解钾细菌C6X对不同富钾矿物含量土壤钾素迁移的影响

为了改善黄土高原地区煤炭开采引起土壤质量急剧退化的现状,该文以玉米为供试植物,通过日光温室短期盆栽的方式,系统研究解钾细菌C6X和玉米生长对土壤钾素迁移的影响.结果表明:1)玉米生长条件下,解钾细菌在富钾矿物质量分数45％上层土壤(0～20 cm)中对速效钾增量的促进作用最佳.2)解钾细菌和玉米生长协同提高上层土壤钾素固定能力,缓效钾增量在土壤富钾矿物质量分数68％为最大值.3)解钾细菌和玉米生长协同促进土壤钾素上移能力,在富钾矿物质量分数45％水平,土壤上移速效钾呈最大值;同时,解钾细菌促进土壤上移速效钾和玉米钾素积累量二者趋于线性稳定,利于土壤钾肥长期管理.因此,解钾细菌和玉米生长协同促进土壤钾素的释放和固定,并促进土壤钾素上移.     

硅酸盐细菌在不同生境土壤中的分布

以水洗钾长石粉为惟一K源的硅酸盐细菌选择性培养基,对我国部分省市土壤中的硅酸盐细菌的分布状态进行了初步调查。采集了0 ~ 10cm土层下土壤样品48个,测定了土壤pH和养分,从中分离出硅酸盐细菌148株,并对其进行了初步鉴定。研究了硅酸盐细菌在不同生态环境中的分布规律及对含K矿物(钾长石、霞石和伊利石)的分解能力,从中筛选出4株高效菌株,对研究硅酸盐细菌在我国不同土壤生态系中资源的保护、开发和利用,具有重要意义。     

硅酸盐细菌NBT菌株解钾效能及对钾的吸持作用

在摇瓶和土壤耗竭条件下研究了硅酸盐细菌NBT菌株的解钾作用以及对作物生长的促进作用。结果表明 ,在摇瓶条件下 ,培养 120h ,NBT菌株可以从钾长石中释放K 159.1mg/L ,比接灭活菌对照 (48.8mg/L)增加 226.02% ;耗竭条件下NBT菌株在未灭菌土壤中的解钾作用与在灭菌土壤中的解钾作用相当。在未灭菌土壤中 ,NBT菌株释放的矿物钾占植株吸钾量的 14.4 %～ 4 3.1% ;不接菌或接灭活菌处理土壤中矿物钾的释放量为零或极少。NBT菌株的解钾效能与土壤中速效性钾及有机质含量密切相关。土柱试验表明 ,供试土壤接种硅酸盐细菌后的土壤滤液中流失的钾比接种灭活硅酸盐细菌后的土壤滤液中流失钾减少 29.6 %～56.5% ;硅酸盐细菌NBT菌株荚膜多糖吸附钾的量占加入钾的量的 31.8%～ 69.4 %。NBT菌株的吸钾作用与NBT菌株本身及荚膜多糖的多少密切相关。     

硅酸盐细菌解钾活性的研究

研究了硅酸盐细菌在实验室及盆栽条件下的解钾活性,并在扫描电镜下观察了硅酸盐细菌对钾长石结构的改变。结果表明:硅酸盐细菌对含钾矿物确有溶解作用,能使固定钾转化为可溶性钾,对植物的生长及产量提高有明显促进作用。     

微晶化对钾长石粉钾素释放的影响

摘要: 利用微晶化设备对钾长石进行机械力活化处理,研究了不同处理时间对钾长石粉颗粒组成、 钾素释放量及生物有效性的影响。结果表明,钾长石经微晶化设备分别加工10 min、 40 min、 120 min和180 min后,微细颗粒（d10 m）组成比例分别达到51.69%、 65.44%、 85.34%和93.93%,比表面积明显增大,衍射峰强度显著减弱,同时钾素的释放量显著提高,其中微晶化处理180 min样品T3效果最好,2 mol/L HNO3和蒸馏水3次提取的钾总量分别为6118.8 mg/kg和2867.8 mg/kg; 4个处理（10 min、 40 min、 120 min和180 min）酸提钾总量分别是蒸馏水提钾总量的2.46、 1.81、 2.19和2.13倍,两种浸提剂提钾总量占钾长石全钾的0.50%~5.73%。微晶化以后钾长石粉中的绝大部分钾素仍以矿物态存在,但其生物有效性显著提高,促进了籽粒苋的生长和钾素积累。     

硅酸盐细菌NBT菌株生理特性的研究

对硅酸盐细菌NBT菌株在以钾长石粉为唯一钾源的培养基中产生的有机酸、氨基酸的种类和含量以及NBT菌株在有氮培养基中产生的植物激素的种类和含量进行了研究。结果表明 ,NBT菌株能合成草酸、酒石酸、柠檬酸和苹果酸等四种有机酸 ,其含量范围分别为 5 1 6～ 2 1 7 30mgL- 1 ,3 44～ 2 91 94mgL- 1 ,4 0 8～ 1 1 3 31mgL- 1 和 3 1 5～ 1 0 8 89mgL- 1 ;同时 ,NBT菌株能合成多种氨基酸。NBT菌株在有氮培养基中能产生并分泌生长素、赤霉素A3(GA3)、玉米素核苷和异戊烯基腺嘌呤四种激素 ;其浓度分别为 0 5 4～ 3 77nmolml- 1 、0 1 9～ 2 97nmolml- 1 、0 91～ 2 62nmolml- 1 和 5 49～ 31 1 5nmolml- 1 。摇瓶试验表明 ,NBT菌株不仅能分解土壤矿物并释放出其中的钾 ,而且具有很强的吸钾功能。NBT菌株细胞吸持的钾占其解钾量的 88 86%～ 95 0 5 %。     

解钾细菌与黏土矿物协同促进玉米生长提高土壤养分有效性

为了揭示解钾细菌在西北矿区浅埋古河道土壤中对植物生长和土壤养分利用的影响,通过日光温室短期盆栽的方式,以不同黏土矿物配比的人工培土为基质模拟古河道不同质地土壤,以西北地区常见农作物玉米为宿主,研究解钾细菌在人工培土基质中的微生物数量变化规律,以及二者协同作用对玉米生长和矿质养分吸收的影响。结果表明:1)土壤黏土矿物含量增大有利于提高土壤解钾细菌数量,促进微生物活性。当黏土矿物质量分数为68%,速效钾质量分数约170 mg/kg时,解钾细菌数量最大;2)玉米地上部分干质量、根冠比、根系活力随黏土矿物含量增大而增大,以解钾细菌作用下黏土矿物质量分数68%的玉米生长效果最佳;3)在解钾细菌作用下,植物氮磷钾积累量和土壤养分利用的最佳土壤黏土矿物质量分数为45%、68%和75%,土壤钾素、氮素和磷素最大利用率分别达到65%、53%和17%;4)解钾细菌在土壤钾素含量低时促进土壤磷素吸收,土壤钾素过量时,促进土壤氮磷钾的吸收,提高土壤养分利用率。因此,土壤黏土矿物与解钾细菌相互作用,而且积极影响植物生长和土壤养分的吸收利用,这对进一步探寻适合矿区浅埋古河道土壤的微生物复垦技术,深入改良和开发矿区退化土壤具有重要意义。     

烟草根际土壤中解钾细菌的分离与多样性分析

土壤中含有丰富的钾元素,但主要以缓效态形式存在于钾长石或云母等硅酸盐矿物中,不能被作物直接吸收利用。解钾微生物能溶解硅酸盐矿物中的钾,提高土壤中作物可利用钾的含量,有望缓解我国钾肥短缺的现状。本研究利用选择性培养基,从烟草根际筛选钾细菌,基于16S rDNA序列分析烟草根际土壤解钾细菌的多样性,通过测定解钾细菌的解钾效能及对烟草的促生作用,筛选有应用潜力的优良解钾细菌菌株。结果表明,从四川、湖北和山东烟区烟草根际土壤分离获得的27株解钾细菌,在解钾固体培养上溶钾圈直径为0.11~0.30 cm。16S rDNA序列分析表明,烟草根际土壤解钾细菌主要包括变形菌门γ亚群(Gammaproteobacteria,85.18%)、变形菌门α亚群(Alphaproteobacteria,3.70%)、变形菌门β亚群(Betaproteobacteria,3.70%)、放线菌门(Actinobacteria,3.70%)和拟杆菌门(Bacteroidetes,3.70%),其中克雷伯菌属(Klebsiella)为优势菌属(66.67%)。27个菌株均有一定的解钾能力,解钾活性为0.59~4.40 mg.L–1。参试菌株均对烟草有一定的促生作用,利用解钾细菌菌液处理烟株20 d后,与对照相比,株高增加0.97%~38.64%,最大叶长增加4.40%~31.02%。本研究筛选出的菌株XF11、GM2、JM19和GL7具有较高的解钾活性和促进植物生长的能力,展现了良好的应用潜力。     

具有拮抗作用的硅酸盐细菌的分离与筛选

从沈阳农业大学试验基地中分离出两株具有解钾能力的细菌C1和Y3,解钾量分别比对照提高44.8%和26.2%,对其生理生化特性分析,确定为芽孢杆菌属,其中C1对4株植物致病真菌有较强的抑制作用。在玉米盆栽试验中,C1和Y3对苗期玉米都有一定的促长作用,体现在植株高度和地上部干重,较对照分别提高了14.5%、31.9%和11.4%、26.7%,均达到显著水平。     

不同土壤中硅酸盐细菌生理生化特征及其解钾活性的研究

在以钾长石粉为唯一 K 源的硅酸盐细菌选择性培养基上,从我国部分省市土壤中筛选到 16 株硅酸盐细菌,以本实验室保藏 NBT 菌株为参照,对其生理生化特性、耐盐性、抗生素抗性、温度敏感性及释K 能力等生物学特性进行了测定。结果表明,17 株硅酸盐细菌菌体均为杆状,产生椭圆至圆形芽胞。其中 SB6、SB13 为短杆状,SB4、SB6、SB10、SB15 菌株是 G ,其余菌株是 G-。NH4 、NO3 为良好 N 源,且能在无 N -培养基上生长。菌株 SB13 和 NBT 解 K 能力较强,释放的 K 比接灭活菌对照分别增加 49.1 %和 45.3 %。菌株SB2、SB4、SB5、SB6 在 20 g/L NaCl 浓度的培养基上能生长,在温度为 10 ~ 40 范围内供试硅酸盐细菌能够良好生长。     

Fertilizing Properties of Potassium Feldspar Altered Hydrothermally

The material obtained through hydrothermal alteration of K-feldspar rock in alkaline conditions is a potential source of soluble potassium (K), but agronomic testing is needed to verify its capacity to supply K to crops. A (NH₄)₂SO₄-based bioassay was used to test the capacity of the material to supply K to tomato plants (Lycopersicon esculentum Mill.) growing in a mixture of silt loam, peat moss, and sand. Potassium chloride (KCl) and unaltered K-feldspar rock powder also were tested for comparison. The fresh weight and K composition of the plants increased as doses of KCl or hydrothermal material increased, but not with increases in K-feldspar rock. Development of stem lesions, which develop as symptoms of K deficiency in the presence of (NH₄)₂SO₄, were eliminated by KCl or hydrothermal material but not by feldspar rock. A beneficial effect may occur due to the calcium (Ca) supplied or with adjustment of soil acidity by the hydrothermal material. The hydrothermal material is a K fertilizer at least as effective as KCl since it yields the same or better plant weight.     

Isolation and identification of potassium-solubilizing bacteria from tobacco rhizospheric soil and their effect on tobacco plants

Soil potassium supplementation relies heavily on the use of chemical fertilizer, which has a considerable negative impact on the environment. Potassium-solubilizing bacteria (KSB) could serve as inoculants. They convert insoluble potassium in the soil into a form that plants can access. This is a promising strategy for the improvement of plant absorption of potassium and so reducing the use of chemical fertilizer. The objectives of this study were to isolate and characterize tobacco KSB and to evaluate the effects of inoculation with selected KSB strains on tobacco seedlings. Twenty-seven KSB strains were isolated and identified through the comparison of the 16S ribosomal DNA. Among them, 17 strains belonged to Klebsiella variicola, 2 strains belonged to Enterobacter cloacae, 2 strains belonged to Enterobacter asburiae, and the remaining 6 strains belonged to Enterobacter aerogenes, Pantoea agglomerans, Agrobacterium tumefaciens, Microbacterium foliorum, Myroides odoratimimus, and Burkholderia cepacia, respectively. All isolated KSB strains were capable of solubilizing K-feldspar powder in solid and liquid media. K. variicola occurred at the highest frequency with 18 strains. Four isolates, GL7, JM3, XF4, and XF11, were selected for a greenhouse pot experiment because of their pronounced K-solubilizing capabilities. After being treated with the four KSB strains, plant dry weight and uptake of both K and nitrogen (N) by tobacco seedlings increased significantly. These increases were higher with the combination of KSB inoculation and K-feldspar powder addition. Isolate XF11 showed the most pronounced beneficial effect on plant growth and nutrient uptake by tobacco seedlings. Combining the inoculation of KSB and the addition of K-feldspar powder could be a promising alternative to commercial K fertilizer and may help maintain the availability of soil nutrients. Further studies are necessary to determine the effects of these bacterial strains on mobilization of potassium-bearing minerals under field conditions.     

Granitic weathering: a Brazilian study

Chemical and mineral studies were carried out on weathered materials from six profiles developed on granites located in different areas of Brazil. Quartz and K-feldspar are the most abundant minerals overall. Kaolinite is the most common secondary mineral and is principally a feldspar weathering product. Mica breakdown is associated with smectite formation in semi-arid regions. In more humid regions mica weathering products include interlayered mica-vermiculite, vermiculite and kaolinite. Changes in the concentrations of Si, Al and K reflect the weathering behaviour of quartz, kaolinite, K-feldspar respectively, although K mobilities sometimes appear to be governed by processes related to the formation of secondary minerals. Ca and Mg are the first elements to exhibit depletion and their removal rates are very fast relative to K. P is also among the most mobile elements. Cr, Co, Ni, Cu, Zn, Rb, Sr, Y, Zr, Nb, Ba and Pb concentrations were measured. The first row transition metals are the most depleted. Rb and Sr are retained relative to Na, Mg, and Ca, and Ba accumulates as weathering proceeds. Y, Zr, Nb and Pb concentrations show little variation. The conclusion is that the factors controlling deep leaching are complex and the common notion that weathering rates are higher at lower latitudes should be reassessed.     

High‐Energy Milling Improves the Effectiveness of Silicate Rock Fertilizers: A Glasshouse Assessment

Abstract

The effectiveness of intensively milled gneiss and potassium (K-feldspar) as K fertilizers was evaluated through a glasshouse experiment with ryegrass. Plant were grown on two soil types for 12 months. Results show that the agronomic effectiveness of milled gneiss was nearly as great as potassium sulfate (K₂SO₄), but milled K‐feldspar was much less effective because of the relatively small extent of dissolution of K‐feldspar in the soil. The positive effects of K‐silicate rock fertilizers (K‐SRFs) included increases in plant biomass, uptake of K and silicon (Si), and soil pH with increasing application rate of the K‐SRFs. The application of K‐SRFs will be most advantageous for amending K‐deficient soils, and high‐energy milling provides a simple method for manufacturing effective multinutrient SRFs.     

Ca Depletion in the Soil Column on a Granite Substrate on the Island of Yakushima, a World Natural Heritage Site

We investigated the vertical profile of element distributions in the soil column on a granite substrate at three sites on the island of Yakushima, a world natural heritage site in southwestern Japan, where stream acidification due to acid rain is of increasing concern. Statistical analysis shows that the elements in the granitic soil can be classified into three groups according to their mineralogical derivations: Group 1 (K, Mg, Mn, Rb, and Nb), group 2 (Fe, Ti, Zr, Cr, and Pb), and group 3 (Ca, Na, Sr, and P), which are related to the presence of K-feldspar and K-mica, Fe-Ti oxides, and plagioclase and apatite, respectively. The pattern of distribution of group-1 elements in the soil column differs slightly among the sites because of differences in the proportions of K-feldspar and K-mica, The organic surface soil is enriched in group-2 elements and shows a strong magnetic susceptibility, indicating the presence of biogenetic magnetite. At all sites, Ca and Sr are intensely depleted due to the selective dissolution of plagioclase. Ca depletion compared to the original granite reaches more than 90 % in the C horizon, resulting in a decreasing capacity for the neutralization of acid rain and an increasing contribution of atmospheric Ca to the surface soil and vegetation.     

Chemical and mineralogical weathering rates and processes in an upland granitic till catchment in Scotland

Weathering in an upland granitic till catchment receiving an intermediate level of acidic deposition has been studied by chemical and mineralogical analyses of soil profiles and chemical analysis of precipitation and streamwater. Long-term weathering rates for base cations calculated from analyses of soil profile horizons using Zr as an internal, immobile, index element are similar for alpine podzols and peaty podzols and are 2–3 meq.m^–2.a^–1 for Ca and Mg, and 10–11 meq.m^–2.a^–1 for K and Na. The high loss of Na is associated with the weathering of oligoclase, particularly in the coarse sand fraction. Loss of K is related to weathering of K-feldspar and micas. Current weathering rates for base cations calculated from input-output budgets are higher than long-term rates by factors of 12, 8 and 3 for Ca, Mg and Na, but lower by a factor of 7 for K probably due to biomass uptake. The higher current overall loss of base cations may be due to increased rates of weathering in recent times but this is not conclusive as there are large uncertainties inherent in both methods of estimation.     

Potassium supply capacity response to K-bearing mineral changes in Chinese purple paddy soil chronosequences

Purpose

Purple paddy soils are important for food production. Their potassium (K) supply capacity affects rice yields through its effect on nutrient availability. We hypothesize that changes in soil mineralogy can influence the K supply capacity and the efficiency of K fertilizer. Designing management practices that optimize crop yield while minimizing environmental impacts is a major challenge in agriculture. For this, it is necessary to understand the evolution of, and interaction of, minerals and different chemical forms of K in the soil system.

Materials and methods

Taking advantage of the long-term paddy cultivation history in China, two purple paddy soil chronosequences, one in Guang’an, Sichuan Province (P sequence) and the other in Longsheng, Guangxi Autonomous Region (PS sequence) in Southwest China, were investigated.

Results and discussion

Depotassification is prevalent in both paddy soil chronosequences, which is consistent with the decrease of illite and K-feldspar in the P sequence and with the decrease of muscovite in the PS sequence. K-bearing primary minerals are the long-term stable source of non-exchangeable K (interlayer K) in both chronosequences. Illite in clay fractions acts as the main sources of non-exchangeable K in the P sequence. In contrast, clay minerals derived from muscovite are the main sources of non-exchangeable K in the PS sequence. Clay mineral authigenesis is an important process in the purple paddy soils rich in K-bearing minerals.

Conclusions

The changes in mineralogy of purple paddy soils do not conform to the usual sequence found in the well-drained natural soils. Artificial submergence promotes the conversion of mineral K (lattice-bound K) to non-exchangeable K and enhances the availability of mineral K. The disintegration of K-bearing primary minerals thus controls the K supply capacity in purple paddy soils.

     

The effects of straw return on potassium fertilization rate and time in the rice–wheat rotation

In order to investigate the effects of straw return on potassium (K) fertilizer application rate and time in the rice–wheat rotation, field experiments were conducted at three sites. The results showed that when the K rate was decreased to 70% of the recommended K dosage, crop yields showed no significant decrease. With K fertilization only at rice phase, crop yields showed no marked difference compared with that provided K fertilizer both at wheat and rice seasons. Though the NH₄OAc-extracted K and HNO₃-extracted K differed slightly among the treatments, the soil apparent K balance was negative without K fertilization. With crop straw fully incorporated, the recommended K dosage could be at least reduced by 30% at the experimental sites and the K fertilizer could be applied only at rice phase. A further hypothesis can be made that the best K rate was the amount of K took away by crop grain. In the long run, straw return combined with K fertilization would be an effective method to maintain soil K fertility and productivity.     

氮钾营养对烟叶衰老过程中内源激素与叶绿素含量的影响

采用盆栽试验和田间试验研究了氮钾营养对烟叶衰老过程中内源激素与叶绿素含量的影响。结果表明,随着烤烟中位叶片的成熟,氮、钾养分,叶绿素和细胞分裂素(CTK)含量均呈下降趋势,而脱落酸(ABA)含量则呈直线上升趋势。增施氮、钾肥料可以有效改善叶片氮、钾营养水平,增加叶绿素含量,提高叶片CTK含量,降低ABA含量,从而延缓叶片衰老。分析表明,烤烟叶片氮、钾含量与其叶绿素、CTK及CTK/ABA值呈极显著正相关关系,与ABA呈极显著负相关关系。因此,烤烟叶片内源激素的含量及其平衡关系与氮、钾营养关系密切,改变氮、钾肥料用量可以调控烤烟叶片的衰老速度。研究还表明,不论单独增施钾肥还是按比例同时增施氮、磷、钾肥,均可提高烟叶含钾量,尤其在烟叶发育前期效果更为突出,即使在钾素供应充足的情况下,成熟叶片中钾的转移能力依然很强。