几种土壤在单一Zn及Cd Cu共存条件下对Zn的吸附

研究了Zn2+在单一及与Cd2+、Cu2+共存条件下在塿土、黄绵土、黑垆土、黄褐土、砂土5种土壤中的吸附特征,并探讨了其吸附机制。结果表明,在20℃、30℃下,Zn2+在各供试土样中吸附等温线总体上均呈I或III型等温线形式,总体上黑垆土、塿土对Zn2+吸附最强,而砂土的吸附总是最差;塿土、黄绵土和黄褐土中Zn2+吸附的温度效应呈现升温正效应特征,砂土中则总体上表现出随温度上升呈下降趋势,黑垆土中Zn2+吸附的温度效应则与重金属处理有关。Freundlich模型是描述Zn2+吸附等温线最佳模型。Cd2+、Cu2+的共存对Zn2+的吸附均具有显著的拮抗作用,但对Zn2+吸附规律的影响不同。机理分析表明,Zn2+在土壤中的吸附主要以化学吸附为主,Cu2+由于其与Zn2+相似的化学吸附特点而竞争Zn2+化学吸附点位,但Cd2+吸附主要竞争以电性引力形式吸附的Zn2+,因而Cu2+对Zn2+吸附的影响较大,而Cd2+影响较小。     

Evaluation of ground-level and space-borne sensor as tools in monitoring nitrogen nutrition status in immature and mature oil palm

Monitoring nitrogen (N) in oil palm is crucial for the production sustainability. The objective of this study is to examine the capability of visible (Vis), near infrared (NIR) and a combination of Vis and NIR (Vis + NIR) spectral indices acquired from different sensors for predicting foliar N content of different palm age groups. The N treatments varied from 0 to 2 kg per palm, subjected according to immature, young mature and prime mature classes. The Vis + NIR indices from the ground level-sensor that is green + red + NIR (G + R + NIR) was the best index for predicting N for immature palms (R² = 0.91), while Vis indices blue + red (B + R) and Green Red Index from the space-borne sensor were significantly useful for N assessment of young and prime mature palms (R² = 0.70 and 0.50), respectively. The application of vegetation indices for monitoring N status of oil palm is beneficial to examine extensive plantation areas.     

日光温室栽培土壤供钾状况及K-Ca吸附交换特性研究

研究了陕西关中地区不同日光温室栽培土壤钾素供应状况及土壤K+、Ca2+离子吸附交换特性。结果表明,日光温室栽培的土壤钾素Q/I曲线及参数与大田栽培土壤明显不同。温室栽培（土娄）土和潮土钾素活度比（AR0）较相应大田土壤分别提高了14.8和6.9倍,土壤对外源钾的缓冲能力下降;从K+和Ca2++Mg2+的交换自由能看,温室栽培土壤存在钾素过多,K+和Ca2++Mg2+离子比例失调问题。不同K+/Ca2+摩尔比下,随着K+、Ca2+总浓度的提高,大田及温室栽培土壤对K+、Ca2+的吸附量均呈线性增加趋势,温室栽培土壤K+吸附率及两种土壤Ca2+吸附率均呈对数增加趋势。K+/Ca2+为2:1时,K+吸附量远大于K+/Ca2+为1:2.5时的吸附量;K+/Ca2+为2:1时,温室栽培土壤Ca2+均呈解吸状态。土壤对K+、Ca2+离子吸附的相对选择性随K+/Ca2+比例及溶液离子总浓度的变化而变化。K+/Ca2+为2:1时,土壤对K+的相对吸附选择性大,K+/Ca2+为1:2.5时,温室栽培土壤对Ca2+的相对吸附选择性显著增加。加入土壤K+的比例和数量过高,非但未提高K+离子的活度,还造成胶体上Ca2+离子的大量解吸,由此可能带来的日光温室土壤胶体稳定性降低及养分不平衡的问题值得关注。     

白浆土施有机肥及石灰对土壤酶活性与大豆产量的影响

白浆土是我国东北地区主要低产土壤之一,土体中白浆层通气透水能力极差,生物酶活性很低,导致土壤表旱表涝严重,旱田作物根系有效土层一般只有20 cm左右。为研究白浆土增施有机肥及石灰对大豆土壤酶活性及大豆产量的影响,设置了4个处理。结果表明3种酶活性均为:常规施肥+有机肥常规施肥+石灰+有机肥常规施肥常规施肥+石灰,说明有机肥的施用增加了土壤酶活性,石灰的施用降低了土壤酶活性;有机肥施用增加了土壤有机质,石灰施用增加土壤pH值,与对照相比,常规施肥+石灰处理大豆增产23.76%;常规施肥+有机肥处理增产28.32%;常规施肥+石灰+有机肥处理增产13.07%。说明有机肥及石灰无论是单独施用或是组合施用均对大豆增产有效。     

Detection and semiquantitative estimation of thyroxine and diiodothyronine in liothyronine sodium.

A method is presented for the detection and semiquantitative estimation of thyroxine and diiodothyronine in liothyronine sodium. Thyroxine is detected by thin layer chromatography, using silica gel H plates developed in butanol-acetone-ammonia (30 + 55 + 15) and sprayed with a 2,7-dichlorofluorescein solution, and estimated by comparison with standard spots. For quantitative results, a larger amount of sample is applied as a streak on a fluorescent silica gel H plate. After a 5 hr development, the band is scraped off and extracted in a small volume of 0.1N NaOH; the extract is centrifuged, transferred to a 2 cm microcell, and examined spectrophotometrically. The diiodothyronine content of liothyronine sodium is estimated by liquid chromatography on a Bondapak C18 column with 0.01N sodium perchloratebutanol-acetonitrile (1000 +62 + 188) as the eluting solvent.     

土层性质对铜和铅在土壤中保持和迁移的影响

The mobility and bioavailability of heavy metals in soils is largely governed by sorption and desorption phenomena.Cu2+ and Pb2+ are among the most potentially toxic heavy metals and they are present,often concomitantly,in many polluting spills and in agrochemicals.The objective was to assess and compare the competitive sorption and desorption capacities and sorption hysteresis of Cu2+ and Pb2+,as well as their migration through the profiles of four natural soils:a Humic Umbrisol,an Umbric Cambisol,an Endoleptic Luvisol and a Humic Cambisol.In all horizons Pb2+ was invariably sorbed and retained to a greater extent than Cu2+.The sorption and retention of Cu2+ were most in?uenced by pH,e?ective cation exchange capacity(CECe) and Mn oxide content.On the other hand,the fixation capacity of Pb2+ was most in?uenced by pH,CECe,and Mn oxide and organic matter contents.pH and CECe were the individual soil properties most markedly in?uencing Cu2+ and Pb2+ sorption and retention.In all the horizons Pb2+ exhibited greater hysteresis than Cu2+.In each soil the hysteresis in the A horizon was greater than that in the B horizon,except in the Bt horizon of the Endoleptic Luvisol,due to its high pH and vermiculite content.Based on migration indices,Pb2+ was less mobile than Cu2+ in the studied soils.     

Interactive Effect of Sulfur and Nitrogen on Nitrogen Accumulation and Harvest in Oilseed Crops Differing in Nitrogen Assimilation Potential

ABSTRACT

Field experiments were conducted to determine the interactive effect of sulfur (S) and nitrogen (N) on nitrogen accumulation, its distribution in various plant parts, and nitrogen harvest of oilseed crops viz. rapeseed (Brassica campestris L. cv. ‘Pusa Gold’) and taramira (Eruca sativa Mill.) differing in their N-assimilation potential. Two combinations of S and N (in Kg/ha): 0S + 100N (?S+N) and 40S + 100N (+S+N) were used. The results showed that combined application of S and N (+S+N) significantly (P < 0.05) increased the nitrogen accumulation in both the genotypes at all the growth stages compared with N applied alone (?S+N). This increase in nitrogen accumulation was due to the improvement in the reduction of nitrate into reduced nitrogen as evident from higher nitrate reductase (NR) activity in the leaves of plants grown with both S and N, compared with N alone. Nitrate-N content in the leaves of plants grown with only N (?S+N) was higher compared to those grown with both S and N (+S+N), showing that combined application of S along with N (+S+N) appreciably reduced the nitrate content in the leaves due to higher NR activity. This decline in nitrate (NO₃ ^?) was followed by an overall increase in N-accumulation in the plants. Consequently, the nitrogen content in the plant was increased by 29–148% in rapeseed and 38-166% in taramira with +S+N treatment. Combined application of S along with N (+S+N) also increased seed protein content and nitrogen harvest index of both the genotypes. It is concluded that combined application of S along with N (+S+N) not only increased the N-accumulation, but also its mobilization towards economic sinks.     

锌离子活度对水稻产量及子粒锌含量的影响及基因型差异

试验采用HEDTA螯合缓冲营养液培养法,选用子粒含锌量有明显差异的两个水稻基因型(碧玉早糯和浙农921),采用4种锌离子活度(pZn2+9.7,10.3,11.0,11.4),研究了锌离子活度对水稻产量和子粒锌积累、分配与子粒品质的影响及基因型差异。结果表明,锌离子活度通过对水稻有效穗数、每穗颖花数、结实率和千粒重的影响而显著影响水稻单株产量,其中影响最大的是单株有效穗数,其次是每穗颖花数,而对结实率的影响相对较小,但均存在明显的基因型差异。锌离子活度显著影响水稻子粒锌含量,随锌离子活度下降,水稻子粒含锌量降低,当锌离子活度低于pZn2+10.3时,两基因型水稻的含锌量均显著降低,但基因型间存在明显差异。不论在何种锌离子活度下,碧玉早糯的子粒含锌量均显著高于浙农921。从子粒锌分配看,颖壳、糙米、精米锌含量均随着锌离子活度提高而提高,当pZn2+从10.3升高到9.7时,碧玉早糯的糙米和精米锌含量开始降低,颖壳锌含量则开始超过糙米的锌含量继续升高;而浙农921糙米和精米锌含量的升高幅度较颖壳锌含量小。不同锌离子活度下,糙米和精米锌含量的比值在0.790~.90之间变化,并以pZn2+为9.7时为最小。因此,通过筛选子粒富锌水稻品种来提高稻米锌含量经济可行;通过增加环境锌离子活度,改善水稻的锌营养能显著提高水稻子粒的锌含量。     

陇东旱地苹果园不同地面覆盖模式的水分与养分效应

为完善和改进果园树盘起垄覆膜集雨保墒模式,提高土壤墒情,探寻更加有效的果园保墒措施,该研究以17 a生苹果园为研究对象,设置常规树盘起垄覆膜行间清耕模式（F）,在F 基础进行改进的树盘起垄覆膜+行间覆草模式（F+W）和树盘起垄覆膜+行间覆草+膜侧添加渗水穴模式（F+W+H）2种改进模式,以不起垄不覆盖为对照（CK）,采用定点试验,连续3 a(2015年干旱、2016年秋旱和2017年常年降雨)开展苹果花前、果实膨大期及采后的水分效应,以及养分效应和树体生长发育响应研究。结果显示：3种覆盖模式可不同程度增加0～200 cm土层的含水率, 以2017年最显著,2种改进模式可缓解300～500 cm土层水分消耗,降低休眠期无效蒸散,3 a三种覆盖模式0～500 cm土层总蒸散量均极显著（P<0.01）低于CK,由低到高顺序为F+W+H、F+W、F、CK。2015年和2016年采后覆盖模式0～300 cm土层硝态氮累积量均极显著（P<0.01）低于CK（比CK低34.4%～39.6%）。3种覆盖模式增加果实中氮磷钾养分吸收,以钾最突出。F+W+H、F+W和F 3 a平均产量分别较CK提高13.1%、13.0%和8.3%。综合各种效应,以2种改进覆盖保墒模式F+W+H和F+W较优。     

Nagina 22 mutants tolerant or sensitive to low P in field show contrasting response to double P in hydroponics and pots

ABSTRACT

A simple screening method is needed to identify rice genotypes tolerant to low phosphorus (P) in soil. Nagina 22 (N22) mutants were classified as gain of function (gof) and loss of function (lof) for tolerance to very low P (soil Olsen P 2.01 mg kg^?1). Two gof and two lof mutants were grown in hydroponics and in pot experiment at three P levels (-P, +P and +2P). Comparing response at +P and +2P in hydroponics we found that shoot and root dry weight were significantly less in gof and significantly more in lof in +2P. In pots with soil, tiller number and yield/plant was 3 fold less in gof but 2.5 to 3 fold more in lof and N22 in +2P compared to +P. That 2P can be used to identify low-P tolerant genotypes was validated using 3 low-P tolerant and 3 sensitive varieties whose response to low P soil is well documented. Both shoot and root dry weight was significantly less in +2P than in +P in tolerant and significantly more in sensitive genotypes. Thus screening in hydroponics in +2P can help identify low-P- tolerant genotypes easily and rapidly avoiding field screening.     

Change of Organic Carbon Content and Its Fractions in Black Soil under Long‐Term Application of Chemical Fertilizers and Recycled Organic Manure

Abstract

Soil organic matter (SOM) is an important indicator for soil quality and sustainable agriculture, and agricultural practices may strongly affect SOM content and chemistry. Thus, a long‐term experiment was conducted in northeast China to study the effect of chemical fertilizers and recycled organic manure on the contents of SOM along its fractions of black soil (0–20‐cm depth). Eight treatments were used: 1) control, 2) recycled organic manure (ROM), 3) nitrogen (N) alone, 4) N+ROM, 5) N+phosphorous (P), 6) N+P+ROM, 7) N+P+potassium (K), and 8) N+P+K+ROM. The results showed that from 1985 to 2002; soil total organic carbon (TOC) decreased by 6.5% over the 18 years in control (33.25 g/kg in 1985), 5.6% in ROM treatment, and 5.1% in N‐alone treatment, and 1.5% in the N+P treatment but increased by 0.3% in the N+P+K treatment. In the three treatments of chemical fertilizers together with ROM (i.e., N+ROM, N+P+ROM, and N+P+K+ROM), soil TOC content in 2002 increased by 0.3%, 1.3%, and 2.8%, respectively, when compared with control in 1985. Compared with control in 2002, light fraction organic carbon (LFOC) content increased by 23% in N+ROM treatment, 24% in N+P+ROM, and 28% in N+P+K+ROM, and readily oxidized carbon (ROC) content increased by 24% 31%, and 39%, respectively, in these three treatments. The ROC was well correlated with soil TOC. Compared with the data from 18 years ago, in all eight treatments organic carbon of soil in the humic acid fraction decreased by 5.0–13% and in fulvic acid decreased by 1.4–14%; however, with chemical fertilizers and ROM applied together, the rate of decrease was reduced. Overall, ROM is effective for increasing the content of soil TOC and thus, its different active carbon fractions in black soil would help to maintain or increase soil productivity.     

Soil organic matter and nutrient accumulation in areas under intensive management and swine manure application

Purpose

Land use change and soil management are frequently associated to land degradation and soil organic matter (SOM) losses in tropical regions. In Brazil, in order to avoid this process, different management strategies have been applied, such as no-tillage and agricultural disposal of swine manure (SM). This study was carried out to evaluate the quantity and quality of SOM, as well as the occurrence of nutrient accumulation in soils of areas under contrasting management systems that have received consecutive applications of SM over the last decades in Brazil.

Materials and methods

Five land uses were sampled: native vegetation (NV), pasture with SM application (PA + SM), no-tillage with SM application (NT + SM), no-tillage (NT), and conventional tillage with SM application (CT + SM). Soil organic carbon (SOC), N, labile C, C management index (CMI), P, Ca²⁺, Mg²⁺, K⁺, Al³⁺, Fe, Zn, Mn, Cu, and H + Al were quantified.

Results and discussion

Except for PA + SM, the agricultural land uses caused decreases in SOC contents comparing to NV. PA + SM showed the highest C stocks, 138.9?±?3.4 Mg ha^?1 down to 0.4 m. The application of SM can be associated to the greater C stocks in PA + SM, NT + SM, and CT + SM and to the higher N contents in all land uses under this practice. Land uses which receive higher rates of swine manure application (PA + SM and CT + SM) have shown CMI greater than 100. However, this practice is associated to the accumulation of P, Cu, Na, and Zn in these soils.

Conclusions

The SM application is associated to improvement on C stocks and SOM quality in area under pasture, no-tillage, and conventional tillage in Paraná State, Brazil. However, this practice is the main driver of nutrient accumulation in these areas.

     

土壤铅和镉溶出伏安法检测中影响因素及其削弱方法研究进展

溶出伏安法具有分析速度快、成本低、灵敏度高等优点被广泛应用于检测土壤重金属含量,但在检测土壤重金属时,溶出伏安检测精度会受到多方面因素的影响。该文在介绍溶出伏安法工作原理的基础上,从伏安参数、试验条件和土壤物质成分三方面阐述溶出伏安法检测土壤Pb2+和Cd2+为的影响因素,解析各因素的影响机理,归纳影响削弱方法的研究进展。研究结论为：方波脉冲阳极溶出伏安法最常用于检测土壤Pb2+和Cd2+,伏安参数包括脉冲幅值、电压增量和脉冲频率,试验条件包括沉积时间、沉积电压和支持电解质种类及其pH值,土壤成分主要干扰因素包括非目标重金属和有机质。针对伏安参数和试验条件的影响可以设计优化试验有效削弱。针对非目标重金属和有机质的干扰影响,目前研究还没有提出有效的削弱方法。最后,展望了溶出伏安法检测土壤重金属的未来发展方向。     

The in vivo and in vitro effects of Ca2+ and Al3+ upon ATPases from barley roots

Experiments were performed to test the effect of Ca²⁺ and Mg²⁺ upon ATPases (E.C. 3.6.1.3) from barley roots (Hordeum distichon L. cv. MULTUM) that had or had not taken up Al³⁺. Furthermore, the effect of the uptake period was examined. With longer duration of the Al³⁺ uptake, the activity of the ATPases dropped, independently of whether they were activated by Ca²⁺ or by Mg²⁺. Mg²⁺ stimulated the activity of the ATPases if no Al³⁺ had been taken up with lacking Ca²⁺ in the assay. If Al³⁺ had been taken up no additional activation by Mg²⁺ to the Ca²⁺ stimulation could be observed, and in some cases Mg²⁺ decreased the Ca²⁺ stimulation.     

保水剂在不同铵盐溶液体系中的吸水和吸附铵离子特征

为探明保水剂与NH4+的相互作用,选用聚丙烯酸盐型保水剂(PAA)和聚丙烯酰胺型保水剂(P(AA-AM)),研究了保水剂在系列NH4Cl、NH4Cl-KCl、NH4Cl-CaCl2溶液体系中的吸水行为和对铵离子的吸附特征。结果表明:铵离子能显著降低保水剂的吸水倍率,并随铵离子浓度的增加,吸水倍率显著降低,相对吸水倍率与NH4+浓度之间具有显著的幂函数的减函数关系;NH4+、K+、Ca2+单一体系,NH4+-K+、NH4+-Ca2+共存体系对保水剂吸水倍率的影响按NH4+-K+相似文献   

Pot study on wheat growth in saline and waterlogged compacted soil: II. Root growth and leaf ionic relations

Soil compaction affects plant growth by causing increased resistance to root penetration and a decreased uptake of water and ions. A pot experiment was conducted to study the effect of soil compaction in conjunction with the soil salinity and waterlogging on root growth and leaf ionic composition of two wheat genotypes (Aqaab and MH-97). Compaction was achieved at a 10% soil moisture content by dropping 5 kg weight, controlled by a tripod stand for 20 times from 0.6 m height on a wooden block placed inside the soil-filled pots. Soil bulk density of non-compact and compact treatments was measured as 1.21 and 1.65 Mg m⁻³, respectively. The desired salinity level (15 dS m⁻¹) was developed by mixing required amount of NaCl in the soil before filling the pots. Waterlogging was developed by flooding the pots for 21 days both at tillering and booting stages. Compaction significantly reduced the root length density (RLD) of both the wheat genotypes while the combined effect of compaction×salinity was more drastic on root length density than compaction alone. Waterlogging however, did not decrease the root length density, rather it mitigated the effect of compaction. Compaction decreased the concentration of K⁺ and K⁺:Na⁺ ratio in leaves. Salinity also decreased the concentration of K⁺ and K⁺:Na⁺ ratio, but increased the concentrations of Na⁺ and Cl⁻ in the crop leaves. Salinity and compaction interacted to cause a greater reduction in K⁺ concentration and the K⁺:Na⁺ ratio, while there was lesser increase in the concentrations of Na⁺ and Cl⁻ compared with salinity alone. Waterlogging also decreased the concentration of K⁺ and K⁺:Na⁺ ratio in leaves. It intensified the effect of salinity but decreased the effect of compaction on leaf ionic composition. Therefore, the effect of compaction on root growth and ion uptake is more severe under salt-affected soil conditions than under normal soil conditions while occasional waterlogging of a compact soil for a few days makes the soil conditions favorable for root growth both under non-saline as well as saline soil conditions. Also, the performance of a genotype in stressed environment is related to maintenance of higher root length density, leaf K⁺ concentration and K⁺:Na⁺ ratio and lower leaf Na⁺ and Cl⁻ concentrations.     

Correlation between the morphogenetic types of litter and their properties in bog birch forests

A formalized arrangement of morphogenetic types of litter according to the physicochemical parameters provided their significant grouping in three genetic associations. The litter group (highly decomposed + moderately decomposed) is confined to the tall-grass group of bog birch forests. The rhizomatous (roughly decomposed) litter is formed in the sedge-reed grass bog birch forests. The litter group (peaty + peatified + peat) is associated with the bog-herbaceous-moss group of forest types. The genetic associations of the litters (a) reliably characterize the edaphic conditions of bog birch forests and (b)correspond to formation of the peat of certain ecological groups. We found highly informative the acid-base parameters, the exchangeable cations (Ca²⁺ + Mg²⁺) and the total potential acidity, which differentiated the genetic associations of litter practically with 100% probability. The expediency of studying litters under groups of forest types rather than under separate types of bog birch forests was demonstrated.     

Analysis and use of cumulative nutrient uptake formulas in plant nutrition and the temporal-weight-averaged influx

A generalized cumulative uptake formula of nutrient uptake by roots following our previous formula (Reginato-Tarzia, Comm. Soil Sci. and Plant., 33 (2002 Reginato, J. C., and D. A. Tarzia. 2002. An alternative formula to compute the nutrient uptake for roots. Communications in Soil Science and Plant Analysis 33 (5&;6):821–30.[Taylor &; Francis Online], [Web of Science ®] , [Google Scholar]), 821-830) is developed. Cumulative nutrient uptake obtained by this formula is compared with the simulated results obtained by the Claassen and Barber (Claassen and Barber, Agronomy J., 68 (1976 Claassen, N., and S. A. Barber. 1976. Simulation model for nutrient uptake from soil by a growing plant root system. Agronomy Journal 68:961–64.[Crossref], [Web of Science ®] , [Google Scholar]) 961–964) and Cushman (Cushman, Soil Sci. Soc., 43 (1979 Cushman, J. H. 1979. An analytical solution to solute transport near root surfaces for low initial concentrations: I. Equation development. Soil Science Society of America Journal 43:1087–90.[Crossref], [Web of Science ®] , [Google Scholar]) 1087–1090) formulas. A mass balance is analyzed for the three formulas of cumulative nutrient uptake in order to decide which of them is correct. Moreover, the mass balance is also verified through a computational algorithm using data obtained from literature, and we compute the potassium (K) uptake for maize for low and high soil concentrations using the three mentioned formulas. The theoretical analysis shows that Claassen and Barber, and Cushman formulas do not verify, in general, the mass balance condition. The Claassen and Barber formula only verifies this condition when the influx is constant and root grows linearly. The Cushman formula verifies the mass balance when the influx is constant regardless of the law of root growth. Reginato and Tarzia formula always verifies the mass balance whatever be the representative functions for the influx and the law of root growth. Moreover, we propose a redefinition of the averaged influx from which the Williams formula (Williams, J. Scientific Res., 1 (1948 Williams, R. F. 1948. The effect of phosphorus supply on the rates of intake of phosphorus and nitrogen upon certain aspects of phosphorus metabolism in gramineous plants. Australian Journal of Scientific Research 1:333–61. [Google Scholar]) 333–361) can be deduced. We remark that Williams formula is a consequence of our definition of temporal-weight-averaged influx for all root growth law expressions. Also, we present a comparison of influx and cumulative uptake of cadmium (Cd) with data extracted from literature. Cumulative uptake is obtained through the Barber–Cushman model and our moving boundary model by using the redefinition of averaged influx on root surface and the correct cumulative uptake formula presented in this paper.     

Nutrient disturbances in forest trees and the nature of the forest decline in Quebec and Germany

The serious decline of forest trees in Quebec and adjacent areas of the U.S. parallel those observed in Germany. In certain locations, in both cases, K deficiency is now occurring on glacial tills and outwash soils and is associated with a low concentration of exchangeable K⁺ and a high molar ratio of exchangeable Ca⁺ ions to K⁺ ions in the soil. This deficiency results from the so-called Ca-K antagonism in which an increased concentration of Ca²⁺ ions blocks the entry of a reduced concentration of K. Mg deficiency is occurring on granitic soils and results from a low concentration of exchangeable Mg²⁺ and a high molar ratio of A1³⁺ ions to Mg²⁺ ions. The role of the parent rock, weathering reactions and atmospheric inputs are discussed in relation to the changes that have resulted from the cumulative effect of acid deposition. The changes in storage, transfer and losses of cationic nutrients in soil and trees can explain the development of these imbalances, which are still increasing, and are resulting in these forest declines.     

水稻根尖边缘细胞对铁毒的形态生理响应

以水稻(Oryza sativa L.)品种Azucena（铁耐性）和IR64（铁敏感）为材料,研究了Fe2+毒胁迫下附着于根尖边缘细胞(即原位边缘细胞)的数目、存活率,根尖细胞形态结构、根尖保护酶活性的变化。结果显示,Fe2+ 毒对根边缘细胞的产生有抑制作用。相对于敏感性品种而言,一定浓度Fe2+(100~200 μmol/L)有利于耐性品种边缘细胞的产生;Fe2+ 毒对边缘细胞有致死效应,随Fe2+浓度的提升,边缘细胞的存活率呈下降趋势,根尖外围细胞壁增厚,并出现细胞程序性死亡特征(敏感性品种)。同时,Fe2+ 毒对根尖保护酶活性有一定的影响,200~400 μmol/L Fe2+处理下,耐性品种POD、CAT、SOD活性都超过对照;敏感品种只有SOD活性超过对照。说明Fe2+毒胁迫下,水稻根尖通过增加边缘细胞数目、提高细胞拒铁作用,维持较高水平的POD、CAT和SOD活性来对抗Fe2+毒,缓解铁毒害。