施磷量对黑木相思苗木生长的影响

为探究黒木相思苗木生长变化对磷肥的反映机制,本研究对1a生黑木相思(Acacia melanoxylon)苗木采用随机区组设计,设置了7个不同施肥量处理(0、50、75、100、125、150、200 mg P/株),测定并分析其苗高、地径、生物量及根系形态指标。结果表明：不同施磷量对苗木高生长、地径、生物量(地上部分、地下部分生物量)以及根系的生长都起促进作用,随时间和施磷量的增加,黑木相思根长、根平均直径、根表面积、根体积、苗高、地径、生物量总体表现均有所增加,总量为100 mg/株的等量施磷量对苗木生长促进作用效果最佳,试验结束时(即施肥第12 wk),该处理的根长、根表面积、根平均直径、根体积、苗高、地径、生物量(地上、地下部分)分别为417.09 cm、35.16 cm2、0.46cm、0.48cm3、36.2mm、2.30mm、1.236g(地上部分)、0.227g(地下部分),其中根长、根表面积、根平均直径、根体积分别比对照增加了81.2%、110.7%、61.2%和127.1%。     

土地利用方式对南方红壤养分状况的影响

土壤养分是土壤学研究重点,是衡量土壤生产力的综合指标,而土地利用方式则是人类活动影响土壤养分变化最直接、最重要、最普遍的因素。随着人类活动对土地利用的范围不断扩大、强度不断加剧,进而对土壤养分造成了不同程度的影响,尤其是对南方红壤的影响。目前,该区域土壤养分退化严重,综述近10年国内外的相关文献,在土地利用方式改变下,以土壤的物理性质、有机质、氮磷钾的动态变化趋势对土壤养分进行分析和总结,以期更准确地预测和评估不同管理措施对土壤质量的影响,并及时采取有效措施,调整生产结构,降低土壤环境污染,提高土壤性能。     

Effects of different soil management practices on total P and Olsen-P sediment loss: A field rainfall simulation study

Field rainfall simulations were conducted in 2002 and 2005 to study the effects of different soil management practices on the total phosphorous (TP) and Olsen-P losses by soil erosion and redistribution along a 15 m long slope in Luoyang, Henan province, China. Field plots were set up in 2001 and included the following soil management practices: subsoiling with mulch (SSM), no-till with mulch (NTM), reduced tillage (RT), and a conventional tillage control (CT). The results showed that there were no significant differences in TP and Olsen-P content in the sediment load between different plots after 6 years uniform tillage practices. The enrichment of TP and Olsen-P at the lower slope showed a clear redistribution along the slope. Effects of tillage practices on the temporal pattern of the enrichment ratio (ER) of TP and Olsen-P was not uniform. ER_TP values were initially high and diminished after a short period of time and leveled to the end of the rainfall test in CT and RT plots, but remained ≥ 1. The ER of Olsen-P at the end of rainfall simulation showed a significant difference when compared to the initial stage, 0.78 to 1.60, respectively. However, the temporal loss rate of TP and Olsen-P showed a similar pattern because it was more depending on the sediment loss rate than on the concentration in the sediment. SSM resulted in 96% less TP and Olsen-P erosion loss compared to CT in 2002. Also, SSM showed the highest reduction in TP and Olsen-P loss after 4 years consistent practice. RT reduced TP and Olsen-P loss by 30%, although the runoff reduction was not significant. NTM was the best alternative with respect to TP and Olsen-P conservation, when considering its lower operational costs.     

三峡库区澎溪河流域消落区土壤氮磷释放研究

通过模拟试验研究了温度和施肥对三峡库区澎溪河流域消落区冲积土、紫色土和水稻土氮磷释放的影响,估算了这3种土壤氮磷的释放量。结果表明,淹水后消落区土壤氮的释放潜力为水稻土冲积土紫色土,不同温度下消落土壤氮的释放潜力表现为20℃略高于10℃,明显高于30℃;消落区土壤间磷释放的差异因温度的不同而异,10℃时3种土壤间上覆水磷浓度相近,20℃和30℃时,土壤磷的释放潜力为冲积土紫色土水稻土,土壤磷的释放随淹水温度的提高而升高。按云阳县耕地平均施肥量(N0.21g/kg和P0.15g/kg)向消落区土壤施入氮磷肥,冲积土、紫色土和水稻土向水体释放的氮分别提高7.05～17.27,10.03～25.41,5.84～13.70倍,释放的磷分别提高1.47～4.88,4.99～16.49,1.18～3.03倍。根据澎溪河流域水温、水位变动情况及消落区土壤面积,估算出未施肥条件下澎溪河流域消落区冲积土、紫色土和水稻土的氮释放负荷为19.36,29.45,236.07t/a,磷释放负荷分别为0.49,0.94,1.91t/a。     

反硝化聚磷菌C18脱氮除磷特性研究

从城市生活污水处理厂好氧池活性污泥中筛选出的一株反硝化聚磷菌C18,经16S rDNA初步鉴定为假单胞菌(Pseudomonas grimontii)。C18在pH 6.5~7.5之间能正常生长,pH为7.5时,脱氮除磷效果最好。C18生长对温度没有特殊要求,当温度为30℃时,磷和氨氮去除率分别达到85.9%和83.6%。厌氧/缺氧最佳连续培养时间为厌氧2 h、缺氧4 h。     

Comparing Nutrient Availability in Low-Fertility Soils using Ion Exchange Resin Capsules

Assessing the nutrient status of low-input, low-fertility desert soils poses some unique challenges. Commonly used soil analysis procedures and resin capsules generally assess nutrient status of fertile agricultural soils. Ion-exchange resin capsules (Unibest Company, Bozeman, Mont.) provide a viable alternative. A study was conducted to determine effectiveness of resin capsules to extract low levels of nutrients applied to native soils. Loamy sand and sandy clay loam desert soils from Utah were treated with combinations of four rates of nitrogen (N) as ammonium nitrate (34–0–0), three rates of phosphorus (P) as phosphoric acid (0–72–0), and two rates of iron sulfate (FeSO₄·7H₂O) and zinc sulfate (ZnSO₄·7H₂O) (include an untreated control). Each soil treatment was implanted with a resin capsule placed into either 250 or 1000 cm³ of soil after addition of water equivalent to 50% field capacity and incubated for either 60 or 120 days at 25 °C. After the appropriate incubation time, capsules were washed and extracted using 2 M hydrochloric acid (HCl), and the extract was used to measure iron (Fe), ammonium (NH₄)-N, nitrate (NO₃)-N, sulfur (S), and zinc (Zn). Conventional soil tests were completed on incubated soils (60 or 120 days). Resin capsules reflected NH₄-N and P fertilizer applied at low rates in the loamy sand but not in the sandy clay loam. Neither Fe nor Zn application was reflected in resin capsules, but the accompanying S was clearly quantified. In comparison to conventional soil test procedures, resin capsule NH₄-N was clearly a better indicator than KCl-extractable NH₄-N; resin capsule NO₃-N was effective, but not as good an indicator as water extraction; and resin capsule P was reflective of soil applied P in loamy sand but not in sandy clay loam, whereas sodium bicarbonate was effective in both soils. Resin capsules show promise for use in low-input conditions, but additional understanding of interactions in variable soils is needed.     

Physiological and Nutritional Evaluation of the Application of Phosphite as a Phosphorus Source in Cucumber Plants

The aim of this study was to determine how different phosphite and phosphate rates applied together affect the growth and morphology parameters in cucumber plants as well as to characterize the nutritional and physiological state of phosphorus (P). Different foliar application rates of phosphite were applied to analyze subsequent biomass production, the relative growth rate, morphological parameters, P bioindicators, P forms, and P-use efficiency. The data suggest that the application of phosphite as a P fertilizer at a rate of ≥0.5 mM would be an appropriate and effective strategy under suboptimal conditions of phosphate in the growth medium, represented by 0.5 mM in our work, as it improved the growth parameters, number of flowers, leaf area, nutritional state of P, incorporation of P in structural organs, and P-use efficiency by the plant. The results indicate that the validity of the foliar use of phosphite as a P fertilizer in cucumber plants was subject to phosphate availability in the culture medium.     

不同维生素预混料对科宝肉鸡生长性能、胫骨质量和抗氧化能力的影响

试验研究3种维生素预混料(处理1、2、3)对科宝肉鸡生长性能、胫骨质量及抗氧化能力的影响。1 200只科宝肉鸡随机分为3个处理,每个处理10个重复,每个重复40只鸡,试验期42 d。结果表明:与处理1相比,处理3和2可显著提高肉鸡21 d体重,显著降低1～21 d饲料增重比;处理3还显著提高肉鸡1～21 d体增重、采食量和21 d胫骨灰分和磷比例及42 d胫骨灰分、钙比例(P<0.05);与处理2相比,处理3显著提高肉鸡42 d胫骨磷比例(P<0.05)。与处理2和1相比,处理3显著提高肉鸡21 d血清总超氧化物歧化酶(T-SOD)活力(P<0.05)。结果表明,根据科宝肉鸡的生长性能、胫骨质量和机体抗氧化能力,适宜维生素预混料为处理3。     

抚仙湖流域坡耕地施肥对土壤水中氮磷质量浓度的影响

在滇中地区抚仙湖尖山河小流域坡耕地布设9个不同施肥水平的微型小区,在微型小区及不同坡位的不同深度埋设多孔杯采样器,采集土壤水样,分析其中总氮和总磷的质量浓度变化特征。结果表明:1)施肥量增大,土壤水中总氮、总磷平均质量浓度增大1,.5和2.0倍施肥处理条件下,0～100 cm土层土壤水总磷质量浓度分别是标准施肥量的1.26和1.63倍;2)同一施肥处理条件下,坡下部土壤水总氮、总磷质量浓度基本高于坡中部0,～50 cm坡下部总氮平均质量浓度约为坡中部的1.30倍,0～100 cm坡下部土壤水总磷平均质量浓度约为坡中部的2.0倍;3)同一施肥处理条件下,随着土层深度的加深,土壤水总氮质量浓度逐渐减小0,～50、50～100、100 cm以下土壤水总氮平均质量浓度分别为4.58、3.93和3.17 mg/L;土壤水总磷质量浓度在50 cm以下呈波浪状减小,在0～100 cm变化较大(0.010～0.021 mg/L),在100 cm以下差异较小(0.010～0.014 mg/L);4)在坡耕地种植烤烟时应将施氮量控制在270.0 kg/hm2以下,施磷量要控制在61.2 kg/hm2以下。     

洞庭湖红壤坡地减氮控磷对玉米产量和径流氮磷的影响

坡地氮磷流失是洞庭湖农业面源污染的重要来源。以湖南省湘阴县红壤坡耕地土壤为研究对象,通过田间小区试验,探讨玉米减量施肥对产量、化肥利用率和氮磷流失量的影响。结果表明,NP常规施肥量在减少20%范围内对玉米产量没有十分显著的影响,但达到30%时玉米表现减产。减量施肥不仅一定程度提高NP化肥肥效和肥料利用率,而且降低土壤NP流失量。氮的径流量减少了12.54%～28.68%,磷减少了1.3%～30.1%。在各种减量施肥处理中,以控释肥减氮处理效果最佳,有效减少农业面源污染。