不同小麦品种（系）中主要矿质元素的含量比较及与品质的关系

采用微波消解、电感耦合高频等离子体原子发射光谱（ICP-AES）的方法,对62份不同小麦品种（系）中锌、铁、铜、钙、钠和钾的含量进行了测定。同时利用红外线品质测定仪对主要品质指标粗蛋白、湿面筋、沉降值进行了测定。结果表明，不同小麦品种（系）中各种矿质元素的含量存在差异，2006年小麦品种中铁含量变幅为18.55-58.19 ug/g，平均为30.83ug/g ，最高与最低的相差39.64ug/g；锌含量变幅为5.70-25.80 ug/g，平均为15.13ug/g ，最高与最低相差20.10ug/g。2008年小麦品种（系）中铁含量变幅为16.68-52.25 ug/g，平均为30.10ug/g，最高与最低相差35.58ug/g；锌含量变幅为12.29-33.47 ug/g，平均为21.11ug/g，最高与最低相差21.18ug/g；钙含量变幅为167.53-348.80ug/g，平均为248.59ug/g，最高与最低相差192.59ug/g；铜含量变幅为2.32-5.83 ug/g，平均为2.98ug/g，最高与最低的相差3.61ug/g；钾含量变幅为1822.71-4414.91 ug/g，平均为2617.87ug/g，最高与最低的相差2634.72ug/g；钠含量变幅为10.25-39.82 ug/g，平均为23.05ug/g，最高与最低的相差29.57ug/g。 两年不同小麦品种（系）中矿质元素的含量分析结果表明：铁、铜、钙、钠和钾含量年际变化不明显,说明小麦对铁、铜、钙、钠和钾的吸收较稳定；锌含量变化较大，可能受环境的影响比较大。分析各矿质元素含量与粗蛋白、湿面筋、沉降值及元素之间的相关关系，结果表明，锌含量与粗蛋白含量呈极显著正相关关系，相关系数为0.317，与湿面筋含量之间呈显著正相关，相关系数达到0.246；铁含量与粗蛋白含量呈显著的正相关关系，相关系数是0.262；铜、钙、钠和钾含量与粗蛋白含量、湿面筋和沉降值之间存在正相关，但不显著，其中钠与沉降值之间为负相关。表明施锌或铁对提高小麦粗蛋白和湿面筋有显著效应，其余矿质元素有促进作用但不明显。 利用RAPD分子标记技术对川育23、41058、川育20及其父母本进行分析，力图从分子水平找到小麦矿质元素含量之间的差异性，琼脂糖电泳结果表明不同的小麦品种（系）间扩增出了差异条带。 以上研究结果，将对筛选“微量营养强化型”小麦新材料，选育“微量营养强化型”小麦新品种奠定基础。 62 different wheat cultivars was digested with HNO3 in a tightly closed vessel heated under micro-wave,then contents of zinc，iron,copper，calcium，sodium and potassium were determined by inductively coupled plasma-atomic emission spectroscopy(ICP-AES)．The main indexes of wheat quality such as total protein、wet glu and sedimentation volume were detected by Infratec 1255 Food & Feed Analyzer at the same time.The obtained results showed that variation for all of the mineral elements concentrations among different cultivars were observed .In 2006, the amplitude variation of the iron content was 18.55-58.19 ug/g,the average value was 30.83ug/g,and 39.64ug/g between the highest-content cultivar and the lowest one; the amplitude variation of the zinc content was 5.70-25.8 ug/g,the average value was 15.13ug/g,and 20.10ug/g between the highest-content cultivar and the lowest one.In 2008, the amplitude variation of the iron content was 16.68-52.25 ug/g,the average value was 30.10ug/g,and 35.58ug/g between the highest-content cultivar and the lowest one; the amplitude variation of the zinc content was 12.29-33.47 ug/g,the average value was 21.11ug/g,and 21.18ug/g between the highest-content cultivar and the lowest one; the amplitude variation of the calcium content was 167.53-348.80ug/g,the average value was 248.59ug/g,and 192.59ug/g between the highest-content cultivar and the lowest one; the amplitude variation of the copper content was 2.32-5.83 ug/g,the average value was 2.98ug/g,and 3.61ug/g between the highest-content cultivar and the lowest one; the amplitude variation of the potassium content was 1822.71-4414.91 ug/g,the average value was 2617.87ug/g,and 2634.72ug/g between the highest-content cultivar and the lowest one; the amplitude variation of the sodium content was 10.25-39.82 ug/g,the average value was 23.05ug/g,and 29.57ug/g between the highest-content cultivar and the lowest one. Analysis was made on the annual variation of mineral elements content in different Wheat cultivars ,the result shows:there is no obvious difference of iron ,copper ,sodium、calcium and potassium concentrations in wheat cultivars, suggesting the absorption of the iron, copper, sodium、calcium and potassium by wheat are relatively steady ,but zinc concentrations change obviously ,maybe influenced heavily by environment . The correlation between mineral elements 、mineral elements and total protein、mineral elements and sedimentation volume as well as mineral elements and wet glut were analysed in this paper, the result showed that there was significant positive correlation between zinc content and total protein (the correlation coefficient is 0.317), positive correlation between zinc content and wet glu (the correlation coefficient is 0.246), positive correlation between iron content and total protein (the correlation coefficient is 0.262). there was positive but not obvious correlation between the contents of copper, calcium, sodium or potassium and total protein, wet glut or sedimentation volume,among which was negative correlation between sodium and sedimentation volume.It was indicated zinc or iron fertilization has prominent effects in improving the total protein in wheat, the rest mineral elements have Non- obvious facilitation. The study then forecasted the genetic difference of different wheat by the molecular marker of RAPD in order to find differences in molecular level. Chuanyu23、41058、chuanyu20 as well as their male and female parents were analysed by RAPD markers,Agarose gel electrophoresis of DNA revealed the appearance of differential bands . The above-mentioned results of this study establish the foundation to screening the new materials of wheat of " strengthening type of micro- nutrition ", and to breeding the new wheat cultivars of" strengthening type of micro- nutrition ".

氮和磷在饲养-堆腐环中的循环率及有机肥料养分利用率

A five-year experiment indicated that the average loss rate of N and P in harvested products through a feeding-composting cycle was about 50% and 15%,respectively.Under high yield condition,the amount of recycled N and P from 80% harvested products and through a feeding-composting cycle in farming systems was about 3751 and 814 kghm~(-2),equivalent to 25%34% of N and 32%56% of P from chemical fertilizers applied each year to the systems.The apparent recoveries of N and P in organic manure increased with the prolongation of fertilization,indicating a synergetic residual effect existed,and was 61% and 39% in average in the five-year experiment.The use of nutrients recycled in the farming systems could not only improve soil fertility,but also increase the recoveries of nutrients and reduce the use of chemical fertilizers.

Iron and inorganic carbon in Liaodong Gulf sediments of Bohai Sea in China

Iron in seawater is an essential trace metal for phytoplankton that plays an important role in the marine carbon cycle. But most studies focused on oceanic iron fertilization in high nutrient low chlorophyll (HNLC) seawaters. A study of inorganic carbon (IC) forms and its influencing factors was presented in Liaodong Gulf sediments, and especially the influence of iron was discussed in detail. Inorganic carbon in Liaodong Gulf sediments was divided into five forms: NaCl, NH3·H2O, NaOH, NH2OH·HCl and HCl. The concentration of NaCl and NaOH forms were similar and they only occupied the minority of total inorganic carbon (TIC). However, NH3·H2O, NH2OH·HCl and HCl forms were the principal forms of TIC and accounted for more than 80% of TIC. Especially, the percentage of NH3·H2O form was much higher than that in the Changjiang River Estuary and Jiaozhou Bay sediments. All forms of inorganic carbon were influenced by organic carbon,pore water, iron, pH, redox potential(Eh) and sulfur potential(Es) in sediments, moreover, the influences had different characteristics for different IC forms. However, the redox reactions of iron affected mainly active IC forms. Iron had little effect on NH2OH·HCl and HCl forms of IC which were influenced mainly by pH. Iron had a stronger influence on NaCl, NaOH and NH3·H2O forms of IC; the influence of Fe2+ was higher than Fe3+ and its effect on NH3·H2O form was stronger than on NaCl and NaOH forms.

旱地长期培肥土壤脲酶和碱性磷酸酶动力学及热力学特征研究

研究了连续25年长期培肥试验条件下土壤脲酶和碱性磷酸酶酶促反应的动力学和热力学特征,从酶学角度揭示长期培肥的效应。结果表明,长期培肥增加了脲酶和碱性磷酸酶酶促反应的Vmax、Vmax/Km和k值;降低了Ea、△G、△H和△S值,说明培肥能提高酶促反应速度、减小活化自由能、加快土壤中物质的生物循环过程。酶促反应动力学参数和热力学参数与土壤性质相关分析表明,酶促反应动力学参数大多依赖于土壤化学性状,基于动力学参数的土壤肥力指标体系可评价土壤肥力水平,且U-Vmax、P-Km、P-Vmax可作为土壤肥力的重要指标。

黄土塬区氮磷配施对冬小麦光合作用、产量形成及水分利用的影响

在黄土高塬沟壑区,研究了不同施肥条件对冬小麦各个生育期的叶面积指数、光合作用、干物质积累、产量形成以及水分利用的影响,结果表明:与对照相比,施肥后小麦叶面积指数和光合速率都显著提高,同化作用增强,平均产量提高了47.6%,水分利用效率提高了24.6%。不同的肥料配施对冬小麦的干物质积累、产量以及水分利用效率的影响顺序基本一致,即高氮高磷>高氮低磷>低氮低磷>低氮高磷,但方差分析表明,在这种氮磷配施方案中起作用的主要是氮肥,磷肥的贡献不大,且二者并没有产生明显的交互作用。

施肥与品种及其种子大小对冬小麦光合及叶绿素荧光特性的影响

以土垫旱耕人为土为供试土样,采用4个冬小麦品种、3种播种方式和4种施肥方式进行盆栽试验,研究施肥、品种和种子大小对小麦叶片光合和叶绿素荧光特性的影响.结果表明:(1)在开花期和灌浆期,旗叶叶绿素相对含量(SPAD值)均为NP配施最高,其平均值分别比对照显著增加17.83%和13.01%;NP配施条件下,在开花期和灌浆期SPAD均为大粒单播较高并显著高于小粒单播;开花期和灌浆期SPAD分别以远丰998和咸农39最高并显著高于其它品种,平均比最低的白芒麦分别高17.68%和18.75%.(2)对旗叶净光合速率来说,开花期的NP配施处理比对照略有下降,而单施N和P分别比对照显著降低13.03%和23.17%,灌浆期的平均值以NP配施最高且比对照显著提高6.95%;小偃6号在开花期显著高于其余品种4.01%~6.19%(P<0.05),而白芒麦和咸农39则在灌浆期具有较明显优势,均分别显著高于其余品种约16.60%~26.91%;在开花期和灌浆期,2种单播方式平均值相近且显著高于混播方式.(3)就叶片Fv/Fm和Fv/Fo值而言,NP配施明显高于其它施肥处理,且NP均衡供应时远丰998和混播方式具有明显优势.可见,氮...

土壤类型和添加有机物料对铵态氮回收的影响

探讨NH4+-N回收率在不同因素下的变化规律。【方法】以黄土高原从北向南不同地区的典型土壤类型为对象,采用Bremner浸取法,研究了土壤类型、植被类型、施肥模式及添加有机物料对铵态氮回收率的影响。【结果】不同类型土壤及不同类型植被间NH4+-N回收率存在极显著差异(P<0.01)。黄土正常新成土的NH4+-N回收率最高(88.8%),极显著大于其他土壤,土垫旱耕人为土的NH4+-N回收率最低(81.0%),简育干润均腐土和干润砂质新成土介于二者之间;不同类型植被间,林地土壤的NH4+-N回收率(91.0%)极显著高于其他类型植被土壤,其他类型植被土壤的NH4+-N回收率表现为农田(85.5%)>裸地(83.8%)>草地(83.6%),但三者之间差异不显著。添加有机物料后,土壤NH4+-N回收率极显著增加(P<0.01),不添加有机物料对照土壤的NH4+-N回收率为84.3%,添加长毛草和苜蓿后的NH4+-N回收率分别为86.6%和85.9%。长期施肥对土壤NH4+-N的回收率无显著影响(P=0.436 5>0.05)。【结论】NH4+-N回收率与粘粒含量呈弱负相关,与有机质含量呈正相关,粘土矿物对N...

不同水肥条件对马铃薯肥料N利用率的影响

在旱棚控制条件下 ,用五因素五水平二次回归正交旋转组合设计 ,研究了水肥施用分配 ,补水量 ,施N量 ,施K量 ,有机肥施用量的综合作用效应 .结果表明 ,五因素对肥料N利用率的作用顺序为施N量 >补水量>水肥施用分配 >有机肥施用量 >施K量 .水肥施用分配相对于不同水、化肥 (N、K )、有机肥量的选择 ,可以大大地提高肥料N利用率 ;量少应重前施用 ,量多重后施或均施为好 .补水量与施N量的耦合规律为 :高水高肥效果最佳 ,肥料N利用率可达 5 7 83 % ,中水中N及低水低N次之 ,为 2 9 17%～ 40 99% ;高水低N或低水高N导致最低的利用率 ,为 2 2 87%或 2 2 5 1%

不同轮作施肥对土壤有机氮分解特征的影响

在各长期轮作施肥系统中,耕层土壤矿化培养过程的pH及剖面矿化势的变化,说明了长期不同的轮作和施肥方式引起土壤有机氮数量和性质的变化。pH变化具有一共同特征,在0~4 周,各处理间差异显著;而后期变化趋势趋于一致,向微碱性环境发展。各处理的剖面矿化势的变化反映了有机氮可矿化数量的改变。小麦连作施肥和苜蓿连作施肥均说明施用有机肥对土壤有机氮水平有较好的提高作用。粮豆轮作3 a对土壤供氮能力的提高作用大于粮饲轮作4 a和裸地处理。

旱地长期定位施肥对土壤剖面硝态氮分布与累积的影响

在 １５ ａ长期定位试验基础上研究了黄土高原旱地长期施用不同用量和配比的氮、磷肥对土壤剖面中硝态氮分布和累积的影响。结果表明：长期大量施用氮肥，在土壤剖面 １００～１８０ ｃｍ之间形成硝态氮累积层，峰值出现在 １４０ ｃｍ处，最大值为 ６７．９２ｍｇ／ｋｇ（单施 Ｎ １８０ ｋｇ／ｈｍ~２）； 配合施用磷肥可以降低土壤剖面硝态氮质量分数，根据试验，提出了旱地合理施肥的氮磷肥用量。

施氮对黄土高原水蚀风蚀交错区土壤矿质氮的影响

研究施氮对黄土高原水蚀风蚀交错区不同土层土壤矿质氮含量和累积量的影响。【方法】试验设作物和施肥2个因子,分析不同施氮水平和不同作物处理下黄土高原水蚀风蚀交错区0~100 cm土层土壤矿质氮的差异。【结果】不同施氮处理对土壤硝态氮含量及矿质氮累积量有明显影响,土壤硝态氮含量和0~100 cm土层土壤矿质氮累积量均随施氮量的增加而增加,但施氮量对土壤铵态氮的影响较小;不同施氮条件下,不同土层土壤硝态氮含量和矿质氮累积量均以0~20 cm土层最高,从总体上看,随着施氮量增加,较深土层(80~100 cm)土壤硝态氮含量和矿质氮累积量亦有所增加;不同作物间,除施90 kg/hm2磷+45 kg/hm2氮处理时,种植黑麦草作物的0~20cm土层土壤NO3--N含量有所增加外,其余施氮处理对种植两种不同作物土壤的NO3--N含量和NH4+-N含量均未产生明显影响,在相同施氮处理下,黑麦草地和苜蓿地0~100 cm土层土壤总矿质氮累积量的差异不明显。【结论】不同水平氮肥处理均对黄土高原水蚀风蚀交错区土壤矿质氮含量及累积量有一定影响,土壤矿质氮含量及累积量均与施氮量密切相关。

水肥空间组合对冬小麦光合特性及产量的影响

以肥熟土垫旱耕人为土为供试土壤,用分层土柱试验法研究了不同土层水分、氮、磷空间组合对冬小麦不同生育时期光合特性及籽粒产量的影响.结果表明:与0～90cm土层整体湿润相比,上干下湿(0～30cm土层干旱胁迫,30～90cm土层湿润)水分处理显著降低了小麦叶片叶绿素相对含量(SPAD)、净光合速率(Pn)和籽粒产量.2种水分条件下,氮磷配施处理对叶片SPAD、Pn和小麦籽粒产量的影响最为显著,其次是施磷处理,而施氮处理影响不显著.不同土层施氮在2种水分条件下各指标的变化趋势相同,均表现为0～90cm土层施氮小麦叶片SPAD、Pn及籽粒产量显著高于0～30、30～60和60～90cm土层施氮.不同土层施磷在2种水分条件下各指标的变化趋势也相同,表现为0～90cm土层施磷小麦叶片SPAD、Pn和籽粒产量与0～30cm土层施磷间差异不显著.不同土层氮磷配施在2种水分处理下表现不同:整体湿润条件下0～90cm土层施肥处理的小麦叶片SPAD、Pn及籽粒产量最高,与0～30cm土层差异不显著,但二者均显著高于30～60和60～90cm土层处理;上干下湿条件下各土层施肥处理间小麦叶片SPAD差异不显著,0～90cm土层施肥处理...

半湿润农田生态系统长期施肥对土壤团聚体中有机氮组分的影响

通过对黄土高原半湿润农田生态系统25年的田间肥料定位试验,研究了长期不同施肥模式对土壤有机氮组分及其在各级团聚体中分布的影响.结果表明:长期施肥对水解氨态氮、水解未知氮在土壤各级团聚体中分布的影响最大,对氨基酸态氮的分布有一定影响,而对氨基糖态氮分布的影响较小.长期施用化肥和有机肥能有效地影响水解氨态氮和水解未知氮与团聚体的结合作用,而氨基糖态氮在土壤氮循环转化过程中具有较强的稳定性.长期施肥条件下土壤水解全氮与有机碳、全氮以及团聚体分形维数均呈极显著正相关,其r分别为0.942,0.981,0.910(P<0.001),说明土壤有机氮组分对土壤团聚体的形成和性质具有显著影响.相关分析表明,土壤全氮或有机质对1～2mm和0.25～1mm土壤团聚体中各有机氮组分的影响较大

轮作和施肥对半干旱区作物地上部生物量与土壤有机碳的影响

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