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951.
《植物养料与土壤学杂志》2017,180(3):381-388
The aim of this research was to investigate the effect of biochar amendment on soil acidity and other physico‐chemical properties of soil in Southern Ethiopia using a field experiment of three treatments: (1) biochar made of corn cobs, (2) biochar made of chopped Lantana camara stem, and (3) biochar made of Eucalyptus globulus feedstock and a control, in which neither of the biochar was used. Each treatment had three levels of 6, 12 and 18 t ha−1. The experiment was setup with RCBD in a factorial arrangement with three replications. In this regard, a total of 36 plots (each 2 × 2 m size) were applied with three replications to the depth of 0–15cm. From these 36 plots, composite soil samples were collected to the depth of 0–30 cm and analyzed for bulk density, total porosity, pH, soil organic carbon, total nitrogen, available phosphorus, potassium, and exchangeable acidity using standard procedures before and after biochar application. Two‐way ANOVA was also used to analyze the impact of the biochars on soil acidity and other properties. For the treatments that had significant effects, a mean separation was made using Least Significance Difference (LSD) test. The results showed the application of biochar significantly reduced, soil bulk density and exchangeable acidity when compared with a control (p < 0.05). Moreover, the total soil porosity, soil pH, total nitrogen, soil organic carbon, available phosphorus, and potassium were significantly increased in the soil. From among applied biochar treatments, Lantana camara applied at the level of 18 t ha−1 had a higher impact in changing soil physico‐chemical properties. In general, the study suggests that the soil acidity can be reduced by applying biochar as it can amend other soil physico‐chemical properties. 相似文献
952.
干热河谷冲沟侵蚀劣地坡积区土体性质与裂缝形态发育特征 总被引:2,自引:0,他引:2
采用实地调查和室内分析等方法,并结合数字图像处理技术,研究了干热河谷冲沟侵蚀劣地坡脚堆积区(PJ)、坡底沉积区(PD)和平地漫流区(PM)土体性质和裂缝形态发育特征,并探讨了土体性质对裂缝形态特征的影响。结果表明,(1)侵蚀劣地坡积区不同部位土体性质差异显著,其中土壤体积质量及黏粒质量分数均表现为PDPJPM,毛管孔隙度为PMPDPJ,有机质为PMPJPD;不同部位土体性质极值比:黏粒质量分数最大(1.94),有机质(0.65)次之,再次是毛管孔隙度(0.27),土壤体积质量(0.09)最小;PJ、PD土体性质变化主要受物源特性和沉积方式的影响,而PM土体性质主要与植被分布以及漫流有关。(2)干热河谷侵蚀劣地不同部位土体裂缝形态特征差异也十分显著,其中裂缝长度密度(Lc)及连通性指数(K)均表现为PDPJ≤PM,面积率(Rc)、面积周长比(APc)及加权平均分形维数(AWMFRAC)则整体上表现为PD≥PJPM(Ⅲ号坡积区的Rc除外);表明裂缝发育强度(Rc)及复杂程度(APc、AWMFRAC)PD最高,其次为PJ,再次是PM。(3)相关分析表明,长度密度与土壤体积质量(p=-0.782)、黏粒质量分数(p=-0.626)均呈显著负相关,连通性指数与黏粒质量分数呈显著负相关(p=-0.618),这表明土壤体积质量及黏粒质量分数对裂缝发育产生了重要影响。 相似文献
953.
954.
杉木耐瘠薄速生优树子代测定及早期选择 总被引:1,自引:0,他引:1
在福建省洋口国有林场,对7年生的杉木耐瘠薄速生优树半同胞子代测定林进行调查和分析测定。参试的各家系间树高、胸径和材积生长量均差异极显著,说明在家系水平上存在明显的分化;从参试的18个家系中选择出23号等5个在瘠薄立地条件下生长表现优良的家系,树高、胸径和材积平均值分别达7.67 m、10.88 cm和0.043 6 m3,与第2代种子园子代相比,其材积现实增益达21.11%,通过这种后向选择所选出的耐瘠薄速生优良家系具有明显的生长优势和耐瘠薄性,可以作为杉木第3代建园材料的补充。 相似文献
955.
956.
Soil strength and water content are important indices for assessing soil resistance to root growth and soil compaction both of which affect other soil properties. Therefore, simultaneous measurement of soil penetration resistance (PR) and soil water content can aid agricultural land management. We measured PR with a conventional cone penetrometer, followed immediately by determining water content using a modified TDR probe inserted into the penetrometer hole. From the results of a field feasibility test, soil water content was measured satisfactorily and correlated well with data obtained by the gravimetric method, except for those data from near the surface owing to soil disturbance when the cone penetrometer was extracted after the PR measurements. Field results demonstrate that PR and soil water content have three‐dimensional variability, with a markedly different distribution pattern between cultivated and subsoil layers at the field scale. Overall, the variability in the PR and soil water data is similar to that reported in previous studies. We conclude that our method produces results helpful to field management of soil and water because it is based on a simple and easy technique for the simultaneous measurement of soil water content and PR. 相似文献
957.
通过设立固定标准地对杨树的中幼林龄期和近熟林龄期生长情况进行调查分析,了解踊桥区祁县镇不同立地条件下杨树长势,判断林分立地条件对生长量影响的关键因子,并进行了标准地土壤剖面结构、理化性质和土壤养分含量对比,结论如下:影响杨树生长的关键因素是林地土层厚度,分析了杨树低产林形成原因是:土壤层浅、瘠薄、空隙度小、质地粘重。并提出相应对策:杨树低产林改造;加强中幼林抚育、进行土壤改良;发展林下经济改善土壤结构理化性质;营造复层林、间接改良土壤,提高林地综合利用率。 相似文献
958.
袁海军 《上海交通大学学报(农业科学版)》2013,(4):57-60
为提高潜水蒸发计算精度,利用潜水蒸发强度、埋深为零时的土面蒸发强度和水面蒸发强度的实测资料对阿维里扬诺夫公式、叶水庭公式和雷志栋公式中E0值的选取进行了探讨,同时对比分析了E0分别为水面蒸发强度和埋深为零时土面蒸发强度两种情况下的潜水蒸发强度。结果表明,针对新疆地区粘壤土类型,对于上述三种公式,若用埋深为零的土面蒸发强度代替水面蒸发强度,计算结果会产生误差,精度偏低,应选用E0为水面蒸发强度进行计算,获得了η与地下水埋深的指数函数关系。该研究为潜水蒸发经验模型中E0值的选取提供参考,同时为求解雷志栋公式中参数η提供一种新方法。 相似文献
959.
Soil saturation effects on forest dynamics: scaling across a southern boreal/northern hardwood landscape 总被引:1,自引:0,他引:1
Patch modeling can be used to scale-up processes to portray landscape-level dynamics. Via direct extrapolation, a heterogeneous landscape is divided into its constituent patches; dynamics are simulated on each representative patch and are weighted and aggregated to formulate the higher level response. Further extrapolation may be attained by coarsening the resolution of or lumping environmental data (e.g., climatic, edaphic, hydrologic, topographic) used to delimit a patch.Forest patterns at the southern boreal/northern hardwood transition zone are often defined by soil heterogeneity, determined primarily by the extent and duration of soil saturation. To determine how landscape-level dynamics predicted from direct extrapolation compare when coarsening soil parameters, we simulated forest dynamics for soil series representing a range of drainage classes from east- central Maine. Responses were aggregated according to the distribution of soil associations comprising a 600 ha area based on local- (1:12,000), county- (1:120,000) and state- (1:250,000) scale soil maps. At the patch level, simulated aboveground biomass accumulated more slowly in poorer draining soils. Different soil series yielded different communities comprised of species with various tolerances for soil saturation. When aggregated, removal of waterlogging caused a 20–60% increase in biomass accumulation during the first 50 years of simulation. However, this early successional increase and the maximum level of biomass accumulation over a 200 year period varied by as much as 40% depending on the geospatial data. This marked discrepancy suggests caution when extrapolating with forest patch models by coarsening parameters and demonstrates how rules used to rescale environmental data need to be evaluated for consistency. 相似文献
960.