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1.
《地理学报(英文版)》2016,(4)
The capacity of soil and water conservation measures, defined as the maximum quantity of suitable soil and water conservation measures contained in a region, were determined for the Loess Plateau based on zones suitable for establishing terraced fields, forestland and grassland with the support of geographic information system(GIS) software. The minimum possible soil erosion modulus and actual soil erosion modulus in 2010 were calculated using the revised universal soil loss equation(RUSLE), and the ratio of the minimum possible soil erosion modulus under the capacity of soil and water conservation measures to the actual soil erosion modulus was defined as the soil erosion control degree. The control potential of soil erosion and water loss in the Loess Plateau was studied using this concept. Results showed that the actual soil erosion modulus was 3355 t·km~(–2)·a~(–1), the minimum possible soil erosion modulus was 1921 t·km~(–2)·a~(–1), and the soil erosion control degree was 0.57(medium level) in the Loess Plateau in 2010. In terms of zoning, the control degree was relatively high in the river valley-plain area, soil-rocky mountainous area, and windy-sandy area, but relatively low in the soil-rocky hilly-forested area, hilly-gully area and plateau-gully area. The rate of erosion areas with a soil erosion modulus of less than 1000 t·km~(–2)·a~(–1) increased from 50.48% to 57.71%, forest and grass coverage rose from 56.74% to 69.15%, rate of terraced fields increased from 4.36% to 19.03%, and per capita grain available rose from 418 kg·a~(–1) to 459 kg·a~(–1) under the capacity of soil and water conservation measures compared with actual conditions. These research results are of some guiding significance for soil and water loss control in the Loess Plateau. 相似文献
2.
《地理学报(英文版)》2016,(10)
Natural ecosystems provide human society with very important products and services. With the rapid increase in population and the over-exploitation of natural resources, humans are continually enhancing the production of some services at the expense of others. This paper estimates changes in ecosystem services, and the relationship between these services in the Guanzhong-Tianshui Economic Region of China. These ecosystem changes are of great significance to the sustainable development of this economic region. The concept of production possibility frontier(PPF) is applied to evaluate the trade-offs and synergy between carbon sequestration, water yield and soil retention. Three land use strategy scenarios – planning, exploitation and protection – are applied to evaluate potential changes in ecosystem services. This study reveals noticeable trade-offs between carbon sequestration, soil retention and water yield, with synergy between carbon sequestration and soil retention. There are synergies between carbon sequestration, water yield and soil retention in the three scenarios. The protection scenario is the most favourable land use strategy for regulating ecosystem service capacity. This scenario results in the highest carbon sequestration, water yield and soil retention. The results could have implications for natural capital and ecosystem services planning, management and land use decision-making. 相似文献
3.
中国水土保持研究回顾 总被引：1，自引：0，他引：1
The preservation and sustainable development of soil and water resources is one of the basic principles for the development of China. Throughout the course of history, all the social improvement and economic development are deeply concerned with soil loss and ecological environmental protection. It is now a common sense that soil and water conservation is the safety insurance for national ecology and its development. For the past long period of time, soil and water loss has been recognized as “the No. 1 killer“ to the ecological environment. The nation is on the stage of the critical conditions for its development. China has massive mountain and upland area with complicated geological conditions and accelerated human destruction and serious soil and water loss.Based on rich historical documents, renovating experience and detailed analysis of the data collected in field experiments and field surveys for soil and water conservation, this paper aims to review the general characteristics of soil and water loss, to explore the relationship between soil and water conservation and sustainable economic development, and to provide relevant strategies for soil and water conservation in China. 相似文献
4.
This paper focuses on the growth response of Caragana microphylla seedlings to changes of artificially controlled water table in Horqin Sandy Land, China. Monitoring results of soil water content shows that soil moisture is closely correlated to groundwater depths. Soil volumetric water increased rapidly when close to water sources and finally stabilized in a saturated state. The soil moisture trend of CK(control) increased gradually at 0–50 cm of soil depth then decreased to 4% below 50 cm soil depth. C. microphylla can adapt to different soil environments by changes in ecological and physiological characteristics. By comparing the ecological characteristics of C. microphylla seedlings at various water tables, we found that a shallow water table of 40 cm depth inhibited seedling growth because of weak ecological characteristics. A groundwater depth of 120 cm was more advantageous for plant height and canopy growth of C. microphylla seedlings. During the first two years, the most suitable water depth for root biomass was 120 cm, and 180 cm for root length. The growth of vertical roots is positively correlated with groundwater depth, and root thickness is the determinate factor for root biomass while the fine root is the determinate factor for root length. A thick root would grow much more in a natural drought environment while access to ground water promotes the growth of fine roots. 相似文献
5.
1 IntroductionIt is well known that the major problem of water resources at present is water shortage in the North China Plain. The development of agricultural production certainly increased the water consumption, so level of groundwater table declined year by year. Crop use water directly from soil water, while rainwater, surface water, and groundwater should be firstly transformed and changed into soil water and then be used by crops. Therefore, water interactions, water balance and soil w… 相似文献
6.
陕西黄土高原人工林土壤干层及形成原因 总被引：1，自引：0，他引：1
1 Introduction Abroad, a lot of research on soil water removal, seeping and evaporation has been done (Ole, 1998; Rapp, 2000). A seeping model of soil water was suggested (Yuin, 1998) and it was known that water removal is very slow in the unsaturated zon… 相似文献
7.
中国西北干旱内陆河流域分布式出山径流模型 总被引：1，自引：0，他引：1
In order to predict the futuristic runoff under global warming, and to approach to the effects of vegetation on the ecological environment of the inland river mountainous watershed of Northwest China, the authors use the routine hydrometric data to create a distributed monthly model with some conceptual parameters, coupled with GIS and RS tools and data. The model takes sub-basin as the minimal confluent unit, divides the main soils of the basin into 3 layers, and identifies the vegetation types as forest and pasture. The data used in the model are precipitation, air temperature, runoff, soil weight water content, soil depth, soil bulk density, soil porosity, land cover,etc. The model holds that if the water amount is greater than the water content capacity, there will be surface runoff. The actual evaporation is proportional to the product of the potential evaporation and soil volume water content. The studied basin is Heihe mainstream mountainous basin, with a drainage area of 10,009 km^2. The data used in this simulation are from Jan. 1980 to Dec. 1995, and the first 10 years‘ data are used to simulate, while the last 5 years‘ data are used to calibrate. For the simulation process, the Nash-Sutcliffe Equation, Balance Error and Explained Variance is 0.8681,5.4008 and 0.8718 respectively, while for the calibration process, 0.8799, -0.5974 and 0.8800 respectively. The model results show that the futuristic runoff of Heihe river basin will increase a little. The snowmelt, glacier meltwater and the evaportranspiration will increase. The air temperature increment will make the permanent snow and glacier area diminish, and the snowline will rise. The vegetation, especially the forest in Heihe mountainous watershed, could lead to the evapoWanspimtion decrease of the watershed, adjust the runoff orocess, and increase the soil water content. 相似文献
8.
Regionalization of soil and water conservation is a base for the planning of soil and water conservation in China. It can provide scientific basis for constructing healthy eco-environment and regional management and development. It makes a brief review of related regionalization of study and makes clear the concept of regionalization of soil and water conservation. In this paper, based on synthetical analysis of the characteristics of eco-environments of China, the principles, indices and nomenclature of the regionalization of soil and water conservation are proposed. Through the construction of the regionalization of soil and water conservation collaboration platform and data reporting system, combined with existing soil and water conservation research, this paper uses the top-down and bottom-up and the combination of qualitative and quantitative methods to build soil and water conservation regionalization preliminary scheme, with 8 regions, 41 sub-regions and 117 sections divided in China. 相似文献
9.
Situated in the hinterland of Eurasia, Central Asia is characterized by an arid climate and sparse rainfall. The uneven spatial distribution of water and land resources across the region has pressured economic and social development. An accurate understanding of Central Asia’s water resources carrying capacity(WRCC) is vital for enhancing the sustainability of water resources utilization and guiding regional economic and social activities. This study aims to facilitate the sustainability of wate... 相似文献
10.
Soil-plant systems play an important role in sand fixing and surface protection in the arid desert of China. This study examines the ecohydrological responses after a soil-plant system change for mobile dune stabilization by using a series of soil hydrological experiments and ecological investigation. The study results showed that decades of succession of soil-plant system has endangered the stability of the protection system. With the accumulated water and nutrient, a bio-logical system develops in a thinner and thinner surface soil. Redistribution of precipitation has changed completely in the ecosystem. In 3-15 mm of soil, a high capacity of crust water retention ultimately limits most rainfall from infiltrating below 10-20 cm deep. When that takes place, lower plants begin to compete for water with grasses and shrubs. A drought horizon forms in 20-500 cm depth with shrub transpiration. Artificial shrubs with deep roots obtain hardly rainfall supply and are gradually eliminated from the protection system. All changes in water environment affect the structure and func-tion and stabilization of whole protection systems. It is necessary to establish a relatively stable water environment by managing the soil-plant system for constructing a sustainable protective system in arid desert. 相似文献
11.
The available soil water capacity (ASWC) is important for studying crop production, agro-ecological zoning, irrigation planning, and land cover changes. Laboratory determined data of ASWC are often not available for most of soil profiles and the nationwide ASWC largely remains lacking in relevant soil data in China. This work was to estimate ASWC based on physical and chemical properties and analyze the spatial distribution of ASWC in China. The pedo-transfer functions (PTFs), derived from 220 survey data of ASWC, and the empirical data of ASWC based on soil texture were applied to quantify the ASWC. GIS technology was used to develop a spatial file of ASWC in China and the spatial distribution of ASWC was also analyzed. The results showed the value of ASWC ranges from 15 × 10-2 cm3·cm-3 to 22 × 10-2 cm3·cm-3 for most soil types, and few soil types are lower than 15 × 10-2 cm3·cm-3 or higher than 22 × 10-2 cm3·cm-3. The ASWC is different according to the complex soil types and their distribution. It is higher in the east than that in the west, and the values reduce from south to north except the northeastern part of China. The "high" values of ASWC appear in southeast, northeastern mountain regions and Northeast China Plain. The relatively "high" values of ASWC appear in Sichuan basin, Huang-Huai-Hai plain and the east of Inner Mongolia. The relatively "low" values are distributed in the west and the Loess Plateau of China. The "very low" value regions are the northern Tibetan Plateau and the desertified areas in northern China. In some regions, the ASWC changes according to the complex topography and different types of soils. Though there remains precision limitation, the spatial data of ASWC derived from this study are improved on current data files of soil water retention properties for Chinese soils. This study presents basic data and analysis methods for estimation and evaluation of ASWC in China. 相似文献
12.
上海市崇明岛农田土壤重金属的环境质量评价(英文) 总被引：1，自引：0，他引：1
The environmental quality of heavy metals (Pb,Cd,Cr,As,Hg) in agricultural surface soil of Chongming Island was assessed by national,local and professional standards based on a large scale investigation,in which 28 samples from vegetable plots,65 samples from paddy fields and 9 samples from watermelon fields were collected from whole island area. Results showed that the average concentration of Pb,Cd,Cr,As and Hg was 21.6 mg·kg-1,0.176 mg·kg-1,69.4 mg·kg-1,9.209 mg·kg-1 and 0.128 mg·kg-1,respectively. Compared with the background value of Shanghai City soil,except for Pb and Cr,all the other heavy metals average concentrations in Chongming Island agricultural surface soil exceeded their corresponding natural-background values. The concentrations of Cd,As and Hg were 33.0%,1.2% and 26.3% higher than the background value of Shanghai City,respectively. In addition,inverse distance interpolation (IDW) tool of GIS was also applied to study the spatial variation of heavy metals. The results indicated that most of agricultural soil quality was good,and the ratio of ecological,good soil,certified soil and disqualified soil were 1.26%,97.1%,1.47% and 0.12%,respectively. About 10.1%,85.7%,27.0%,55.4% and 55.2% soil samples exceeded the Pb,Cd,Cr,As and Hg background value of Shanghai City,respectively. Among these three land use type soils,vegetable soil was most seriously polluted by heavy metals,which is probably related to the over-application of pesticides. The annual deposition fluxes of Pb,Cd,As and Hg were 7736 μg.m-2.a-1,208 μg.m-2.a-1,2238 μg.m-2.a-1 and 52.8 μg.m-2.a-1,respectively. Crop straw burning was the important source of heavy metals of atmospheric deposition,and atmospheric deposition contributed a lot to heavy metals in agricultural soil in Chongming Island. 相似文献
13.
François Michaud Hermes U. Ramírez-Sánchez Claude Parron Pedro F. Zárate-del Valle François Fernex Geneviève Barci-Funel 《Journal of Paleolimnology》2006,35(4):819-836
Lake Chapala, located 120 km northeast of Colima Volcano, lies at the north and northeast of the Citala rift in the Trans-Mexican
Volcanic Belt. It belongs to the watershed of the Lerma River, which originates from the Mexico City area, 450 km to the east.
Sediment cores, 0.5–2 m long, were collected from the lake. Magnetic susceptibility of the lake sediments generally ranges
from 400 to 800 × 10−9 m3 kg−1; but in some layers it exceeds 1000 or 1500 × 10−9 m3 kg−1. The magnetic susceptibility vertical profiles display a thin peak (2–5 cm) or a double peak with magnetic susceptibility
> 2000 × 10−9 m3 kg−1. Scanning electron microscope analysis shows that the main mineral responsible for the magnetic susceptibility is titano-magnetite,
which is relatively abundant in the magnetic layers. In most of the cores, the layer with magnetic susceptibility > 2000 ×
10−9 m3 kg−1 is coarser grained than the directly under and overlying sediments, which are composed of fine silt. But not all coarser
levels are magnetic nor are all magnetic levels bound to coarser layers. The high titano-magnetic concentration probably originates
from volcanic ash falls. Sedimentation rates, evaluated for several sites by means of the 210Pb and 137Cs methods, allow a date approximation (between 1535 and 1670) for the strong magnetic layer deposition. Since important eruptions
of Colima Volcano, with ash fall, were reported from 1576 to 1623, the main peak of magnetic susceptibility in the sediment
profiles is assumed to be related to these events. The main magnetic layer extends to greater depth in the profiles of the
eastern part of the lake plain than at the west. It can, therefore, be suggested that a relative subsidence occurs in the
eastern part of the lake; the axis of the eastern plain overlaps the area displaying the maximum subsidence rate and seems
therefore to correspond to the prolongation of Citala rift. 相似文献
14.
中国东北漫岗黑土区切沟侵蚀发育特征 总被引：4，自引：0，他引：4
In this study, short-term gully retreat was monitored from the active gullies selected in representative black soil area,
using differential global positioning system (GPS). With the support of geographic information system (GIS), multi-temporal
digital elevation models (DEM) were constructed from the data collected by GPS and used for further analysis. Based on the
analysis of multi-temporal DEM, we discussed the erosion-deposition characteristics within gully and a developing model for
black soil gully area of Northeast China was proposed. The results are: (1) The analysis of the monitored gully data in 2004
indicated that the retreat of gully head reached more than 10 m, gully area extended 170–400 m2, net gully eroded volume 220–320 m3, and gully erosion modulus 2200–4800 t·km−2·a−1. (2) Compared with the mature gully the initial gully grows rapidly, and its erosion parameters are relatively large. The
erosion parameters have not only to do with flow energy, but also with the growth phase. (3) There are significant seasonal
differences in gully erosion parameters. The extension of gully area and width dominates in winter and spring without marked
net erosion while changes mainly occur in gully head and net erosion in rainy season. (4) It is remarkable for freeze-thaw
erosion in the black soil area of NE China. The gully wall of SG2 extended 0.45 m under freeze-thaw effect in 2004, and the
distance of gully head retreated maximally 6.4 m. (5) Due to freeze-thaw action and snowmelt, gully is primarily in the interior
adjustment process in winter and early spring. There are much more depositions compared with that during rainy season, which
can almost happen throughout the gully, while erosion mostly occurs near head, esp. for gullies having a relatively long history
of development. On the other hand, the process of energy exchange with exterior dominates in rainy season. It is considered
that this cyclic process is an important mechanism for gully growth in high latitude or/and high attitude regions.
Foundation: Key Project for National Natural Science Foundation of China, No.40235056; The Ph.D. Programs Foundation of Ministry of Education
of China, No.20030027015; China Postdoctoral Science Foundation, No.20070410482; Doctoral Foundation of University of Jinan,
No.B0620; National Natural Science Foundation of China, No.40672158; Key Subject Foundation Supported by Shandong Province
Author: Hu Gang (1976–), Ph.D and Associate Professor, specialized in soil erosion, environmental evolution and regional planning. 相似文献
15.
Taking the Chaohe River Basin above the Miyun Reservoir in North China as a study area, the characteristics and variation
trends of annual runoff and annual precipitation during 1961–2005 were analyzed applying Mann-Kendall test method on the basis
of the hydrologic data of the major hydrological station (Xiahui Station) located at the outlet of the drainage basin and
the meteorological data of 17 rainfall stations. Human activities including water conservancy projects construction and water
diversion as well as implementation of soil and water conservation from 1961 to 2005 were carefully studied using time series
contrasting method. The referenced period (1961–1980) that influenced slightly by human activities and the compared period
(1981–2005) that influenced significantly by water conservancy and soil conservation measures were identified according to
the runoff variation process analysis and abrupt change points detection during 1961–2005 applying double accumulative curve
method, mean shift t-test method and Mann-Kendall mutation test technique. Based on the establishment of a rainfall-runoff
empirical statistical model, impacts and the runoff-reducing effects of water conservancy and soil conservation measures on
runoff reduction were evaluated quantitatively. The major results could be summarized as follows: (1) The annual precipitation
in the drainage basin tends to decrease while the runoff has declined markedly since the 1960s, the average annual runoff
from 1991 to 2000 was only 90.9% in proportion to that from 1961 to 1970. (2) The annual runoff variations in the drainage
basin are significantly related to human activities. (3) During 1981–1990, 1991–2000, 2001–2005 and 1981–2005, the average
annual runoff reduction amounts were 1.15×108, 0.28×108, 1.10×108 and 0.79×108 m3 respectively and the average annual runoff-reducing effects were 31.99%, 7.13%, 40.71% and 23.79% accordingly. Runoff-reducing
effects by water conservancy and soil conservation measures are more prominent in the low water period. 相似文献
16.
Neil L. Rose David Morley Peter G. Appleby Richard W. Battarbee Tiiu Alliksaar Piero Guilizzoni Erik Jeppesen Atte Korhola Jaan-Mati Punning 《Journal of Paleolimnology》2011,45(4):447-468
Sediment accumulation rate (SAR) is an important physical parameter in all lakes and increases have been observed in many
over the last c.100 years. This has been ascribed to changes in land-use and land-management causing accelerated catchment
soil erosion and an increase in autochthonous organic matter production. The EU Water Framework Directive requires that assessment
of biological, hydromorphological and chemical elements of water quality should be based on the degree to which present day
conditions deviate from those expected in the absence of significant anthropogenic influence, termed reference conditions.
Currently however, the reference condition for sediment accumulation rate for lakes of different types is undefined. To improve
our understanding of the controls on SARs we compiled SAR and lake typology data for 207 European lakes derived from 210Pb dated cores to assess how rates have changed through time (in 25 year classes) both overall and for lakes of different
types. Seventy-one percent of these sediment cores showed surface SARs higher than “basal” (mainly nineteenth century) rates,
11% showed no change while 18% showed a decline. Lakes were then classified into lake-types using four variables: alkalinity
(3 classes), altitude (3 classes), maximum depth (2 classes) and lake area (2 classes). This generated a possible 36 lake
classes of which 25 were represented in the dataset. Nine lake-types contained >10 lakes. Little change in SAR occurred prior
to 1900 and most increases occurred in more recent periods, in particular 1950–1975 and post-1975. This indicates a general
acceleration in SAR in European lakes during the second half of the twentieth century. Reference SARs were estimated for six
lake-types with the highest number of sites. European mountain lakes had the lowest reference SAR (0.005 ± 0.003 g cm−2 yr−1) while lowland, high alkalinity sites had the highest (0.03–0.04 g cm−2 yr−1). SARs for other lake-types ranged between 0.012 and 0.024 g cm−2 yr−1. Using the mountain lake-type as an example, the 1850 reference SAR appears to show good agreement with available data for
lakes beyond Europe indicating these values may be more broadly applicable. Contemporary SARs in lakes of all classes showed
exceedence over their defined reference SAR. This may be partly due to diagenetic processes. Greatest exceedences were found
in shallow, low altitude lakes and these are considered to be the ones under the greatest threat from continued elevation
of SAR. It is considered that climate change may play a progressively more important role in driving SAR in the future. 相似文献
17.
近50年中国光合有效辐射的时空变化(英文) 总被引：2，自引：1，他引：1
Based on long-term measurement data of weather/ecological stations over China,this paper calculated and produced annually-and seasonally-averaged Photosynthetically Active Radiation(PAR) spatial data from 1961 to 2007,using climatological calculations and spatialization techniques.The spatio-temporal variation characteristics of annually-and seasonally-averaged PAR spatial data over China in recent 50 years were analyzed with Mann-Kendall trend analysis method and GIS spatial analysis techniques.The results show that:(1) As a whole,the spatial distribution of PAR is complex and inhomogeneous across China,with lower PAR in the eastern and southern parts of China and higher PAR in the western part.Mean annual PAR over China ranges from 17.7 mol m-2 d-1 to 39.5 mol m-2 d-1.(2) Annually-and seasonally-averaged PAR of each pixel over China are averaged as a whole and the mean values decline visibly with fluctuant processes,and the changing rate of annually-averaged PAR is-0.138 mol m-2 d-1/10a.The changing amplitudes among four seasons are different,with maximum dropping in summer,and the descending speed of PAR is faster before the 1990s,after which the speed slows down.(3) The analysis by each pixel shows that PAR declines significantly(α=0.05) in most parts of China.Summer and winter play more important roles in the interannual variability of PAR.North China is always a decreasing zone in four seasons,while the northwest of Qinghai-Tibet Plateau turns to be an increasing zone in four seasons.(4) The spatial distributions of the interannual variability of PAR vary among different periods.The interannual variabilities of PAR in a certain region are different not only among four seasons,but also among different periods. 相似文献
18.
长江口滨岸湿地沉积物对上覆水体中无机氮的净化能力估算 总被引：1，自引：0，他引：1
Estuarine wetlands serve as a natural barrier to remove the land-generated pollut-ants and attenuate the pollutant load from the land to the sea. As one of the most important estuarine wetlands, the Yangtze estuarine wetlands have attracted particular interests in the biogeochemical studies of nutrients. The objectives of this study were to characterize the seasonal and spatial distribution of dissolved inorganic nitrogen (DIN) fluxes across the sediment-water interface; to calculate the total DIN fluxes in a year and different seasons; and to evaluate the DIN removing capability of the sediment in the tidal wetlands of the Yangtze Estuary. The spatial distribution of DIN fluxes shows complicated seasonal variations and spatial differences. The annual DIN fluxes range from -22.22 mmol N m-2 h-1 to 19.54 mmolN m-2 h-1, with an average of -1.48±1.34 mmol N m-2 h-1. The tidal wetlands in the Yangtze Estuary behave as a source of water DIN in spring when DIN is released from sediment into overlying water, and the released amount of DIN is 1.33×104 tons of nitrogen (T N). In sum-mer, autumn and winter, the sediment absorbs the DIN from the overlying water, and the absorbed amounts of DIN are 4.36×104 T N, 6.81×104 T N and 2.24×104 T N, respectively. The average amount of DIN in overlying water of the Yangtze Estuary is 52.6×104 T N yr-1, and the perennial average amount of DIN absorbed from the overlying water by the sediment is 12.1×104 T N yr-1. The annual DIN elimination rate of the tidal wetlands was 23.0%. 相似文献
19.
An overview of recent changes in salinity in the surface waters of the Aral sea basin is given. Total dissolved salts (salinity)
in most waters are higher than admissible values for drinking water, and ionic composition has changed with time. Salinity
of the ‘Big Sea’ of the Aral was 48 g L−1 in 1998, but has decreased to below 21 g L−1 in the ‘Small Sea’ due to the building of a new dam between the two parts of the Aral Sea. 相似文献
20.
为阐明祁连山青海云杉(Picea crassifolia)林分布带对其土壤碳、氮含量的影响,以分布在祁连山东段和西段的典型青海云杉林为研究对象,通过野外取样和室内分析,论述了青海云杉林浅层土壤碳、氮含量特征及其相互关系。结果表明:(1)祁连山东、西段土壤剖面有机碳含量均随土壤深度的增加而减小,但不同土层差异显著性不同,0~40cm含量分别为73.57±17.17g·kg-1和45.85±11.93g·kg-1;东、西段土壤剖面有机碳储量没有明显的变化规律,0~40cm有机碳储量分别为205.51±39.44t·hm-2和134.93±25.80t·hm-2。(2)祁连山东、西段土壤全氮含量随土层深度变化和不同土层差异显著性变化规律同土壤有机碳含量,0~40cm全氮含量分别为4.56±0.88g·kg-1和2.81±0.66g·kg-1;东、西段土壤全氮储量亦同土壤有机碳储量变化规律,0~40cm储量分别为12.77±2.08t·hm-2和8.38±1.56t·hm-2。(3)祁连山东、西段土壤剖面不同土层C/N比差异显著性变化规律相同,其C/N值分别为15.92±1.24和16.10±2.07;C/N比值大小主要取决于有机碳含量;线性分析表明,土壤有机碳与全氮含之间呈极显著的正相关关系,可用乘幂曲线模型Y=aXb较好地描述(p0.01)。上述研究结果可为祁连山水源涵养林建群种青海云杉林的经营和管理提供理论依据和数据支撑。 相似文献