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31.
地道潞党参营养特性与产地土壤特征研究 总被引:3,自引:1,他引:2
通过现场调查和实验室分析相结合的方法,对山西省潞党参营养特性和产地土壤特征进行了综合分析研究。结果表明,地道潞党参主要分布在海拔1000~1700 m的中低山上,降雨量大,气候冷凉湿润,昼夜温差大。产地土壤成土母质主要为黄土母质和堆垫母质,土壤类型为褐土性土,土壤质地以壤土为主,土壤有机质和有效养分含量高,形成地道潞党参生长独特的生态环境。地道潞党参营养元素中氮、磷、钾和铁、锰含量高,尤其是铁的含量较高,对部分微量元素有奢侈吸收的现象,而且主要分配到地下部分,形成地道潞党参独特的营养特性。 相似文献
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市郊菜园土壤污染及治理 总被引:11,自引:0,他引:11
针对衡阳市郊菜园土壤受到污染的实际,分析了主要污染源,提出了控制与治理污染的措施。 相似文献
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在一个连续进行了 8年N肥定位试验的酸樱桃园,调查了每年施用 N60 kg· hm~(-2)和行间生草制对土壤营养状况的影响。结果表明:在肥沃土壤里NH_4~+是速效N的主要存在形式,而NO_3~-的含量很低。生草地土壤中含有较多的 NH_4~-,而清耕带土壤中含有较多的 NO_3~-。施肥增加土壤速效 N的含量。土壤 NO_3~-的季节性变化表明 5至 6月份土壤中 NO_3~-的含量高,而花前和 7月份土壤中 NO_3~-含量低。 P、K在清耕带 10 cm以下土壤的含量低于生草地土壤,但在 0~ 10cm土层中K的含量高于生草地。P的含量不受影响。施N减少了土壤P、K的含量。土壤中Mg的含量分布均匀,不受施N和地面管理制度的影响。 相似文献
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Fertilizer recommendations for citrus production on heavier textured, calcareous soils increase with the age of the tree up to 168 kg N ha−1 year−1 from a soluble source in one or two applications. Such practices may be inefficient and could cause detrimental effects on fruit quality. A variety of fertilization practices are used in South Texas, and additional evaluation is needed. Rates and sources of nitrogen (N), phosphorus (P), and a commercial program consisting of both a soil component containing organic acids and a foliar component were evaluated on grapefruit production for 6 years. Increasing rate of N application increased leaf nutrient concentration, grapefruit yield, and affected fruit shape as indicated by a decrease in the equatorial:polar diameter (E:P) ratio. Since the response to increasing N application by the E:P ratio was linear while grapefruit yield was quadratic, high N application has a negative effect on fruit shape beyond the level of increasing total yield. Phosphorus application had no effect on any parameter measured, even though soil testing indicated soil P levels were below those at which a P response would be expected. Comparisons between granular 21-0-0 applied broadcast and liquid N-32 injected in a band in the soil at the drip line showed an increase in the number of fruit per tree, but no differences in yield. The ‘Actagro’ program greatly improved available soil P levels and increased the juice brix:acidity ratio, but did not affect grapefruit yield. Phosphorus availability may therefore be a factor in improving grapefruit juice quality. The soil profile within the citrus root zone was found to contain large amounts of inorganic N, but availability of this residual N was limited since yield responses occurred at the N application rates applied in this study. The amount of N contained in the fruit harvested was a small fraction, roughly 5–10%, of the residual amount in the soil. While N uptake in the fruit increased with N fertilizer application, the increase in N taken up relative to the amount applied averaged 42%. 相似文献
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This research aims to improve erosion control practice in the Loess Plateau, by studying the surface erosion processes, including splash, sheet/interrill and rill erosion in four contrasting soils under high rainfall intensity (120 mm h−1) with three-scale indoor artificial experiments. Four contrasting soils as sandy loam, sandy clay loam, clay loam and loamy clay were collected from different parts of the Loess Plateau. The results showed that sediment load was significantly impacted by soil properties in all three sub-processes. Splash rate (4.0–21.6 g m−2∙min−1) was highest in sandy loam from the north part of the Loess Plateau and showed a negative power relation with the mean weight diameter of aggregates after 20 min of rainfall duration. The average sediment load by sheet/interrill erosion (6.94–42.86 g m−2∙min−1) was highest in clay loam from middle part of the Loess Plateau, and the stable sediment load after 20 min showed a positive power relation with the silt content in soil. The average sediment load increased dramatically by rill and interrill erosion (21.03–432.16 g m−2∙min−1), which was highest in loamy clay from south part of the Loess Plateau. The average sediment load after the occurrence of rill showed a positive power relation with clay content and a negative power relation with soil organic matter content. The impacts of slope gradient on the runoff rate and sediment load also changed with soil properties. The critical factors varied for different processes, which were the aggregate size for splash erosion, the content of silt particles and slope gradient for sheet/interrill erosion, and the content of clay particles, soil organic matter and slope gradient for rill erosion. Based on the results of the experiments, specific erosion control practices were proposed by targeting certain erosion processes in areas with different soil texture and different distribution of slope gradient. The findings from this study should support the improvement of erosion prediction and cropland management in different regions of the Loess Plateau. 相似文献