Long-Term Effect of Fertilizer and Rice Straw on Mineral Composition and Potassium Adsorption in a Reddish Paddy Soil

Increasing K⁺ adsorption can be an effective alternative in building an available K pool in soils to optimize crop recovery and minimize losses into the environment. We hypothesized that long-term fertilization might change K⁺ adsorption because of changes in the chemical and mineralogical properties of a rice (Oryza sativa L.). The aims of this study were (i) to determine clay minerals in paddy soil clay size fractions using X-ray diffraction methods and a numerical diagram-decomposition method; (ii) to measure K⁺ adsorption isotherms before and after H₂O₂ oxidation of organic matter, and (iii) to investigate whether K⁺ adsorption is correlated with changes in soil chemical and mineral properties. The 30-yr long-term fertilization treatments caused little change in soil organic C (SOC) but a large variation in soil mineral composition. The whole-clay fraction (<5 μm) corresponded more to the fertilization treatment than the fine-clay fraction (<1 μm) in terms of percentage of illite peak area. The total percentage of vermiculite-chlorite peak area was significantly negatively correlated with the total percentage of illite peak area in the <5 μm soil particles (R=-0.946, P<0.0006). Different fertilization treatments gave significantly different results in K⁺ adsorption. The SOC oxidation test showed positive effects of SOC on K⁺ adsorption at lower K⁺ concentration (?120 mg L^?1) and negative effects at higher K⁺ concentration (240 mg L^?1). The K⁺ adsorption by soil clay minerals after SOC oxidization accounted for 60–158% of that by unoxidized soils, suggesting a more important role of soil minerals than SOC on K⁺ adsorption. The K⁺ adsorption potential was significantly correlated to the amount of poorly crystallized illite present (R=0.879, P=0.012). The availability of adsorbed K⁺ for plant growth needs further study.     

集雨栽培冬小麦田土壤水分和矿质氮

在半湿润易旱地区的关中红油土上,研究了垄上覆膜集雨栽培措施对冬小麦(Triticumaestivum)田土壤水分和矿质氮的影响。结果表明覆膜有一定的蓄水保墒效果,冬小麦返青期,0～40cm土壤贮水量覆膜处理比不覆膜处理平均多7.7mm;覆膜能使冬小麦在生长后期更有效地利用土壤深层贮水,在小麦成熟期,100～200cm土壤贮水量覆膜处理比未覆膜处理少23.8mm。覆膜有利于作物对氮肥的吸收利用,氮肥用量相同的处理,覆膜条件下的硝态氮浓度和矿质氮累积量低于不覆膜处理;施氮也可以明显增加土壤剖面中的硝态氮含量和矿质氮累积量。     

Concentrations of macro- and micro-elements in the milk of pasture-fed thoroughbred mares

OBJECTIVE: To determine the changes in Ca, P, Mg, Na, K, S, Cu, Fe and Zn concentrations of milk during the lactation in pasture-fed Thoroughbred mares and then calculate the dietary mineral requirements of the sucking foal and the lactating mare. PROCEDURE: Milk was sampled on days 1, 3, 7, 14, 21, 28 and at various times between 55 to 65, 85 to 95 and 135 to 150 days after parturition from 21 pasture-fed mares. The concentrations of macro- and micro-elements in the milk were determined by inductively coupled plasma emission spectrometry. RESULTS: Concentrations (mg/L) of these elements were highest in colostrum (Mg 302, Na 561, K 955, S 1035, Cu 0.76, Fe 0.79 and Zn 5.5) except for Ca (1245) and P (895), which where highest on day 7. The mean milk mineral element concentrations (mg/L) over days 55 to 150 were Ca 843, P 543, Mg 47, Na 120, K 590, S 219, Cu 0.19, Fe 0.34 and Zn 2.1. The mean plasma element concentrations (mg/L) over the same period were Ca 120, P 77.1, Mg 17.0, Na 3110, K 168, S 983, Cu 1.1, Fe 1.5 and Zn 0.49. Concentration gradients between plasma and milk were observed and, in the case of Ca, P, Mg, K and Zn, their concentrations in milk were greater than those in plasma, while a reverse situation was observed for Na, S, Cu and Fe. CONCLUSION: With the exception of Ca and P, the highest concentrations of mineral elements were observed in the colostrum. The nursing foal should have access to good pasture or creep feed, because the intakes of Ca, P and Cu from milk may be less than optimum to meet the daily mineral element requirements.     

钙锌对蛋用型鸡育成期体组织中矿物元素含量的影响

试验研究了在玉米—豆饼型基础饲粮中添加不同水平锌和钙对蛋用型鸡育成期体组织中矿物元素含量的影响。结果表明,随着饲粮锌水平的提高,肝脏(P<0.01)、肾脏(P<0.05)、胰脏(P<0.01)中锌含量显著升高,而肺脏中锌含量没有显著变化(P>0.05)。饲粮高钙对组织中锌含量的影响未达到显著水平(P>0.05)。饲粮高锌使肝脏磷含量(P<0.05)、肾脏磷(P<0.01)和铜含量(P<0.05)、肺脏钙(P<0.01)和镁含量(P<0.01)显著降低。饲粮商钙使胰脏铜含量(P<0.05)显著提高,使胰脏锰含量显著降低(P<0.05)。     

氮素形态不同配比对黄瓜生长和性别分化的影响（初报）

采用基质培养研究氮素形态不同配比对黄瓜生长及性别分化的影响,结果表明用纯NO3--N营养液处理,黄瓜植株营养生长旺盛,当NH4 -N占25％和50％时,黄瓜的生殖生长明显促进,表现为比纯NO3--N处理第一雌花低0.4、0.6节,雌花率增加了23.9％、31.0％,单株产量增加了35.3％、28.7％。叶片和果实中矿物元素钾增加了0.02％～1.41％,铁增加了11～124,ug/g DW,锌增加了37.6～47.0μg/g DW,镁、锰、铜差异不大。黄瓜在不同生育期对氮素形态的敏感性有差异,幼苗期比生长旺盛期不敏感。     

Bone mineral changes in growing, pregnant and lactating cattle

Bone mineral content (BMC) was determined in one or two coccygeal vertebrae by dichromatic photon absorptiometry in two sets of cattle: A. This set consisted of six fattening bulls. Their increases of BMC and weights were closely correlated. However, BMC increased slightly more than weight. B. There were 28 cows in this set. BMC was measured during lactation and pregnancy. It was found that BMC increased during the dry period and decreased during early lactation. There were great individual variations in BMC, and the skeletal turnover seemed to be great.     

土壤脱湿过程中NaCl胁迫对羊草生长和矿质元素吸收的影响

用不同盐分浓度的NaCl中性盐对羊草进行胁迫,探讨在土壤脱湿过程中,NaCl胁迫对羊草生长和矿质元素吸收分配的影响。结果表明,当土壤溶液NaCl浓度小于125mmol/L(土壤总盐小于o．34％)时,盐分胁迫对羊草株高、根长、干物质积累量和相对生长率(RGR)无显著影响,且根系的钾钠吸收选择性和运输选择性随盐度处理水平的增加而增强。但当NaCl浓度超过225mmol/L(土壤总盐大于0．53％)后,其株高、根长、干物质积累量和相对生长率(RGR)随盐度增加而显著降低(P＜0．05),根系的钾钠吸收选择性和运输选择性也随盐度处理水平的增加而逐渐减弱。NaCl胁迫条件下,羊草对K、Ca的比吸收率(SAR)降低,茎叶K、Ca含量随盐度的增加显著减少(P＜0．05),Na、Cl含量则均随盐度的增加而显著提高,植株K／Na降低。羊草茎叶的盐分离子(Na^ 、Cl^-)含量与相对生长率(RGR)之间呈显著的负相关关系。     

黄土高原不同林龄土壤质地和矿质元素差异研究

对黄土高原不同林龄和不同树种条件下土壤的机械组成和矿质元素含量进行了分析研究,结果表明:①成林土壤砂粒、粉粒含量低于中幼林土壤,粘粒含量高于中幼林土壤,且呈显著性差异;②成林土壤Al2O3、Fe2O3、TiO2、MnO2、K2O含量相对于中幼林土壤有不同程度的增加,除MnO2外,差异均为极显著;成林土壤中Al2O3、Fe2O3、TiO2、MnO2在土壤中下层有不同程度的富集,SiO2、CaO含量降低;③矿质元素含量与土壤质地密切相关。