (KZCX1-SW-01-03).
Biography: JIA Xia (1975), female, Ph. D. candidate of Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016,
P. R. China.
Responsible editor: Song Funan 相似文献
9.
In order to clarify the effects of a mixture of deciduous broad-leaved trees on soil fertility, we investigated litter biomass
accumulation, mineral soil chemical and physical characteristics, characteristics of nitrogen mineralization, and the mutual
relationships between them in Japanese cypress (Chamaecyparis obtusa) stands mixed with deciduous broad-leaved trees at different ratios (mixture ratio; MR = 0, 16, 33, 43, 100% by basal area)
in the northern Kanto region of Japan. Litter biomass in the forest floor and mineral soil was 19.1 Mg ha−1 in MR 0% and decreased approximately 60 % in MR 33%, MR 43% and MR100%. The permeability at 0–5 cm soil depth in MR100% was
twice as much as that in MR 0%. Increases in soil permeability were likely due to larger soil pores in the higher MR with
much accumulated deciduous broad-leaves. At 0–5 cm soil depth, the differences in carbon concentration among the plots were
not clear. On the other hand, carbon concentrations at 5–10 cm depth increased from 90 g kg−1 to 147 g kg−1 with increases in MR from 0% to 100%. Concentrations of exchangeable bases increased two to four times with increases in
MR from 0 to 100% at 0–10 cm depth. Soil pH (H2O) generally increased with increases in MR at each depth. The rates of net nitrogen mineralization at 0–5 cm depthin vitro increased from 25 to 87 mg kg−1 2 weeks−1 with increases in MR from 0 to 100%. However, increases in nitrification with increases in MR were not clear compared with
nitrogen mineralization. These results indicated that a mixture of deciduous broad-leaved trees in a Japanese cypress stand
was effective in preventing soil fertility decline.
This study was supported by a grant from the Showa Shell Sekiyu Fundation for Promotion of Environmental Research. A part
of this study was presented at the 7th International Congress of Ecology (1998). 相似文献
10.
To access the process of nitrogen mineralization in soil, the buried-bag technique was used among traditional agroforestry systems in the Bhabhar belt of Kumaun Himalaya. The present study, determined the relationship between various parameters of N-mineralization with agroforestry systems, seasons and soil depths. Season and soil depth have significantly (p?<?0.001) affected the process of ammonification, nitrification and net N-mineralization. The soil ammonium-N pool was comparatively higher than the nitrate-N pool. Highest amount of ammonium and nitrate-N were recorded in the agri-horticulture (AH) system, and lowest in the agri-horti-silviculture (AHS) system. Among the systems, highest amount of inorganic-N (ammonium?+?nitrate) was recorded during rainy season while, lowest during winter season. The highest ammonification rate (6.47?±?1.47 mg kg?1 month?1) was observed in agri-silviculture system and lowest (5.67?±?1.68 mg kg?1 month?1) in AHS system, while nitrification value was maximum (2.53?±?0.40 mg kg?1 month?1) in AH system and minimum (2.23?±?0.37 mg kg?1 month?1) in AHS system. The values of net N-mineralization were ranged from 4.03?±?0.53 to 13.29?±?0.44 mg kg?1 month?1. The values of inorganic-N and net N-mineralization were significantly more (P?<?0.01) in the surface soil layer (0–20 cm) than the subsurface layers (20–40 cm and 40–60 cm). Nitrogen mineralization was negatively correlated with the soil pH and positively correlated with soil organic carbon and total soil nitrogen. Higher rate of N-mineralization in AHS system indicated rapid turnover of nitrogen due to soil management practices and suggested that the changes in agroforestry based land-use systems alter the process of net N-mineralization, nitrification and ammonification.
相似文献11.
Two-year-old seedlings ofPinus koraiensis, Pinus sylvestriformis andFraxinus mandshurica were treated in open-top chambers with elevated CO2 concentrations (700 μL·L−1, 500 μL·L−1) and ambient CO2 concentrations (350 μL·L−1) in Changbai Mountain from June to Sept. in 1999 and 2001. The net photosynthetic rate, dark respiration rate, ribulose-1,5-bisphosphate
carboxlase (RuBPcase) activity, and chlorophyll content were analyzed. The results indicated the RuBPcase activity of the
three species seedlings increased at elevated CO2 concentrations. The elevated CO2 concentrations stimulated the net photosynthetic rates of three tree species exceptP. sylvestriformis grown under 500 μL·L−1 CO2 concentration. The dark respiration rates ofP. koraiensis andP. sylvestriformis increased under concentration of 700 μL·L−1 CO2, out that ofF. mandshurica decreased under both concentrations 700 μL·L−1 and 500 μL·L−1 CO2. The seedlings ofF. mandshurica decreased in chlorophyll contents at elevated CO2 concentrations.
Foundation item: This paper was supported by the National Natural Science Foundation of China (No. 30070158). Knowledge Innovation Item of
Chinese Academy of Sciences (KZCX2-406) and “Hundred Scientists” Project of Chinese Academy of Sciences.
Biography: Zhou Yu-mei (1973-) Ph. Doctor, Assistant Research fellow Institute of Applied Ecology. Chinese Academy of Sciences. Shenyang
110016. P.R. China.
Responsible editor: Song Funan 相似文献
12.
Robinia pseudoacacia stands act as a typical ecological protection forest in hilly semi-arid area of China. Two fields of surface runoff were
separately set up inR. pseudoacacia stand and its clearcut area in the western Liaoning Province (18°50’–122°25’ E, 40°24’–42°34’ N) for measuring the characteristics
of runoff and sediment as well as soil moisture dynamics. Contractive analysis of the two land types showed that there existed
a significant difference in volumes of runoff and sediment between the sites ofR. pseudoacacia stand and its clearcut area. The runoff volume and sediment volume in clearcut are were much bigger than those inR. pseudoacacia stand, with an increase amount of 40%–177% for runoff and 180%–400% for sediment. Hydrograph of surface runoff of typical
rainfall showed that the peak value of runoff inR. pseudoacacia stand was decreased by 1.0–2.5×10−3m3·s−1 compared with that in its clearcut area, and the occurring time of peak value of runoff inR. pseudoacacia stand was 10–20 min later than that in its clearcut area. Harmonic analysis of soil moisture dynamics indicated that the
soil moisture inR. pseudoacacia stand was 2.3% higher than that in clearcut area, and the soil moisture both inR. pseudoacia stand and its clearcut area could be divided into dry season and humid season and varied periodically with annual raifall
precipitation. It was concluded thatR. pseudoacacia stand plays a very important role in storing water, increasing soil moisture, and reducing surface runoff and soil erosion.
Foundation item: This paper was supported by Chinese “863” Plan Water-Saving Agriculture (2002AA2Z4321), the Key Knowledge Innovation Project
(SCXZY0103), and The “Tenth-five” Plan of Liaoning Province (2001212001).
Biography: GAO Peng (1967-), male, Dr. candidate, associate professor of Institute of Applied Ecology, Chinese Academy of Sciences,
Shenyang 110016, P. R. China.
Responsible editor: Song Funan 相似文献
13.
WANG Qing-kui WANG Si-long 《林业研究》2006,17(3):197-200
Conversion of natural secondary broad-leaved forest to Cunninghamia lanceolata plantation is a common management practice in subtropical China. In this study, we compared soil physico-chemical properties, microbial biomass in one natural secondary broad-leaved forest and two C. lanceolata plantation sites to estimate the effects of forest conversion on soil microbial biomass at the Huitong Experimental Station of Forestry Ecology, Chinese Academy of Sciences. Concentrations of soil organic carbon, total nitrogen, NH4^＋-N and microbial biomass carbon and nitrogen were much lower under C. lanceolata plantations as compared to natural secondary broad-leaved forest. Soil microbial biomass C in the first and second rotation of C. lanceolata plantations was only 53%, 46% of that in natural secondary broad-leaved forest, and microbial biomass N was 97% and 79%, respectively. The contribution of microbial biomass C to soil organic C was also lower in the plantation sites. However, the contribution of microbial N to total nitrogen and NH4^＋-N was greater in the C. lanceolata plantation sites. Therefore, conversion of natural secondary broad-leaved forest to C. lanceolata plantation and continuous planting of C. lanceolata led to the decline in soil microbial biomass and the degradation of forest soil in subtropical China. 相似文献
14.
At present, our understanding of the dynamics of microbial biomass and soil N in silvopastoral systems is very limited. In
this paper, the effects of understorey management on soil microbial C and N, net N mineralization, and net nitrification were
studied in two seven-year-old radiata pine (Pinus radiata D. Don) – pasture systems, consisting of plots with and without ryegrass (Lolium perenne) as an understorey. Mini-plots (1 × 1 m) with animals excluded and herbage repeatedly clipped and removed were used for soil
sampling. Three mini-plots formed a transect at each of two positions: 0.9 and 3.5 m north of the tree rows. Measurements
were taken from July 1997 to June 1998 about once every 40 days. One composite sample was collected from each of two sampling
depths (0–10 and 10–20 cm) at each transect position on each sampling date. Temporal and spatial variability of N mineralization
rates and microbial biomass C and N was large. Net mineralization and nitrification rates were higher in the bare ground than
in the ryegrass plots for a major part of the year, particularly from late spring to early fall. Net N mineralization and
nitrification rates were higher in the 0–10 than in the 10–20 cm soil layers in both the ryegrass and bare ground treatments;
however, the depth effect on microbial biomass C and N was only significant in the ryegrass treatment. In the surface soil
layer, microbial biomass C and N were substantially greater in the ryegrass than in the bare ground plots. Soil microbial
properties and activities were closely linked to pasture root activities, soil depth, and site biophysical conditions.
This revised version was published online in June 2006 with corrections to the Cover Date. 相似文献
15.
Water is usally thought of a limiting factor for the restoration of semi-arid ecosystem. In the growing season of 2006, a study was conducted to determine the effects of modeling precipitation on seasonal patterns in concentrations of soil-available nitrogen and to describe the seasonal patterns in soil nitrogen availability and seasonal variation in the rates of net nitrogen mineralization of topsoil at Daqinggou ecological station in Keerqin sand lands, Inner Mongolia Autonomous Region, China. Manipulation of water （80 mm） was designed to be added to experiment plots of sandy grasslands in dry season. Water addition （W） treatment and control （CK） treatment were separately taken in six replications and randomly assigned in 12 plots （4 m×4 m for each） with 2-m buffers betweens. Results showed that the content of soil inorganic nitrogen and net nitrogen mineralization rate were not affected by adding water in sandy grassland of Keerqin sand lands. Net ni- trogen mineralization rates ranged from 0.5μg·g^-1,month^-1 to 4 μg.g^-1.month^-1. The highest values of soil inorganic nitrogen and net nitrogen mineralization occurred on October 15 in control plots. The seasonal changes of soil inorganic nitrogen contents exhibited ＂V＂ shape pattern that was related to seasonal patterns of soil ammonium-N （ascending trend） and nitrate-N transformation （descending trend）. 相似文献
16.
Distribution of ectomycorrhizas and ectomycorrhizal fungal inoculum with soil depth in a birch forest 总被引：2，自引：0，他引：2
The distributions of ectomycorrhizas and ectomycorrhizal fungal inoculum with soil depth (0–45 cm) were determined in a 40-year-oldBetula platyphylla var.japonica forest. Mycorrhizal and non-mycorrhizal fine roots were measured in each soil core sample that was collected at soil depths
of 0–5, 5–10, 10–15, 15–20, 20–25, 30–35, and 40–45 cm. The ectomycorrhizas were mainly distributed (>50%) in the top soil
(0–5 cm) of organic forest floor horizons. Below 5 cm the quantity of ectomycorrhizas decreased sharply. The percentage of
fine roots which were ectomycorrhizal gradually declined with the depth of soil. The ectomycorrhizal fungal inoculum was evaluated
by a bioassay method, measuring the lengths of the entire root system and of the ectomycorrhizal roots of birch seedlings
planted in each soil sample. The soil samples were collected from 0–5, 10–15, 20–25, 30–35, and 40–45 cm depths of the soil
profile. Ectomycorrhizal formation on birch seedling roots in the bioassay was high in both the soil depth intervals 0–5 cm
and 10–15 cm, while the amount was lower in the soil depth interval from 20–45 cm. The results of these investigations show
that the amount of the ectomycorrhizas in soil, and the ectomycorrhizal fungal inoculum potential as determined by bioassay,
are not always consistent with each other. 相似文献
17.
利用盆栽试验,研究施入不同比例的泥炭、风化煤对风沙土的改良作用及其促进樟子松幼苗生长的效果,并初步分析了两种有机物料的作用机理。试验结果表明,泥炭和风化煤都显著地改良了风沙土的理化性质,随着施入量的增加,两者对风沙土的影响都表现出土壤pH值下降、持水量增加、养分含量提高,且泥炭的效果普遍比风化煤的效果要好;两者均促进了樟子松幼苗生长。不同含量的泥炭对促进樟子松幼苗生长(苗高、地径、根长、生物量)的效果表现为8%>10%>5%>2%>0。不同含量的风化煤对高生长的影响依次是5%>8%>10%>2%>0,对地径生长的影响依次为5%>8%>2%>10%>0,对生物量的影响依次为5%>2%>8%>10%>0。总的来看,泥炭的效果比风化煤好。结合樟子松在沙地中的生长特性,推断泥炭和风化煤中含有微量抑制樟子松生长的物质,并提出8%的泥炭与风沙土之比是促进沙地樟子松幼苗生长的最佳配比。 相似文献
18.
ZHOULi LUOFeng-xia DAILi-min ZHANGHui-hua 《林业研究》2003,14(1):67-70
The fresh pollen vitality,the effect of different storage conditions on the pollen vitality,and the difference of vitality among the species of seven species of Syringa were determined in Shenyang,China.The results indicated that the pollen vitality (81.5%) of Syringa villosa was the highest among the seven tested species,followed by S.microphylla and S.meyeri,and that of S.oblata var.affinis was the lowest.The low temperature was the best condition for storage of pollen of Syringa,and the most proper temperature for the storage was 0-2℃.The storability of S.microphylla was the best of all,and it could be stored over 60 days at the temperature of 0-2℃,next was S.villosa and S.meyeri. 相似文献
19.
亚热带地区杉木人工林和阔叶林土壤活性有机质研究(英文) 总被引：1，自引：2，他引：1
土壤活性有机质对土壤养分如氮、磷、硫的生物化学循环具有作用,其含量和质量影响土壤的初级生产力。本试验在中国科学院会同森林生态实验站通过对第一代、第二代杉木纯林和地带性阔叶林土壤活性有机质组分的对比研究,发现杉木纯林土壤活性有机质的含量低于地带性阔叶林。第一代杉木纯林易氧化有机碳、微生物生物量碳、水溶性有机碳和水溶性碳水化合物的含量分别比第二代杉木纯林高35.9%、13.7%、87.8%和50.9%,比地带性阔叶林的低15.8%、47.3%、38.1%和30.2%。在调查的三种林地内,土壤微生物生物量碳和水溶性有机碳含量下降幅度较大,其次为水溶性碳水化合物,而易氧化有机碳的变化最小。同时,杉木纯林土壤养分等理化性质也比地带性阔叶林低。这表明在杉木纯林取代地带性阔叶林以及杉木纯林连栽后林地的土壤肥力降低。图3 表2参26。 相似文献