红壤溶磷菌的筛选及溶磷机制

采用以磷酸铝为磷源的蒙金娜(PVK)液体培养基研究了从红壤土中筛选出的4种溶磷菌的溶磷效果,选出其中的优势菌株B1,并对其溶磷机理做出初步探讨。结果表明,所筛选出的4株溶磷菌在液体培养条件下均有显著的溶磷效果,其中菌株B1在培养4 d后有效溶磷量最大,达到292.8 mg L-1。各处理培养液pH在培养期间均有显著下降,pH从7.0下降至3.2~4.7。高效液相色谱测定发现,各菌株培养液中有机酸的种类与含量随培养时间变化而不同,其中菌株B1主要分泌草酸和苹果酸,培养1 d后有机酸总量可达到5 mmol L-1;通过添加有机酸对磷酸铝活化的试验表明,分泌有机酸溶磷仅是菌株B1溶磷机制之一,可能还存在其他溶磷机制。菌株B1生长的适宜pH范围为5~9,最适培养温度为30℃,100 ml三角瓶的最适装液量为30~40 ml。经鉴定,菌株B1与苏云金芽孢杆菌有99.9%的相似性。     

控释肥用量对棉花生长特性和土壤肥力的影响

以国抗棉GK12号为供试材料,以等养分量复合肥作对照,研究不同控释肥施用量对大田棉花生长和土壤肥力的影响。结果表明,控释肥处理的棉花株高、茎粗、叶面积均较普通复合肥具有优势。控释肥对大田果枝数、桃数影响显著。在施氮量为75 kg hm-2和150 kg hm-2条件下,控释肥处理的棉花产量较复合肥处理分别增加18.9%和13.6%。在多个棉花生育期,与复合肥处理相比,控释肥处理提高了0~20 cm和20~40 cm土层硝态氮含量,未对土壤的铵态氮含量造成显著影响,土壤中有效磷和速效钾含量与普通复肥处理间未出现显著的差异。     

水稻穴播同步侧位深施肥技术试验研究

根据水稻种植的农艺要求,在同步开沟起垄水稻精量穴播技术的基础上进一步提出了一种水稻穴播同步侧位深施肥技术。调查了在不同种植方式条件下不同品种的水稻根系在稻田中的分布情况,根据根系的分布情况研究了深施肥技术参数,确定了深施肥深度以不超过10 cm为宜,研究了培杂泰丰、玉香油占2种品种水稻施入0~5 cm土层与5~10 cm土层中的肥料比例关系。试验结果表明华南农业大学研制的同步开沟起垄侧位深施肥水稻精量穴播机能满足水稻穴播同步侧位深施肥技术的要求,可以作为实施水稻穴播同步侧位深施肥技术的载体。生产试验表明:水稻穴播同步侧位深施肥技术具有增产、节本的效用。在同等的施肥条件下,机械播种及深施肥处理的有效穗、穗平均实粒数、结实率均高于机械播种人工撒施肥和人工撒直播人工撒施肥,增产418.5~957 kg/hm2,增幅5.86%~13.41%。该文研究可为深施肥机具的设计提供参考依据。     

长期施氮肥对黄棕壤微生物生物性状的影响及其调控因素

基于黄棕壤小麦-甘薯轮作的长期定位试验,探究不同施氮处理土壤微生物生物量碳(MBC)、氮(MBN)含量和酶活性的变化及其潜在调控因子,为科学施氮提高土壤质量和改善土壤生态功能提供依据。试验选取始于2011年4个施氮处理:不施肥(CK)、不施氮肥(PK)、施化学氮肥(NPK)和化学氮肥配施有机肥(NPKM),调查两季作物收获后土壤MBC和MBN含量、酶活性及微生物碳氮利用效率的变化,并通过冗余分析(RDA)和结构方程模型(SEM)明确调控弱酸性黄棕壤中MBC和MBN变化的潜在因素。小麦和甘薯两季的结果表明:施氮肥降低了土壤MBC、MBN含量和蔗糖酶(SSC)、脲酶(SUE)活性,与NPK处理相比, NPKM处理增加了MBC、MBN含量和SSC、SUE活性。长期施用氮肥提高了土壤有机碳(SOC)和土壤养分[全氮(TN)和矿质态氮(MN)]含量,但施氮肥显著降低土壤p H以及微生物的碳氮利用效率。与小麦季相比,甘薯季土壤SOC和MN含量有所下降,而MBN含量和SSC活性有所升高。RDA和SEM结果表明,氮肥的施用强化了MBC与MBN、SSC与MBC以及SUE与MBC之间的关联性;不同施氮处理下土壤p H、有机碳、氮含量以及微生物的碳氮利用效率的变化直接或间接地影响土壤MBC、MBN含量和SSC、SUE活性,其中p H是调控土壤MBC变化的直接因素,而土壤SSC和SUE活性与MBC、MBN含量相互影响。长期施用氮肥降低了黄棕壤MBC、MBN含量和酶活性,化学氮肥配施有机肥有利于缓解生物性状的下降,土壤p H是影响MBC变化的主要因素,小麦-甘薯轮作中土壤微生物强烈的碳代谢过程利于增加MBN。     

施用农家肥和化肥对盐碱地桑树生长和叶片光合日变化的影响

研究了施用化肥和农家肥对盐碱地桑树生长和叶片光合及叶绿素荧光日变化的影响,结果表明:盐碱地桑树的生长、光合和叶绿素荧光日变化明显受施肥的影响。施用化肥在一定程度上改善了盐碱地桑树的生长状况,但其作用效果没有农家肥明显。施用农家肥不但促进了桑树地上部生长,而且增加了桑树的根冠比,说明施用农家肥可促进盐碱地桑树根系生长。施用农家肥提高了盐碱地桑树叶片光合能力,表现在桑树的光合日积累量增加和光能原初转化效率提高,维持了盐碱地桑树叶片在中午时PSⅡ反应中心的活性,减缓了盐碱地桑树叶片中午的光抑制。施用农家肥桑树叶片在1天之中可以维持较高的气孔导度和蒸腾速率,以保证光合碳同化原料(CO2)的供应,且降低了桑树叶片中午时的叶面温度和叶片的卷曲程度,从而保持了叶片对光能的捕获和利用能力。     

基于地统计与遥感反演相结合的有机质预测制图研究

土壤水分对土壤光谱反射率有显著影响,而以往有机质遥感反演制图中却很少将水分作为预测建模的变量。为了使遥感制图更加符合野外实际环境,提高有机质预测制图精度,在充分考虑土壤样点空间自相关、异相关与野外复杂环境特点的基础上,通过地统计获得研究区水分的空间分布数据,结合遥感反射率,建立多因子预测模型,得到了吉林省黑土区土壤有机质空间分布图。结果表明,有机质遥感制图中,水分因素的加入,使模型的建立更加符合野外实际情况,显著提高了有机质预测制图的精度。     

Nutrients management strategies to improve yield and quality of sugar beet in semi-arid regions

The objective of this study was to evaluate the effects of organic and inorganic fertilizers on the yield and quality of sugar beet genotypes (Beta vulgaris L.). Therefore, a field trial was carried out in Peshawar, Pakistan, during the winters in 2012–2013. The field experiment was conducted in a randomized complete block design with split plots, having three replications. Fertilizer treatments (control, composted manure Higo Organic Plus at 5 t ha^?1, Maxicrop Sea Gold seaweed extract at 5 L ha^?1, farm yard manure at 10 t ha^?1, inorganic nitrogen–phosphorus (NP) at 90:60 kg ha^?1, NP at 120:90 kg ha^?1 and NP at 150:120 kg ha^?1) were allotted to main plots, while genotypes (Sandrina, Serenada and Kawe Terma) were allotted to the sub-plots. Plots treated with the application of NP at 120:90 kg ha^?1 produced the highest beet yield (76.4 t ha^?1) and sugar yield (11.1 t ha^?1), and had the second highest polarizable sugar content (14.52%) and more economic return (Rs. 553,000 per hectare) as compared to control plots. Sugar beet genotype Serenada had significantly higher beet yield (55.5 t ha^?1) and sugar yield (7.9 t ha^?1) and a higher economic return (Rs. 380,000 per hectare) than the other genotypes. Sugar beet genotype Serenada supplied with NP at 120:90 kg ha^?1is recommended for the general cultivation in the agro-climatic conditions of Peshawar valley.     

The effect of residual copper levels on the nutrition and yield of oats grown in microplots on three organic soils

Abstract

Oats (Avena sativa L. cv. Garry) were grown in microplots of three organic soils at site A (peat), site B (muck) and site C (mucky peat) in the summer of 1983. The soil surface (0 to 20 cm) varied in total Cu from 13 to 1659, 135 to 1745, and 81 to 1063 μg/g at sites A, B and C, respectively, due to applications of CuSO₄.5H₂O made at three rates in 1978, at sites A and B, and in 1979 at site C. Neither the rates of Cu application nor total soil Cu influenced yields. High levels of residual Cu increased the levels of Cu in straw at sites A and B, and in grain at site C. However, even the highest levels of Cu in straw and grains, were below the 20 μg/g which is often considered to be the threshold of Cu phytotoxicity. Data on the levels of other nutrients (P, K, Ca, Mg, Fe, Mn, Zn, B, Mo and S) in the tops and roots of oats generally revealed no significantly adverse effects of the Cu applications or total accumulated Cu in the three soils.     

保水剂与肥料互作及保水缓/控释肥料研究展望

保水剂在农业上的作用日益重要,肥料与保水剂一体化使用是水肥调控的重要技术,是肥料研究的国际前沿。保水剂是吸水量超过自身重量数百倍以上的亲水性高聚物。保水剂一般分为天然的,合成的及半合成的。保水剂与肥料可以通过物理混合、包膜或化学合成三种方式结合为一体化的保水缓/控释肥料。保水剂具有吸水吸肥功能,保水剂可吸附大量中性分子,对阳离子养分也有较强吸附作用,对阴离子养分吸附弱。肥料种类与盐浓度影响保水剂的吸附作用与膨胀能力。保水缓/控释肥料在土壤中对肥料养分有延迟释放作用。保水缓/控释肥料可改善土壤持蓄水分和水肥交互作用,促进植物对养分的吸收和作物增产。保水缓/控释肥料发展方向是包膜和化成保水缓/控释肥料。保水缓/控释肥料湿润及养分控释机理研究也需要加强。     

Influence of management practices on soil organic matter changes in the Northern China plain and Northeastern China

Soil organic matter (SOM) is strongly related to soil type and management practices. Changes in government policy have brought drastic changes in farm management practices in the last two decades in rural China. This study investigates changes in SOM in two different soils: Ustepts and Udolls. Ustepts, in the North China Plain where the climate is warm and sub-humid, developed from an alluvial flood plain with organic matter <10 g kg⁻¹. Udolls, in Northeastern China where the climate is cool and sub-humid, developed from loess-like materials with organic matter >20 g kg⁻¹. Two locations for Ustepts and three locations for Udolls were used to collect 567 soil samples in 1980–1982 and again in 2000 for SOM analysis. Soil organic matter increased for Ustepts and decreased for Udolls soils over the sampling period, resulting from differences in fertilizer rates and crop residue input to soil. Higher fertilizer input and crop intensity and initially very low SOM content in Ustepts all contributed to greater OM input than oxidation release. In contrast, lower fertilizer input and crop intensity, and initially high SOM content in the Udolls, led to lower OM input than oxidation release. Increasing SOM content through higher mineral fertilizer input is a valuable option for sustainable agriculture production in areas where SOM is low and there is a shortage or potential shortage of food supply.