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11.
膜下滴灌棉田生物改良盐碱地效果研究 总被引:5,自引:0,他引:5
通过在膜下滴灌棉田间作苜蓿(Ⅰ)、孜然(Ⅱ)和碱蓬(Ⅲ),并以未间作的处理作为对照(CK),研究不同盐生植物改良盐碱地的效果。结果表明:间作盐生植物的棉田在生育期内可以达到保水和抑制盐分累积的效果,土壤含水量峰值基本保持在40 cm深度,其中以间作苜蓿(Ⅰ)和孜然(Ⅱ)的保水效果较好,在0~40 cm深度范围土壤含水量与对照组相比分别提升了29.80%和14.49%;间作苜蓿(Ⅰ)和孜然(Ⅱ)的处理抑制盐分累积的效果也较好,在0~40 cm深度范围抑盐率分别为125%和70.38%。同时,通过在膜间种植盐生植物,棉花的株高、茎粗和干物质量均有一定程度的增加,籽棉产量也有相应的提升,其中以间作孜然和苜蓿的处理提升较多,分别比对照组提升10.45%和7.74%。由此可见,膜下滴灌棉田间作盐生植物是一种有效的盐碱地改良措施,而盐生植物的选择对改良的效果影响较大,综合试验结果对比,间作孜然和间作苜蓿的生物改良措施效果较好。 相似文献
12.
黄土高原退耕还林措施对深层土壤含水率的影响 总被引:3,自引:0,他引:3
深层土壤水分分布状况对于黄土高原植被恢复和农业可持续发展意义重大。对陕北黄土区不同退耕还林措施(1979年种植的侧柏林、油松林和苹果林)及农地(对照)20 m深土壤剖面的土壤水分、根系分布状况及土壤粘粒含量进行了取样分析。结果表明:退耕还林措施显著降低了土壤含水率,总体表现为农地(11.30%)苹果林(6.66%)≈油松林(6.48%)≈侧柏林(5.92%)。深层土壤含水率同时受植物根系和土壤质地的影响,植物根系是影响4~10 m土壤含水率的主要因素,根系通过吸水作用降低了土壤含水率,但随着深度的增加,根系对土壤含水率的影响逐渐减弱,土壤质地对土壤含水率的影响逐渐增强,土壤含水率与土壤粘粒含量之间呈正相关关系。侧柏人工林根系影响土壤水分深度可达18 m,油松林的影响深度为16 m,35 a树龄的苹果林耗水深度为19 m左右。 相似文献
13.
完善的后续政策是巩固退耕还林成果的重要前提 总被引:6,自引:0,他引:6
1999年以来,长江上游、黄河上中游等地区开展的退耕还林的试点工作,是加强西部地区生态环境建设和保护的重要举措,也是贫困山区农民脱贫致富的有效途径.目前,第一批退耕还林工程现已进入成果巩固阶段,但是,原有的政策措施已不适应成果巩固阶段的要求.为把退耕还林工作扎实、稳妥、健康地向前推进,必须进一步完善退耕还林的政策措施.针对退耕还林工程中存在的问题,提出了巩固退耕还林成果的后续政策. 相似文献
14.
《Scandinavian Journal of Forest Research》2012,27(5):433-442
Abstract This research reports the major evaluation results from an operational stand-based forest inventory using airborne laser scanner data carried out in Norway. This is the first operational inventory in which data from two separate districts are combined. Laser data from two forest areas of 65 and 110 km2 were used to predict six biophysical stand variables used in forest planning. The predictions were based on regression equations estimated from 250 m2 field training plots distributed systematically throughout the two forest areas. Test plots with a size of 0.1 ha were used for validation. The testing revealed standard deviations between ground-truth values and predicted values of 0.58–0.85 m (3.4–5.6%) for mean and dominant heights, 2.62–2.87 m2 ha?1 (9.3–14.3%) for basal area, and 18.7–25.1 m3 ha?1 (10.8–12.8%) for stand volume. No serious bias was detected. For 10 of the 12 estimated regression models there were no significant effects of district. 相似文献
15.
基于GIS的祁连山森林景观格局分析 总被引:24,自引:2,他引:24
在地理信息系统软件ArcGIS环境下 ,将祁连山区DEM图和坡向图分别同植被图叠加 ,分析研究区各景观组分在空间的分布特征 ;用定量分析景观结构和景观格局程序Fragstats计算景观和各景观组分的相关指数 ,分析其连通性、完整性、破碎化程度及聚集程度。结果表明 :研究区各景观组分分布受海拔高度和坡向的影响非常明显。各景观组分的完整性、连通性和破碎化程度也很不均衡。草地是研究区面积最大、连通性和完整性最好的景观组分 ;青海云杉林呈斑块状或带状分布在阴坡和半阴坡 ,形状最为不规则 ,平均斑块面积小且距离近 ,易受干扰而发生重大变化 ;宜林地和祁连圆柏林相对于农田、疏林地有较强的扩张特征 ;而杨类阔叶林各斑块间相隔距离大 ,斑块之间的邻接性差 ,破碎化程度最为严重。 相似文献
16.
17.
目的 试图给出确定森林群落树种丰富度的方法,解决物种丰富度测度问题,完善森林生物多样性研究的方法。 方法 采用Monod模型表达种-面积曲线,通过数学手段确定最小森林群落面积和最大树种数。 结果 用本研究提出的方法对不同气候带森林物种丰富度进行测算,结果表明:热带森林群落具有更高的最大树种数和更大的群落最小面积,物种丰富度随气候带由热带到寒温带逐渐减少。 结论 用最大树种数能够确切表达不同气候带森林群落树种丰富度,克服了现有研究中直接把不同大小调查面积上的树种数量视为树种丰富度的弊端。 相似文献
18.
19.
M. von Lützow L. Zelles I. Scheunert J. C. G. Ottow 《Biology and Fertility of Soils》1992,13(3):130-134
Summary Seasonal effects of liming, irrigation, and acid precipitation on microbial biomass N and some physicochemical properties of different topsoil horizons in a spruce forest (Picea abies L.) were measured throughout one growing season. The highest biomass N was recorded in autumn and spring in the upper soil horizons, while the lowest values were obtained in summer and in deeper horizons. The clearest differences between the different soil treatments were apparent in autumn and in the upper horizons. Liming increased the microbial biomass N from 1.7% of the total N content to 6.8% (Olf1 layer) and from 1% to 2% of the total N content in the Of2 layer. The main inorganic-N fraction in the deeper horizons was NO
inf3
sup-
. An increase in cation exchange capacity was observed down to the Oh layer, while soil pH was only slightly higher in the Olf1 and Of2 layers after liming. The effects of irrigation were less marked. The microbial biomass N increased from 1.7% of total N to 4.8% in the Olf1 layer and from 1% to 2% of total N in the Of2 layer. In the Olf1 layer an increase in C mineralization was observed. Acid precipitation decreased the microbial biomass N in the upper horizons from 4.8% of total N to 1.8% in the Olf1 layer and from 2% to 0.5% in the Of2 layer. No significant changes in soil pH were observed, but the decrease in cation exchange capacity may result in a decrease in the proton buffering capacity in the near future. 相似文献
20.
M. L. Vélez M. P. A. Coetzee M. J. Wingfield M. Rajchenberg A. G. Greslebin 《Plant pathology》2014,63(1):212-220
Phytophthora austrocedrae is a recently discovered pathogen that causes severe mortality of Austrocedrus chilensis in Patagonia. The high level of susceptibility of the host tree, together with the distribution pattern of the pathogen, have led to the hypothesis that P. austrocedrae was introduced into Argentina. The aim of this study was to assess the population structure of P. austrocedrae isolates from Argentina in order to gain an understanding of the origin and spread of the pathogen. Genetic diversity was determined based on amplified fragment length polymorphisms (AFLPs). In total, 48 isolates of P. austrocedrae were obtained from infected A. chilensis trees, representing the geographical range of the host. Four primer combinations were used for the AFLP analysis. Of the 332 scored bands, 12% were polymorphic. Gene diversity (h) ranged from 0·01 to 0·03; the Shannon index (I) ranged from 0·01 to 0·04. A high degree of genetic similarity was observed among the isolates (pairwise S values = 0·958–1; 0·993 ± 0·009, mean ± SD). A frequency histogram showed that most of the isolate pairs were identical. Principal coordinate analysis using three‐dimensional plots did not group any of the isolates based on their geographical origin. The low genetic diversity (within and between sites) and absence of population structure linked to geographic origin, together with the aggressiveness of the pathogen and the disease progression pattern, suggest that P. austrocedrae might have been introduced into Argentina. 相似文献