内蒙古高原紫花苜蓿土壤氮素丰缺指标和推荐施氮量     

米春娇  孙洪仁  王显国  高凯  张玉霞  刘庭玉 《草地学报》2021,29(12):2785-2791

为了给内蒙古高原紫花苜蓿（Medicago sativa L.）测土施氮奠定科学基础，本研究采用“零散实验数据整合法”和“养分平衡-地力差减法”新应用公式，开展了该自然区域紫花苜蓿土壤氮素丰缺指标和推荐施氮量研究。结果表明：内蒙古高原生长第1年紫花苜蓿土壤碱解氮第1~6级丰缺指标为≥48，20~48，8~20，4~8，2~4和<2 mg·kg^-1，土壤全氮第1~5级丰缺指标为≥1.4，0.8~1.4，0.4~0.8，0.2~0.4和<0.2 g·kg^-1，土壤有机质第1~6级丰缺指标为≥17，10~17，6~10，3~6，2~3和<2 g·kg^-1。当紫花苜蓿目标产量9~18 t·hm^-2、氮肥利用率40%时，内蒙古高原紫花苜蓿第1~6级土壤推荐施氮量分别为0，68~135，135~270，203~405，270~540和338~675 kg·hm^-2。  相似文献   

柑橘幼果发育期碳水化合物代谢及其与生长发育的关系   总被引：1，自引：0，他引：1  

徐昌杰  张上隆 《果树学报》2001,18(1):20-23

温州蜜柑幼果在盛花后逐渐生长 盛花后6 d开始大量脱落 日本甜夏橙幼果在盛花后12 d内重量未增加，一直处于急剧落果期。甜夏橙幼果中蔗糖含量高出温州蜜柑20多倍，种间还原糖含量变化趋势略有不同。两种柑橘的淀粉含量变化也不同，但它们的淀粉含量与淀粉酶活性、幼果相对脱落率均呈负相关。对幼果碳水化合物代谢与生长、脱落的关系作了讨论。  相似文献   

姜片虫虫体抗原氨基酸的测定   总被引：1，自引：0，他引：1  

喻诚沼  马细妹  任园 《江西农业大学学报》1989,(1)

本文报道4种方法制备姜片虫虫体抗原,进行氨基酸组成的测定。其氨基酸总量(mg/100ml)结果显示:Ag-F1:608.50;Ag-F2:645.80;Ag-F3:357.14;Ag-F4:501.40;以 Ag-F3总量为最低,但值得重视的是 Ag-F3的丙氨酸(8.34),组氨酸(8.60),甘氨酸(11.00);苏氨酸(12.00),均显著降低。而 Ag-F4的组氨酸(4.80)为17种氨基酸含量最低者。其原因有待探讨。  相似文献   

东北梅花鹿茸不同部位水解氨基酸含量的比较分析   总被引：2，自引：1，他引：1  

王艳梅  邹兴淮 《经济动物学报》2003,7(4):18-21

对 10支东北梅花鹿茸作了不同部位水解氨基酸含量的比较分析 ,结果表明 ,水解氨基酸含量在东北梅花鹿茸腊片、粉片、血片和骨片各部位之间差异极显著 (P <0 0 1)。  相似文献   

以豆粕为原料制备反刍动物饲用肽的研究     

王雅晶  李胜利  骆雅萍  李静 《中国饲料》2005,(20):15-17

本文通过正交试验,选用碱性微生物蛋白酶,研究得出酶解法制备大豆肽的最佳工艺参数:豆粕预处理条件为90℃水浴加热10min,酶解条件为底物浓度5%(W/V)、加酶量5万单位/g蛋白质、温度50℃、pH值10、酶解时间5.5h。蛋白质水解率达到25%,平均肽链长度为4.0。制得大豆肽粗蛋白质含量66.83%(DM)。并对制得大豆肽和原料豆粕的氨基酸含量进行分析。  相似文献   

套袋对红富士苹果色素及糖、酸含量的影响   总被引：58，自引：4，他引：58  

王少敏  高华君  张骁兵 《园艺学报》2002,29(3):263-265

 以苹果(Malus pumila) ‘长富2’品种为试材, 研究了套袋对果皮色素及果肉糖、酸含量的影响。结果表明, 套袋果果皮色素、可溶性糖、可滴定酸具有同对照果基本相同的消长规律, 但含量均始终低于对照; 摘袋后果实可溶性糖含量迅速升高, 且花青苷积累速度明显快于对照; 套袋主要降低了果实中山梨醇和蔗糖的含量, 果糖和葡萄糖降低幅度相对较小。  相似文献   

More evidence that anaerobic oxidation of methane is prevalent in soils: Is it time to upgrade our biogeochemical models?     

《Soil biology & biochemistry》2015

Estimating future fluxes of CH₄ between land and atmosphere requires well-conceived process-based biogeochemical models. Current models do not represent the anaerobic oxidation of methane (AOM) in land surface soils, in spite of increasing evidence that this process is widespread. Our objective was to determine whether AOM, or potential AOM, commonly occurs in 20 hydromorphic soils spanning a wide range of chemical properties. Bulk soil samples were collected under shallow water near the shoreline of 15 recently drained fish ponds in southern Bohemia (Czech Republic), as well as from below the water table at 3 peatland locations in northeast Scotland and 2 acid sulfate soils on the southern coast of Finland. Each soil slurry was incubated under both oxic and anoxic conditions, with or without the addition of alternative electron acceptors (SO₄²⁻ and NO₃⁻) or H₂PO₄⁻. Here, “oxic” and “anoxic” conditions refer to anoxic soil respectively incubated in a headspace containing air or argon. Using the isotope dilution method, we determined the gross production and oxidation rates of CH₄ after 2 days incubation under oxic headspace conditions, and after 2, 21 and 60 days incubation under anoxic conditions. Large differences in net CH₄ fluxes were observed between soil types and between incubation conditions. AOM was detected in each of the 20 bulk soil samples, which spanned >6 pH units and 2 orders of magnitude in organic C content. Significant positive relationships were found between AOM and gross CH₄ production rates under anoxic conditions, resulting in AOM rates that were sometimes higher than CH₄ oxidation rates under oxic headspace conditions. There was no relationship between net and gross CH₄ production rates, such that 2 soil types could display similar low net rates, yet conceal very large differences in gross rates. The effects of alternative electron acceptors on AOM were idiosyncratic and resulted in no net trend. We did find, however, a negative effect of SO₄²⁻ and H₂PO₄⁻ on gross CH₄ production rates under anoxic and oxic conditions respectively. Under oxic headspace conditions, CH₄ oxidation was related to soil organic C content. Taken collectively, our results suggest that AOM, or potential AOM, is prevalent over a wide range of soil types, that AOM may contribute substantially to CH₄ oxidation in soils, and that AOM in soils should be integrated to current process-based CH₄ cycling models.  相似文献   

碳纳米管的酸化处理对碳纳米管/聚氨酯复合材料微观结构及性能的影响     

张岚  顾继友  姜宪凯 《东北林业大学学报》2011,39(2):75-78

对多壁碳纳米管进行酸化处理,并采用原位聚合法制备了碳纳米管/聚氨酯复合材料。利用X射线光电子能谱分析(XPS)、电子扫描显微镜(SEM)、动态力学分析(DMA)研究了碳纳米管酸化与否对复合材料性能的影响。结果表明,碳纳米管经酸化处理后产生了羧基,碳纳米管的原位加入使得复合材料的储存模量和玻璃化转变温度都有所提高,而且经过酸化的碳纳米管对聚氨酯材料的改性要比未酸化碳纳米管对聚氨酯材料的改性效果更为显著。  相似文献   

石榴果实的糖酸组成及风味特点   总被引：2，自引：0，他引：2  

秦改花  黄文江  赵建荣  邓盾  周玉丽 《热带作物学报》2011,32(11):2148-2151

采用高效液相色谱法测定4种石榴成熟期果实中糖和酸的组成,并对其味感值和糖酸组分与果实风味指标间的相关性进行分析。结果表明,石榴果实中可溶性糖组分有蔗糖、葡萄糖、果糖和山梨醇,其中葡萄糖和果糖含量最高,分别占总糖含量的43.84%~48.36%和49.18%~50.67%。4个品种中,"玉石籽"的总糖含量最高,"白皮"的最低。石榴果实中主要有机酸是奎宁酸、琥珀酸、草酸、L-苹果酸、莽草酸、柠檬酸和D-苹果酸,其中"玛瑙籽"的总酸含量最高,"青皮"的最低。石榴果实中果糖的味感值最大、其次是葡萄糖;味感值最大的酸是奎宁酸,其次为柠檬酸。相关性分析结果表明,石榴果实的糖酸比与甜味/酸味比值之间呈极显著正相关,各品种间糖酸比(甜味/酸味比值)的差异主要取决于有机酸的含量,与糖含量无关。综合其风味特点,"青皮"和"玉石籽"是甜味较浓的品种,"白皮"和"玛瑙籽"则是酸味较浓的品种。  相似文献   

用酶法制备藏羊血食用蛋白粉的研究     

胡勇  靳义超  吴海玥  仇桂芳  韩银仓  冶成君 《青海畜牧兽医杂志》2011,41(5):14-15

采用四因素三水平正交试验,对藏羊血制备食用蛋白的工艺进行了分析。经分析食用蛋白粉水解最佳条件为：酶解用酶量4.5g,酶解温度为46℃,酶解时间为7.5h,酶解的pH值为10.5,活性炭作用于水解液时由室温升至80℃所需最佳时间为6～8min。  相似文献