Sequential extraction of copper from soils and relationships with copper in maize

We studied copper uptake by maize grown on soils that have been contaminated with CuSO₄. In soil the total copper level ranged from 24 to 135 mg kg^–1. The copper distribution in soil fractions was assessed by sequential extraction, showing that anthropogenic copper is mainly concentrated in oxides fractions. The copper concentration of maize at the maturity stage reached values from 36.3 to 65.9 mg kg^–1 compared to copper levels usually found in non-contaminated crops (5–30 mg kg^–1). Here we demonstrate that copper can be accumulated by maize and that copper concentration in maize can be predicted by equations including copper concentration of soil fractions.     

不同耕作和培肥模式对豫中冬小麦田土壤腐殖质及微生物区系的影响

了解不同耕作与培肥模式对麦田土壤的影响,对提升麦田土壤地力及促进小麦的持续高产具有重要的意义。试验于2011-2012年在许昌县陈曹乡史庄村小麦试验田进行,以周麦22为试验材料,分别于孕穗期、开花期和成熟期取土测定土壤微生物与腐殖质含量。借助方差分析和相关分析等经典统计方法研究了不同耕作模式（浅耕15~20 cm;深耕35~40 cm）和培肥模式（单施化肥;化肥增施有机肥）对麦田土壤腐殖质与微生物的影响。试验结果表明：深耕增施有机肥能够显著提高小麦生育后期0~5和5~20 cm耕层土壤富里酸含量（p〈0.01）。增施有机肥有利于小麦生育后期各耕层土壤胡敏酸含量的积累（p〈0.05）,其中20~40 cm耕层土壤增幅最为明显,成熟期深耕增施有机肥与浅耕增施有机肥和开花期相比增幅分别达253.85%与300.00%;深耕增施有机肥能够显著提高小麦孕穗期与成熟期5~20 cm耕层土壤细菌数量（p〈0.01）,成熟期浅耕增施有机肥与深耕增施有机肥处理细菌数量和开花期相比增幅分别达690.38%和508.75%,其中深耕增施有机肥处理与其它三个处理相比细菌数量最多且差异极显著（p〈0.01）。增施有机肥能够显著提高小麦成熟期0~5与20~40 cm耕层土壤真菌数量（p〈0.01）,深耕增施有机肥能够显著提高小麦孕穗期5~20 cm耕层土壤真菌数量（p〈0.01）。深耕增施有机肥能够显著提高小麦生育后期20~40 cm耕层土壤放线菌数量（p〈0.05）。相关分析表明,在本研究培肥和耕作模式下麦田土壤腐殖质组分的含量与微生物区系的数量呈正相关关系。     

Effects of organic and inorganic fertilisation on soil nutrient dynamics in a Savannah region (DR Congo)

Very few studies have considered the residual effect of inorganic and organic fertilisation on oxisol chemistry and plant productivity while studying the response of maize to fresh fertiliser application. The purpose of the present study was to examine the effects of five treatments of inorganic and organic fertilisers on maize productivity and soil fertility under field conditions in a Savannah region. The trials were conducted from 2009 to 2011 and the treatments included inorganic nitrogen–phosphorus (NP), Entada abyssinica, Tithonia diversifolia, inorganic NP combined with E. abyssinica, and inorganic NP combined with T. diversifolia, and no fertilised plots. The combination of NP with T. diversifolia or E. abyssinica leaves resulted in the highest increase in grain yields during the first crop season.The positive residual effects of fertilisers on maize grain yield were strong and significant in the immediate succeeding season and decreased during the second year following fertilisation. The highest residual effect was observed in plots fertilised with E. abyssinica combined with NP, followed by T. diversifolia combined with NP, and E. abyssinica and T. diversifolia without NP, respectively. The lowest residual effect was observed in plots fertilised with inorganic NP. Analytical results revealed that total nutrients in the soil matrix are not dominantly in forms available for plant uptake. There were significant residual effects for total potassium in the site with low initial nutrient levels. The soil content of bioavailable phosphorus, nickel, zinc, copper, and cobalt was in general below detectable levels.     

Use of Maize (<Emphasis Type="Italic">Zea mays</Emphasis> L.) for phytomanagement of Cd-contaminated soils: a critical review

Maize (Zea mays L.) has been widely adopted for phytomanagement of cadmium (Cd)-contaminated soils due to its high biomass production and Cd accumulation capacity. This paper reviewed the toxic effects of Cd and its management by maize plants. Maize could tolerate a certain level of Cd in soil while higher Cd stress can decrease seed germination, mineral nutrition, photosynthesis and growth/yields. Toxicity response of maize to Cd varies with cultivar/varieties, growth medium and stress duration/extent. Exogenous application of organic and inorganic amendments has been used for enhancing Cd tolerance of maize. The selection of Cd-tolerant maize cultivar, crop rotation, soil type, and exogenous application of microbes is a representative agronomic practice to enhance Cd tolerance in maize. Proper selection of cultivar and agronomic practices combined with amendments might be successful for the remediation of Cd-contaminated soils with maize. However, there might be the risk of food chain contamination by maize grains obtained from the Cd-contaminated soils. Thus, maize cultivation could be an option for the management of low- and medium-grade Cd-contaminated soils if grain yield is required. On the other hand, maize can be grown on Cd-polluted soils only if biomass is required for energy production purposes. Long-term field trials are required, including risks and benefit analysis for various management strategies aiming Cd phytomanagement with maize.     

Sensitivity of a crop growth simulation model to variation in LAI and canopy nitrogen used for run-time calibration

Run-time calibration, i.e. adjusting simulation results for field observations of model driving variables during run-time, may allow correcting for deviations between complex mechanistic simulation model results and actual field conditions. Leaf area index (LAI) and canopy nitrogen contents (LeafNWt) are the most important driving variables for these models, as they govern light interception and photosynthetic production capacity of the crop. Remote sensing may provide (spatial) data from which such information can be estimated. How, when and at what frequency such additional information is integrated in the simulation process may have various effects on the simulations. The objective of this study was to quantify the effects of different run-time calibration scenarios for final grain yield (FGY) simulations in order to optimize remote sensing image (RS) acquisition. The PlantSys model was calibrated on LAI and LeafNWt for maize in France and used to simulate maize crop growth in the Argentina and the USA, for which non-destructive estimates of LAI and leaf chlorophyll contents were acquired by optical measurement techniques. Leaf chlorophyll data were used to estimate LeafNWt. Due to its structure, the PlantSys model was more susceptible to run-time calibration with LeafNWt than with LAI. Run-time calibration with LAI showed the largest effect on FGY before and around flowering, and could mainly be related to maintenance respiration costs. Run-time calibration with LeafNWt showed the largest effect on FGY at and after flowering and could mainly be related to the change in effective radiation interception due to change in leaf life. The accuracy of LAI estimates showed a major effect on FGY for underestimations but was small in absolute sense. The accuracy of LeafNWt estimates had significant impact at all crop development stages, but was the strongest after flowering where crop growth and nitrogen uptake are less able to recuperate from changes in LeafNWt. In absolute sense, the effect on FGY was as strong as the accuracy of the LeafNWt estimates when applied in the early reproductive stages. Based on these results it was concluded that remotely sensed in-field variability of LAI and LeafNWt is valuable information that can be used to spatially differentiate model simulations. Run-time calibration at sub-field level may lead to more accurate simulation results for whole fields.     

Crop growth,soil water and nitrogen balance simulation on three experimental field plots using the Opus model—A case study

Over a period of 5 years, the agro-ecosystem model Opus was used to simulate soil water and nitrogen balance as well as crop growth for three experimental field plots. At these plots, different agricultural management practices were applied. The data set obtained from these plots consists of automatically recorded time series of daily volumetric soil water contents measured by TRIME-probes as well as daily pressure heads measured by tensiometer. Aboveground total biomass, yield, nitrogen-uptake by crops as well as nitrate contents in the soil were measured at 6–10 sample times per year. The objective of this study was an evaluation of the accuracy of Opus regarding the simulation of crop growth, soil water and nitrogen balance. The simulations of soil water contents and pressure heads correspond with the commonly measured trends in soil depths shallower than 60 cm. In depths deeper than 60 cm, some differences between measured and simulated soil water contents as well as pressure heads could be observed. Nitrate contents in the root zone and the aboveground total biomass were simulated satisfactorily. In contrast to that, simulated and observed yields show greater discrepancies. This indicates the need of a site specific calibration of crop growth parameters within the Opus model.     

13C-dating, the first method to calculate the relative age of molecular substance homologues in soil

This article reports the design of ¹³C-dating, the first method to calculate the relative age of molecular substance homologues occurring in fractions from the same soil sample. Soil is a major carbon pool impacting modern climate by CO₂ release and uptake. Molecular substances that sequester carbon in soils are poorly known due to the absence of methods to study molecular-level C dynamics over agricultural time scales, e.g., 0–200 years. Here, I design a method to calculate the relative age of the plant-derived C₃₁ n-alkane occurring in 6 fractions from a soil sample naturally ¹³C-labelled by maize cropping during 23 years. Soil fractions are the bulk soil extract, two humin-encapsulated fractions and three particle-size fractions. Results show that C₃₁ n-alkane homologues have relative ages ranging from −6.7 years for the humin-encapsulated homologue to +25.1 years for the 200–2,000-μm fraction homologue. Such a wide variation of 31.8 years evidences temporal pools of molecular substances in soil. This finding also reveals that physical encapsulation can strikingly change the dynamics of a single molecular substance. ¹³C-dating thus allows to assess the carbon storage potential of molecular substances from crop soils. Such knowledge will help to identify molecular compounds, associated soil pools and agricultural practices that favour carbon sequestration. ¹³C-dating is further applicable to any environmental sample containing organic matter subjected to a ¹³C isotope shift with time. ¹³C-dating will also help to study the sequestration and delayed release of chemicals in various disciplines, such as pollutants in environmental sciences, pharmaceuticals in medicine, and nutrients in food science.     

Herbicides interactions with cow manure and field soil organic matter

The direct interaction of the herbicide metazachlor ‐chosen as an example‐ with the soil organic matter has been studied by laboratory incubation of old and young cow manures containing metazachlor. The extraction efficiencies of solvents of increasing polarities indicated the formation of association compounds by bonds weaker than covalent between metazachlor and the organic matter: electron donor‐acceptor complexes, hydrogen bonding complexes, and complexes by both bonding types. Laboratory incubation of metazachlor in soil of low organic matter content indicated that the soil mineral part only had a diluting effect on the soil organic matter capacity to adsorb metazachlor. Similar association compounds were observed in the soil of a cauliflower field crop. Their concentrations were greater in the plots treated with organic fertilizers than in the organic fertilizers untreated plots. The free‐ unbound metazachlor was faster metabolized than the one bound to the soil organic matter, explaining why the organic fertilizer treatments slow down the herbicide soil biodegradation during the main first crop period. Inclusion of metazachlor in the field soil humic acids lattice ‐another kind of herbicide association compound with the soil organic matter‐ occurred at crop end when most of the metazachlor was metabolized; the soil concentrations of this kind of association compound thus was low, so that the release after crop of metazachlor in the environment has no practical significance.     

有机无机肥料对土壤肥力和作物产量的影响研究初报

研究有机无机肥料对土壤肥力及作物产量的影响．５年的定位监测结果表明，施无机Ｎ、Ｐ、Ｋ结合冬蔬菜残茎叶还田，不但能增加作物产量和提高经济效益．而且还能培肥土壤．而无机肥料加猪粪或冬绿肥还田的增产效果及土壤培肥效果与全无机肥相近．稻秆还田是增加土壤有机质的一项比较明显的有效措前，这一结论得到了再次验证．施用有机肥料可以增加土壤有效态微量元素的含量．     

土壤铜植物毒害的不同评价终点和室内外测定差别研究

本论文对山东陵县、湖南祁阳和浙江嘉兴3种性质差异较大的土壤上进行的室内外的土壤外源铜(Cu)的植物毒性试验结果进行了比较。结果发现3种室内评价终点(大麦根长、西红柿和小白菜苗期生物量)和田间植物(玉米、小麦、水稻和油菜产量)对土壤中Cu毒性的敏感性存在较大的差异。大麦根伸长和小白菜生物量法高估了土壤中Cu对田间小麦、玉米和水稻产量的毒害,而室内西红柿生物量法则低估了土壤中Cu对田间小麦、玉米和水稻产量的毒害。小白菜和田间油菜的敏感性接近,可以用室内小白菜苗期生物量作为土壤中Cu对田间油菜产量毒性评价的植物。当采用相同植物比较时,陵县小麦、祁阳玉米和嘉兴油菜的室内苗期值可以作为土壤Cu对相同田间植物产量的毒害作用(EC_(10))的评价指标。但是,室内苗期毒害指标会低估Cu对田间祁阳小麦和高估嘉兴水稻的毒害作用,说明土壤Cu植物毒害室内外测定的差别受土壤和植物的影响。     

盐碱地施用脱硫石膏对土壤养分及油葵光合特性的影响

通过分析宁夏平罗西大滩不同改良年份盐碱地土壤养分含量,测定油葵(Helianthus annuus)光合日变化曲线、光响应曲线和油葵产量,研究了施用脱硫石膏对盐碱地土壤改良及油葵光合特性的影响.结果表明,在盐碱土壤上施用燃煤电厂脱硫石膏后,土壤电导率、pH值随土壤改良年限增加而逐年下降,土壤有机质含量、碱解氮、有效磷和速效钾则逐年上升.随着土壤改良年限增加,油葵叶片净光合速率、蒸腾速率、气孔导度、胞间二氧化碳浓度均明显下降,气孔限制值和水分利用效率也明显下降(P<0.01).同时,随着改良年限增加,油葵叶片暗呼吸速率、光饱和点和最大净光合速率增加,而光补偿点降低.施用脱硫石膏后油葵盘径、百粒重和产量随土壤改良年限增加也显著提高(P<0.05).因此,施用燃煤电厂脱硫石膏能够显著地改良盐碱地土壤、提高油葵叶片光合能力,从而促进作物生长、提高作物产量.图2表3参29     

玉米（Zea mays）对镉积累与转运的品种差异研究

通过田间实验,研究了25个玉米（Zea mays）品种在Cd质量分数为50 mg·kg-1胁迫条件下,Cd对不同玉米品种生长的影响,以及不同玉米品种对Cd积累和转运的品种差异,以期筛选出Cd低积累玉米品种。结果表明：25个玉米品种的生物量和产量对Cd胁迫的响应,以及不同品种根、茎叶和籽粒对Cd的吸收、累积及转运能力存在显著差异（P＜0.05）。有20个品种生物量和19个品种产量下降;有2个品种籽粒的Cd质量分数超过了国家规定的食品卫生标准（≤0.1 mg·kg-1）,占供试品种的8.0%,所有品种茎叶的Cd质量分数均超过了国家规定的饲料卫生标准（≤0.5 mg·kg-1）,超标率为100%;25个玉米品种的富集系数范围为0.063~0.899、茎叶转运系数范围为0.038~0.554、籽粒转运系数范围为0.000~0.111,均小于1,其中有8个品种富集系数〉0.5,1个品种茎叶转运系数〉0.5,而所有品种的籽粒转运系数均〈0.5,说明玉米对土壤Cd仍有一定的吸收能力,但地下部向地上部转运能力以及由茎叶向籽粒的转运能力较弱;根据玉米生物量、产量、籽粒Cd含量以及对Cd的富集系数和转运系数等指标进行评价,认为云瑞8号、会单4号、路单7号3个品种可作为Cd低累积玉米品种,可在云南Cd重度污染土壤上推广种植。     

Quantification and fractionation of mercury in soils from the Chatian mercury mining deposit,southwestern China

Contents of total Hg and Hg fraction, organic matter, pH, grain size and chemical composition were measured to investigate the pollution characteristics and binding behavior of Hg in soils collected from the Chatian Hg mining deposit (CMD), southwestern China. The average concentration of Hg concentration in the CMD soils was 155 and 1,315 times higher than that in control soils and Chinese soils, respectively, suggesting that the CMD soils were heavily contaminated by the element. The finding was confirmed by Müller geoaccumulation index assessment with 75% very seriously polluted, 6.25% highly to very highly polluted and 18.75% moderately to highly polluted. Hg sources in the region were natural and anthropogenic: in addition to the pedogenic process and original geochemical situation, human mining–refining activities have also seriously impacted the redistribution of Hg in soils, especially in paddy soils. Based on the BCR protocol, soil Hg was divided into exchangeable (EXC), amorphous Fe–Mn oxides (AFe–MnOX), organic-crystalline iron oxides (OM-CFe) and residual (RES) fraction. The average percentage of the four fractions in the CMD followed the trend: RES (85.77%) > OM-CFe (12.44%) > AFe–MnOX (0.93%) ≥ EXC (0.86%), suggesting that the majority proportion of soil Hg in the study area remained of residual form inside the soil mineral matrix. However, their concentrations and percentages significantly varied among different locations and land use types. Soil physico-chemical parameters were key factors affecting the presence of Hg fraction. Generally, Hg fraction concentrations were positively correlated with the sand contents and soil pH values, which was presumably due to the basic anthropogenic input of Hg-containing materials and their similarity to sand in physical characteristics. However, organic matter caused adsorption–fixation and reduction–volatilization to coexist, which had opposite effects on Hg concentrations in soil, consequently exhibiting its dual nature.     

The MONICA model: Testing predictability for crop growth, soil moisture and nitrogen dynamics

A fundamentally revised version of the HERMES agro-ecosystem model, released under the name of MONICA, was calibrated and tested to predict crop growth, soil moisture and nitrogen dynamics for various experimental crop rotations across Germany, including major cereals, sugar beet and maize. The calibration procedure also included crops grown experimentally under elevated atmospheric CO₂ concentration. The calibrated MONICA simulations yielded a median normalised mean absolute error (nMAE) of 0.20 across all observed target variables (n = 42) and a median Willmott's Index of Agreement (d) of 0.91 (median modelling efficiency (ME): 0.75). Although the crop biomass, habitus and soil moisture variables were all within an acceptable range, the model often underperformed for variables related to nitrogen. Uncalibrated MONICA simulations yielded a median nMAE of 0.27 across all observed target variables (n = 85) and a median d of 0.76 (median ME: 0.30), also showing predominantly acceptable results for the crop biomass, habitus and soil moisture variables. Based on the convincing performance of the model under uncalibrated conditions, MONICA can be regarded as a suitable simulation model for use in regional applications. Furthermore, its ability to reproduce the observed crop growth results in free-air carbon enrichment experiments makes it suited to predict agro-ecosystem behaviour under expected future climate conditions.     

土壤重金属复合污染对作物的影响

本文采用盆栽试验，研究了石灰性土壤中铜、镍、铅、锌复合污染对大豆和水稻的影响，并讨论了离子冲量在表征复合污染的综合效应及污染金属总量控制中的应用。结果表明：对于水稻，共存元素协同使产量降低，它们的影响顺序是：铜＞锌＞镍＞铅；对于大豆，铜、铅、锌的存在降低了镍的毒性，影响顺序了：铜＞铅＞锌＞镍。供试元素在作物体内的累积、分布和迁移除了受到本身性质和添加量影响外，还受到元素相互作用的影响，后者的影响很     

施肥及秸秆还田处理下玉米季温室气体的排放

以华北地区冬小麦-夏玉米轮作农田为研究对象,在玉米整个生长季,运用静态箱法针对正常施肥及正常施肥结合秸秆还田处理进行了为期3年N2O排放通量的连续观测,并开展了1季CO2和CH4交换通量的研究.在玉米整个生长过程中施肥阶段N2O的排放量占到了总排放量的83%—96%,表明现有化肥的使用明显导致了农田N2O排放增加.与控制地相比,施肥和耕种可导致玉米田CO2排放明显增加,且正常施肥及秸秆还田样地CO2排放主要集中在苗期至吐丝期.控制地、正常施肥样地及施肥结合秸秆还田样地CH4的累积排放量均为负值,说明旱地土壤是CH4的一个汇.秸秆还田在一定程度上增加了玉米季N2O和CO2的排放量,但对CH4的吸收有所抑制.正常施肥样地和秸秆还田样地全球净增温潜势分别为-1392.8 kg C.hm-2和-179.2 kg C.hm-2,表明华北农田在现有耕作方式下是大气温室气体的一种重要汇.     

施用污泥堆肥对作物和土壤的影响

污泥中的有机质、营养成分可为农业生产提供重要的有机肥源,但污泥中的重金属是制约污泥农用的重要因素,为检验污泥堆肥施用后对作物及土壤的影响,文章对污泥与稻草或木屑堆肥的产品进行了盆栽试验研究。结果表明,污泥与稻草或木屑的堆肥作为肥料施用于萝卜(Brassicacampestris)和菜心(Brassicaparachinensis),产量明显提高,部分堆肥产品增产效果优于化肥,且后效明显。堆肥施用使土壤中有机质、各养分含量增加,微生物活动增强、数量增加,然而作物和土壤中的重金属含量也有不同程度的提高。     

不同施肥模式对华北平原小麦-玉米轮作体系产量及土壤硝态氮的影响

为了探索培育高产粮田的施肥模式,实现氮肥资源的高效利用与环境效益,以华北平原的小麦（Triticum aestivum）-玉米（Zea mays L.）轮作体系作为研究对象,通过2007─2011年4个轮作季,探讨不同的施肥模式对作物产量和土壤硝态氮的影响。试验以处理A（当地传统管理）作为对照,从测土确定施肥量、按作物生长发育明确施肥时期、合理分配各时期的养分配比及增施有机肥等方面改变传统施肥模式,设置3种高产施肥培育模式,分别为处理B（现有高产田推荐管理）、处理C（高肥料投入管理）和处理D（水肥高效管理）,进行田间小区试验。4个轮作季的总产量以处理D为最高,达75430 kg·hm-2,其次是处理C为75166 kg·hm-2,当地传统的产量最低。冬小麦季的吸氮量为处理C和D显著高于A处理,分别高出444.78 kg·hm-2和310.20 kg·hm-2,但与处理B无显著差异;处理D在夏玉米季的吸氮量为776.75 kg·hm-2,显著高于处理A。处理B的氮肥偏生产力值最高为38.21,处理D为36.71,处理A和C均为28.33。各处理经过4个轮作季后,土壤硝态氮均在120-160 cm出现累积峰,A、B、C和D的硝态氮峰值分别为58.65、28.98、105.89、45.29 mg·kg-1。在0-100cm土层,处理B的硝态氮累积量达到144.22 kg·hm-2,显著高于处理A、C、D;所有处理在100-200 cm土层均出现较高的硝态氮累积,处理C高达1021.19 kg·hm-2;0-400 cm的土壤硝态氮累积量分别为724.27、711-92、1324.30、730.70 kg·hm-2。处理A、B、C、D在耕层土壤氮素的表观损失分别为1298.95、653.18、1236.39和718.43 kg·hm-2,处理B、D显著低于处理A、C,D和B间差异不显著。因此,处理D是培育高产的理想施肥模式,合理的施肥量、科学的施肥时期以及有机无机的合理配比是达到高产、提高肥效和环境友好的关键。     

Modeling soil and plant phosphorus within DSSAT

The crop models in the Decision Support System for Agrotechnology Transfer (DSSAT) have served worldwide as a research tool for improving predictions of relationships between soil and plant nitrogen (N) and crop yield. However, without a phosphorus (P) simulation option, the applicability of the DSSAT crop models in P-deficient environments is limited. In this study, a soil-plant P model integrated to DSSAT was described, and results showing the ability of the model to mimic wide differences in maize responses to P in Ghana are presented as preliminary attempts to testing the model on highly weathered soils. The model simulates P transformations between soil inorganic labile, active and stable pools and soil organic microbial and stable pools. Plant growth is limited by P between two concentration thresholds that are species-specific optimum and minimum concentrations of P defined at different stages of plant growth. Phosphorus stress factors are computed to reduce photosynthesis, dry matter accumulation and dry matter partitioning. Testing on two highly weathered soils from Ghana over a wide range of N and P fertilizer application rates indicated that the P model achieved good predictability skill at one site (Kpeve) with a final grain yield root mean squared error (RMSE) of 535 kg ha⁻¹and a final biomass RMSE of 507 kg ha⁻¹. At the other site (Wa), the RMSE was 474 kg ha⁻¹ for final grain yield and 1675 kg ha⁻¹ for final biomass. A local sensitivity analysis indicated that under P-limiting conditions and no P fertilizer application, crop biomass, grain yield, and P uptake could be increased by over 0.10% due to organic P mineralization resulting from a 1% increase in organic carbon. It was also shown that the modeling philosophy that makes P in a root-free zone unavailable to plants resulted in a better agreement of simulated crop biomass and grain yield with field measurements. Because the complex soil P chemistry makes the availability of P to plants extremely variable, testing under a wider range of agro-ecological conditions is needed to complement the initial evaluation presented here, and extend the use of the DSSAT-P model to other P-deficient environments.     

土壤肥力长期定位试验研究初报

１９８７～１９９７年的土壤肥力长期定位试验结果表明：空白区的产量更能反映耕地基础地力的高低;在目前的施肥水平下,氮、磷、钾配合施用能增加土壤有机质、全氮和碱解氮的含量;增施氮、钾肥能显著增加水稻产量。监测点较好地反映了广东省目前的农业生产状况,对农业生产具有一定的指导意义。