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1.
Abstract. A two year field experiment was carried out in a semiarid Mediterranean area in order to evaluate, the effect on soil erosion of adding different urban organic wastes: a stabilized municipal waste (compost), an unstabilized municipal waste, and an aerobic sewage sludge. All the treatments significantly reduced soil erosion, compared to the control soil. The soil amended with compost was the most effective treatment, reducing soil loss by 94% and runoff by 54%.  相似文献   
2.
旱地保护性耕作地表径流和土壤水分平衡模型   总被引:12,自引:3,他引:12  
在田间试验和对现有径流模型及土壤水分平衡模型改进的基础上,建立了适用于保护性耕作的地表径流和土壤水分平衡模型。该模型以日为步长,根据气象数据、土壤水分状况、作物生长发育及耕作管理措施,模拟不同耕作管理体系下地表径流和田间水分平衡的变化。针对保护性耕作的特点,主要对径流曲线数字(USDA—Curve Number)法进行了改进,在PERFECT模型的基础上增加了坡度和降雨强度两因素的影响,从而使模型较全面地考虑了残茬覆盖、耕作、坡度及降雨强度等多种因素对径流的影响;采用简单实用的Priestley—Taylor公式计算潜在蒸散量,并考虑作物覆盖与残茬覆盖对土壤蒸发与作物蒸腾的影响。通过田间径流试验和根层有效贮水量测定数据的验证,证明了地表径流和土壤水分的模拟值与实测值比较接近。  相似文献   
3.
全球气候暖干化对秦岭南北河流径流泥沙的影响研究   总被引:8,自引:12,他引:8  
以秦岭南侧汉江和北侧渭河多年的径流泥沙观测资料,分析了全球气候暖干化对秦岭南北径流泥沙的变化。分析指出在80年代后,由于全球气候变化的影响,秦岭南北河流年均径流量均减少,与1935-1980年相比,汉江河流年均径流量减少1.9%,渭河河流年均径流量减少27.4%;同时汉江河流泥沙含量明显减少,但渭河河流泥沙含量呈增加趋势,是汉江河流泥沙含量133倍,表明了秦岭南北两侧在全球气候暖干化表现出明显的区域响应性。  相似文献   
4.
喀喇昆仑山盖孜河水文水资源特性分析   总被引:2,自引:1,他引:2  
喀喇昆仑山河流自有水文资料记载以来 ,近 10年洪灾发生频率明显高于以往 ,人民的生命财产损失程度也大幅度增加。在分析了盖孜河流域的径流及气候多年变化过程后 ,认为洪灾频发的原因是近年来流域内降水及气温呈上升趋势 ,导致高山冰川退缩 ,河流径流增加 ,洪灾增大、频率增高 ;小区域多年气候变化过程从侧面印证了我国西北地区气候由暖干向暖湿变化。  相似文献   
5.
Abstract – Standard metabolic rate (SMR, closely related to basal and resting metabolism) varies by up to threefold among juvenile Atlantic salmon, Salmo salar L., of similar size at common temperature. Here, consequences of this variation are predicted by combining empirically derived relationships between SMR, specific dynamic action, energy budgets, water velocity, food level in the environment and food availability to fish. The range of velocities across which growth is predicted to occur is inversely related to a fish’s SMR. Growth is positively related to SMR at high but negatively related to it at low‐food levels. The relationship between food level and the range of velocities over which lower SMR fish can grow but higher SMR fish cannot is asymmetrically bi‐phasic and peaked. It is predicted that maternal manipulation of offspring SMR would generate fitness benefits through bet‐hedging against unpredictability in food level and increases in the overall range of velocities that the family of offspring can occupy and thrive in.  相似文献   
6.
利用土工合成材料综合测定仪(直剪仪),以水分含量14.57%的糙米为样品,测定了在不同的法向压应力、不同的剪切速率下糙米的剪切应力并计算出内摩擦角。实验结果表明:糙米的剪切应力随着法向压应力(25kPa~100kPa)的增大而增大;剪切速率(1.33mm/min~2.67mm/min)较低时糙米的内摩擦角随着法向压应力的增大而减小;随着剪切速率(1.33mm/min~5.20mm/min)的增大,糙米的内摩擦角减小。  相似文献   
7.
The serial discontinuity concept (SDC) proposes that hypolimnetic‐releasing impoundments cause major disruptions to the naturally occurring physical, chemical and biological gradients of rivers but that this impact diminishes with distance downstream. Such a gradient in discharge, flow velocity and temperature regime occurs below a large hypolimnetic‐releasing impoundment, the Hume Dam, on the River Murray in south‐eastern Australia. To examine the effects of this disturbance gradient on a warm‐water large‐bodied freshwater fish, the Murray cod (Maccullochella peelii), a bioenergetics model was developed and calibrated to explore energy expended under differing water velocities and temperature regimes. Model simulations predicted negative growth of juveniles directly downstream of the impoundment, due largely to the energetic costs associated with active and, to a lesser extent, standard metabolism outweighing the achievable energetic gains through food consumption. As flow velocity and temperature regimes became more favourable downstream, so did the simulated growth of the species. It was not until +239 km downstream of the impoundment that the model predicted that flow velocity and temperature regimes were suitable for greater weight gains. The modelled growth responses of juvenile Murray cod are consistent with the predictions of the SDC, emphasising that changes in the bioenergetics of individuals are likely to be reflected in reduced growth rates under the changed flow velocity and temperature regimes imposed by disturbance gradients. This research represents a valuable step in the biological understanding of Murray cod within variable riverine environments and emphasises the urgency required to mitigate impacts associated with hypolimnetic impoundments.  相似文献   
8.
Determination of the threshold shear velocity is essential for predicting sand transport, dust release and desertification. In this study, a wind tunnel experiment was conducted to evaluate the influence of salinity and moisture on the threshold shear velocity of saline sand. Saline sand samples (mean particle size of 164.50-186.08 μm and the total silt, clay and salt content of 0.80%-8.25%) were collected from three saline sand dunes (one barchan dune and two linear dunes) in the Qarhan Desert, Qaidam Basin of China. Original saline sand samples were placed in two experimental trays for wet and dry processing to simulate deliquescence and desiccation, respectively. Surface moisture content ranging from 0.30% to 1.90% was generated by the steam method so that the saline sand can absorb water in a saturated water vapor environment. The motion of sand particles was determined by the observers with a solid laser. The laser sheet (0.80 cm thick), which was emitted by the solid laser, horizontally covered the sand surface and was bound to the sand. Results show that the cohesion of saline sand results from a combination of salt and water. The threshold shear velocity increases exponentially with the increase in crust thickness for the linear sand dunes. There is a positive linear correlation between the original moisture content and relative threshold shear velocity. The threshold shear velocity of dewatered sand is greater than that of wet sand with the same original moisture content. Our results will provide valuable information about the sand transport of highly saline soil in the desert.  相似文献   
9.
为探讨秃尾河流域径流量对气候变化的关系,利用秃尾河流域1970~2005年36 a来的气温、降水和天然径流量数据,对该流域气温、降水和径流量年际和季节性的变化特征及趋势进行了分析,研究了气候因子与径流量的相关性.研究结果表明:秃尾河流域年平均气温呈现明显升高趋势,以冬季升温为主;年降水表现为缓慢减少趋势,降水减少主要表...  相似文献   
10.
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