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1.
注重培养学生的绿色创新思维是当今国际人才教育发展的大趋势。该文针对目前农业院校无机化学教育体系中存在的一些问题,并结合高等农业院校所具有的独特优势,提出了在无机化学教学中注入绿色创新思维培养,并对培养的具体方法和途径进行了探讨,进而激发大学生们对无机化学学习的热情和兴趣。  相似文献   
2.
在保护地栽培,高肥力土壤条件下,研究施用天然复合酵素剂SS-200对菠菜、黄瓜生长发育、产量和品质的影响。结果表明:与常规施用化学肥料相比,施用天然复合酵素剂SS-200,有利于菠菜、黄瓜上的生长发育,其叶片数,茎粗,株高都有显著增加;施用天然复合酵素剂SS-200增加了菠菜产量,增产达到24.5%,也提高黄瓜的果实产量,平均1 hm2可以增产13.9%;同时施用SS-200菠菜叶柄中的硝酸盐含量降低了700 mg/L,达到9.2%,而SS-200对黄瓜的可溶性糖和Vc含量影响不大;由于肥料投入的降低及产量的增加,1 hm2菠菜的利润达到55 284元/hm2,黄瓜的利润也达到了67 082元/hm2。  相似文献   
3.
甘蓝型油菜种子无机磷含量变异的初步分析   总被引:5,自引:1,他引:5  
以微量比色法对100个甘蓝型油菜品种的种子无机磷含量进行初步检测,发现不同甘蓝型油菜品种之间种子无机磷含量存在一定差异。大部分品种的成熟种子中无机磷含量为0.2-0.4μg/g,有2个品种的无机磷含量达到0.7μg/g,1个品种超过1.1μg/g。  相似文献   
4.
根据2018年5、8月莱州湾的生态调查资料,采用营养盐限制法则及潜在性富营养化评价模式等方法,对莱州湾无机氮(DIN)、活性磷酸盐(PO34–-P)和硅酸盐(SiO23–-Si)的平面分布、结构及限制特征进行了分析。结果显示,2018年5、8月莱州湾的DIN浓度范围为1.64~106.36 μmol/L,平均值为24.18 μmol/L,5月明显高于8月;PO34–-P浓度范围为0~2.010 μmol/L,平均值为0.182 μmol/L,8月明显高于5月;SiO23–-Si浓度变化范围为0.97~78.93 μmol/L,平均值为18.30 μmol/L,8月明显高于5月。DIN、PO34–-P、N/P高值区主要位于莱州湾西部的小清河口和黄河口附近海域;SiO23–-Si、Si/N、Si/P高值区主要位于湾底部、龙口–莱州近岸海域。对营养盐结构的分析表明,莱州湾存在明显的磷限制和枯水期的硅限制,陆源输入是莱州湾营养盐的主要来源。营养盐结构限制平面分布表明,春季莱州-招远养殖区和夏季东营-潍坊养殖区易引发赤潮,夏季莱州–招远养殖区初级生产力受到一定限制,对养殖业造成一定的影响。  相似文献   
5.
Sustainable soil and crop management practices that reduce soil erosion and nitrogen (N) leaching, conserve soil organic matter, and optimize cotton and sorghum yields still remain a challenge. We examined the influence of three tillage practices (no-till, strip till and chisel till), four cover crops {legume [hairy vetch (Vicia villosa Roth)], nonlegume [rye (Secaele cereale L.)], vetch/rye biculture and winter weeds or no cover crop}, and three N fertilization rates (0, 60–65 and 120–130 kg N ha−1) on soil inorganic N content at the 0–30 cm depth and yields and N uptake of cotton (Gossypium hirsutum L.) and sorghum [Sorghum bicolor (L.) Moench]. A field experiment was conducted on Dothan sandy loam (fine-loamy, siliceous, thermic, Plinthic Paleudults) from 1999 to 2002 in Georgia, USA. Nitrogen supplied by cover crops was greater with vetch and vetch/rye biculture than with rye and weeds. Soil inorganic N at the 0–10 and 10–30 cm depths increased with increasing N rate and were greater with vetch than with rye and weeds in April 2000 and 2002. Inorganic N at 0–10 cm was also greater with vetch than with rye in no-till, greater with vetch/rye than with rye and weeds in strip till, and greater with vetch than with rye and weeds in chisel till. In 2000, cotton lint yield and N uptake were greater in no-till with rye or 60 kg N ha−1 than in other treatments, but biomass (stems + leaves) yield and N uptake were greater with vetch and vetch/rye than with rye or weeds, and greater with 60 and 120 than with 0 kg N ha−1. In 2001, sorghum grain yield, biomass yield, and N uptake were greater in strip till and chisel till than in no-till, and greater in vetch and vetch/rye with or without N than in rye and weeds with 0 or 65 kg N ha−1. In 2002, cotton lint yield and N uptake were greater in chisel till, rye and weeds with 0 or 60 kg N ha−1 than in other treatments, but biomass N uptake was greater in vetch/rye with 60 kg N ha−1 than in rye and weeds with 0 or 60 kg N ha−1. Increased N supplied by hairy vetch or 120–130 kg N ha−1 increased soil N availability, sorghum grain yield, cotton and sorghum biomass yields, and N uptake but decreased cotton lint yield and lint N uptake compared with rye, weeds or 0 kg N ha−1. Cotton and sorghum yields and N uptake can be optimized and potentials for soil erosion and N leaching can be reduced by using conservation tillage, such as no-till or strip till, with vetch/rye biculture cover crop and 60–65 kg N ha−1. The results can be applied in regions where cover crops can be grown in the winter to reduce soil erosion and N leaching and where tillage intensity and N fertilization rates can be minimized to reduce the costs of energy requirement for tillage and N fertilization while optimizing crop production.  相似文献   
6.
采用室内土柱模拟试验,研究在山东平均降雨条件下不同施磷量对褐土各组分无机磷含量及形态转化的影响.结果表明,经过模拟降雨后,在0~10 cm土层中,各施磷处理的无机磷总量随着施磷量的增加而升高;随着土层的加深(10~50 cm),各土层无机磷总量是施磷量为P2(180 kg/hm2)时最高.而在10-30 cm土层,是施磷量为P3(1440 ks/hm2)的土壤无机磷总量高于P1,而在30~50 cm则是P1高于P3.同时,不同施磷量对磷组分含量及其占无机磷总量的比例都发生了改变,当施磷量分别为P1、P2和P3时,各无机磷组分的含量及所占比例按高低排序分别为:Ca10-P>Al-P,O-P>Ca8-P>Fe-P>Ca2-P;O-P>Ca8-P,Ca10-P>Fe-P,AI-P>Ca2-P和Ca10-P,O-P>Fe-P,Ca8-P>Al-P>Ca2-P.随着土层深度的加深,O-P、Fe-P和Ca10-P的含量保持相对稳定,而有效态无机磷源(Ca2-P、Ca8-P和AI-P)有降低的趋势;在小雨强度下,不同施磷量处理的土壤磷淋失量差异不显著,而随着降雨强度的加大,P3处理的土壤磷淋失量明显高于PI和P2处理的磷淋失量.以上结果说明,施磷量显著影响无机磷总量、各组分无机磷含量及其转化;在大于中等降雨条件下,高磷处理磷淋失量明显高于低磷处理磷淋失量.  相似文献   
7.
 Soil organic matter level, mineralizable C and N, microbial biomass C and dehydrogenase, urease and alkaline phosphatase activities were studied in soils from a field experiment under a pearl millet-wheat cropping sequence receiving inorganic fertilizers and a combination of inorganic fertilizers and organic amendments for the last 11 years. The amounts of soil organic matter and mineralizable C and N increased with the application of inorganic fertilizers. However, there were greater increases of these parameters when farmyard manure, wheat straw or Sesbania bispinosa green manure was applied along with inorganic fertilizers. Microbial biomass C increased from 147 mg kg–1 soil in unfertilized soil to 423 mg kg–1 soil in soil amended with wheat straw and inorganic fertilizers. The urease and alkaline phosphatase activities of soils increased significantly with a combination of inorganic fertilizers and organic amendments. The results indicate that soil organic matter level and soil microbial activities, vital for the nutrient turnover and long-term productivity of the soil, are enhanced by use of organic amendments along with inorganic fertilizers. Received: 6 May 1998  相似文献   
8.
 The phosphate-solubilizing potential of the rhizosphere microbial community in mangroves was demonstrated when culture media supplemented with insoluble, tribasic calcium phosphate, and incubated with roots of black (Avicennia germinans L.) and white [Laguncularia racemosa (L.) Gaertn.] mangrove became transparent after a few days of incubation. Thirteen phosphate-solubilizing bacterial strains were isolated from the rhizosphere of both species of mangroves: Bacillus amyloliquefaciens, Bacillus licheniformis, Bacillus atrophaeus, Paenibacillus macerans, Vibrio proteolyticus, Xanthobacter agilis, Enterobacter aerogenes, Enterobacter taylorae, Enterobacter asburiae, Kluyvera cryocrescens, Pseudomonas stutzeri, and Chryseomonas luteola. One bacterial isolate could not be identified. The rhizosphere of black mangroves also yielded the fungus Aspergillus niger. The phosphate-solubilizing activity of the isolates was first qualitatively evaluated by the formation of halos (clear zones) around the colonies growing on solid medium containing tribasic calcium phosphate as a sole phosphorus source. Spectrophotometric quantification of phosphate solubilization showed that all bacterial species and A. niger solubilized insoluble phosphate well in a liquid medium, and that V. proteolyticus was the most active solubilizing species among the bacteria. Gas chromatographic analyses of cell-free spent culture medium from the various bacteria demonstrated the presence of 11 identified, and several unidentified, volatile and nonvolatile organic acids. Those most commonly produced by different species were lactic, succinic, isovaleric, isobutyric, and acetic acids. Most of the bacterial species produced more than one organic acid whereas A. niger produced only succinic acid. We propose the production of organic acids by these mangrove rhizosphere microorganisms as a possible mechanism involved in the solubilization of insoluble calcium phosphate. Received: 21 April 1999  相似文献   
9.
利用盆栽试验研究了几种人工合成磷源在轻粘质潮土根际和本体土壤中的形态转化及配施不同形态氮肥对其形态转化的影响 ,结果表明 ,作物耗竭引起根际所有形态无机磷不同程度的下降。施入土壤的DCP(CaHPO4 ·2H2 O)、OCP(Ca8(PO4 ) 6 )、Al P(AlPO4 ·nH2 O)等大部分转化为其它形态无机磷 ,而Fe P(FePO4 ·nH2 O)和FA(Ca10 (PO4 ) 6 F2 )大部分以自身形态存在 ,尤其是FA很少向其它形态转化 ,根际条件促进了它们向其它无机磷形态的转化。Al P和FA等的形态转化明显受氮肥形态的影响 ,Al P配施NO- 3 N下 ,绝大部分转化为磷灰石 ,NH 4 N配施下促进了FA向其它形态的转化 ,在所有的磷源处理中 ,根际和本体磷酸铁都有显著地增加 ,NH 4 N和CO(NH2 ) 2 处理下存在磷酸铁的根际累积 ;其次是磷酸二钙和磷酸铝也有明显地增加 ,二者存在根际的亏缺。不同磷源的形态转化规律与其有效性大小相一致。  相似文献   
10.
在北京郊区中壤质潮土上设置田间试验。结果表明:花椰菜获最大产量的氮供应量为300kghm-2。生育期花椰菜主要吸收表层(0~30cm)土壤中的无机氮,对下层(30~60cm)土壤无机氮(Nmin)的利用随氮供应量的增加而减少。不同生育期0~60cm土层中无机氮(Nmin)含量均随氮供应量增加而增加,但施肥后土壤中最高无机氮(Nmin)含量出现的时间随氮供应量增加而延迟。花椰菜生育期土壤有机氮矿化速率随生长期延长而增加,平均达N1.3kghm-2d-1,相当于各处理总吸氮量的47.5%~89.2%。试验后0~30cm及30~60cm土层无机氮(Nmin)含量随氮供应量增加而明显增加,但60~90cm土层无机氮(Nmin)受氮供应的影响不明显。花椰菜当季氮肥利用率及氮素利用率随施氮量增加而降低,最佳产量时的氮肥利用率及氮素利用率分别为36.5%和50.8%。土壤-花椰菜体系氮素表观损失量随氮施用水平的增加而明显增加,但其占总氮供应(肥料氮+播前土壤氮)的比例受氮供应的影响不明显,大致为20%。  相似文献   
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