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991.
992.
Species diversity and stability of natural secondary communities in different layers with different cutting intensities 10
years later were investigated by calculating Marglef Richness index (R), Shannon-Wiener diversity index (H), Simpson diversity index (P), and Pielou Evenness index (J). Results show that the values of R, H and P among different layers are listed in a decreasing order: the shrub layer > the arbor layer > the herb layer, all the three
indices values reach the maximum under medium selective cutting intensity after 10 years. The J value of the shrub layer shows a concave parabolic change with the increase in cutting intensity; it shows a linear increase
for the arbor layer, whereas the J value of the herb layer shows an opposite change pattern. The values of R at different cutting intensities had high significant difference, but other indices had not significant difference. The stability
of communities at different cutting intensities after 10 years is non-cutting> low selective cutting intensity > medium selective
cutting intensity > high selective cutting intensity > extra-high intensity > clear cutting. The stability of communities
at different cutting intensities after 10 years shows that the greater cutting intensities, the worse the stability is. 相似文献
993.
分析主要生态因子对火炬松生长的影响,结果表明:立地类型、海拔高度、坡度对火炬松的胸径、树高、单株材积、单位面积蓄积量等,均有极显著的影响;土壤的腐殖质、速N、速P含量与火炬松胸径、树高的生长密切相关,从而影响了单株材积和单位面积蓄积;土壤K含量对火炬松生长没有影响;年降水量、2~7月份的降水量对火炬松的胸径、树高生长有明显的影响,年积温对胸径生长有明显影响,对树高生长没有影响。 相似文献
994.
The mineralization/immobilization of nitrogen when organic sources are added to soil is represented in many simulation models as the outcome of decomposition of the added material and synthesis of soil organic matter. These models are able to capture the pattern of N release that is attributable to the N concentration of plant materials, or more generally the C:N ratio of the organic input. However, the models are unable to simulate the more complex pattern of N release that has been observed for some animal manures, notably materials that exhibit initial immobilization of N even when the C:N of the material suggests it should mineralize N. The APSIM SoilN module was modified so that the three pools that constitute added organic matter could be specified in terms of both the fraction of carbon in each pool and also their C:N ratios (previously it has been assumed that all pools have the same C:N ratio). It is shown that the revised model is better able to simulate the general patterns on N mineralized that has been reported for various organic sources. By associating the model parameters with measured properties (the pool that decomposes most rapidly equates with water-soluble C and N; the pool that decomposes slowest equates with lignin-C) the model performed better than the unmodified model in simulating the N mineralization from a range of feeds and faecal materials measured in an incubation experiment. 相似文献
995.
本文以团山沟单元小流域作为流域系统产沙的源地,将其它中小流域输沙模数与单元小流域侵蚀模数之比定义为泥沙输移比,系统的研究了岔巴沟流域次暴雨泥沙输移比的时空变化特征及降水水文影响因子和地貌形态因子的综合影响。研究发现,从长远来看,流域系统的侵蚀与产沙可达到平衡,但就次降雨或年度而言,流域系统经常处于泥沙滞留和滞留的泥沙重新侵蚀搬运的状态。降雨量、径流系数、降雨时间、水流平均含沙量能很好的表达岔巴沟各流域次暴雨泥沙输移比,在考虑地貌形态因子的影响后,得到了岔巴沟流域次暴雨泥沙输移比的降水水文因子与地貌形态因子关系的综合表达式。 相似文献
996.
土壤数据库在土壤学研究工作中作为一种存储、分析工具的重要性是不言而喻的.本研究利用ArcGIS和Visual FoxPro建立了包括8 830个图斑、269个土壤剖面数据的无锡和常州市1:5万土壤数据库,根据“土壤质量演变规律与持续利用‘973'项目”的土壤肥力质量指标(pH、速效磷和速效钾)和全国养分分级标准(全氮)编制出土壤表层(0~15 cm)pH、全氮、速效磷和速效钾的空间分异图,从中表明pH 1~2级的土壤占整个研究区面积90%左右;土壤养分全氮、速效磷和速效钾的空间分布有明显共同特征-太滆平田区养分含量要显著高于其他地区.对不同母质和不同土壤类型(亚类级别)间的土壤表层容重、粘粒、pH、有机质、全氮、全磷、全钾、速效磷和速效钾进行了方差分析,结果显示,除全氮之外,其他属性均有显著差异.在1:5万尺度范围内,成土母质对pH、容重、全磷、有机质和速效钾起到主导作用,土壤类型对pH起到主导作用,成土母质对土壤属性的影响程度要大于土壤类型. 相似文献
997.
998.
Sarah I. Beldin Bruce A. Caldwell Phillip Sollins Elizabeth W. Sulzman Kate Lajtha Susan E. Crow 《Biology and Fertility of Soils》2007,43(6):837-841
The cation exchange capacity (CEC) of a soil depends on the type and amount of both mineral and organic surfaces. Previous
studies that have sought to determine the relative contribution of organic matter to total soil CEC have not addressed differences
in soil organic matter (SOM) composition that could lead to differences in CEC. The objectives of this study were (1) to compare
the CEC of two distinct SOM pools, the “light fraction (LF)” composed of particulate plant, animal, and microbial debris,
and the “heavy fraction (HF)” composed of mineral-bound organic matter; and (2) to examine the effects of differences in aboveground
vegetation on CEC. Soil samples were collected from four paired grassland/conifer sites within a single forested area and
density fractionated. LF CEC was higher in conifer soils than in grassland soils, but there was no evidence of an effect of
vegetation on CEC for the HF or bulk soil. LF CEC (but not HF CEC) correlated well with the C concentration in the fraction.
The mean CEC of both fractions (per kg fraction) exceeded that of the bulk soil; thus, when the LF and HF CEC were combined
mathematically by weighting values for each fraction in proportion to dry mass, the resulting value was nearly twice the measured
CEC of bulk soil. On a whole soil basis, the HF contributed on average 97% of the CEC of the whole soil, although this conclusion
must be tempered given the inflation of CEC values by the density fractionation procedure. 相似文献
999.
Assessing soil erosion and control factors by the radiometric technique in the Boussouab catchment,Eastern Rif,Morocco 总被引:1,自引:0,他引:1
In the Eastern Rif of N Morocco, soil conservation is seriously threatened by water erosion. Large areas of soil have reached an irreversible state of degradation. In this study, the 137Cs technique was used to quantify erosion rates and identify the main factors involved in the erosion process based on a representative catchment of the Eastern Rif. To estimate erosion rates in terms of the main factors affecting soil losses, samples were collected taking into account the lithology, slope and land use along six selected transects within the Boussouab catchment. The transects were representative of the main land uses and physiographic characteristics of that Rif sector. The reference inventory for the area was established at a stable, well preserved, matorral site (value of 4250 Bq m− 2). All the sampling sites were eroded and 137Cs inventories varied widely (between 245 and 3670 Bq m− 2). The effective soil losses were also highly variable (between 5.1 and 48.8 t ha− 1 yr− 1). Soil losses varied with land use. The lowest average values were on matorral and fallow land (10.5 and 15.2 t ha− 1 yr− 1, respectively) but much higher with alfa vegetation or cereal crops (31.6 and 27.3, respectively). The highest erosion rate was on a badland transect at the more eroded part of the catchment, with rates exceeding 40 t ha− 1 yr− 1 and reaching a maximum of 48.8 t ha− 1 yr− 1.The average soil losses increased by more than 100% when the slope increased from 10° (17.7 t ha− 1 yr− 1) to 25° (40. 8 t ha− 1 yr− 1). Similar results were obtained when comparing erosion rates in soils that were covered by matorral with respect to those under cultivation. Lithology was also a key factor affecting soil loss. Soils on marls were more erodible and the average erosion rates reached 29.36 t ha− 1 yr− 1, which was twice as high as soils on the glacis and old fluvial terraces (average rates of 14.98 t ha− 1 yr− 1). The radiometric approach was very useful to quantify erosion rates and to examine the pattern of soil movement. The analysis of main erosion factors can help to promote rational soil use and establish conservation strategies in the study area. 相似文献
1000.
[目的] 从地形和社会经济两个因素出发探讨广东省土地覆被变化的时空差异及成因,为土地资源的可持续利用提供依据。[方法] 基于1992-2015年间广东省土地覆被数据,使用土地利用动态度、土地利用转移矩阵、灰色关联分析等方法量化土地覆被变化的时空特征与差异。[结果] 广东省土地覆被变化以2000年为节点可分为前期(1992-2000年)和后期(2000-2015年)两个阶段。前期耕地面积显著增加,建筑用地面积增速缓慢;后期耕地面积减小,建筑用地面积扩张迅速。地形因素造成土地覆被变化存在空间差异性。在高程低,坡度缓的区域土地覆被变化主要是耕地转化为建筑用地,而在坡度中等区域主要是林地转为耕地。社会经济因素造成土地覆被变化呈现较明显时间差异性,多种因子驱动广东省土地覆被发生变化。但对于不同的土地覆被类型,驱动因子前后期的关联度大小不同,土地覆被发生变化是多种因子驱动叠加的结果。[结论] 地形因素会造成土地覆被变化的空间差异,而社会经济因素导致土地覆被变化的时间差异。 相似文献