天津汉沽农田土壤－植物系统中汞的分布、迁移和积累

本文研究了受汞污染的农田土壤—植物系统中汞的分布,迁移和积累的规律。土壤中的汞在离污染源3公里的范围内含量最高;主要集中在0一20厘米的土壤上层,几乎不往下迁移。植物可以从土壤和大气中吸收、积累汞。在汉沽区没有发现由于汞污染所造成的植物受害症状。植物中的汞含量与土壤中的汞含量成正相关。土壤汞含量与水稻茎叶汞含量的相关系数为0.836(N=7),与糙米汞含量的相关系数为0.898(N=7)。植物不同部位的汞含量根>叶>茎>种子。不同作物种子比较,糙米>高粱>小麦。在大气中汞含量高的地段,植物地上部分汞含量高于根。土壤、植物中的汞不断地向大气扩散,而大气中的汞随着降雨、降尘等又不断地沉降到土壤和植物的气生表面,并可被植物吸收。汞向其邻近地区扩散的能力较小。     

滩涂围垦和土地利用对土壤微生物群落的影响

土壤微生物在生态系统营养物质循环过程,特别是碳、氮循环过程中扮演着重要的角色。上海市崇明岛位于长江入海口,因其土壤发育时间较短、土地利用历史背景清晰、土壤本底均一,不同土壤围垦年代的土壤,代表了土壤发育年代的不同时期。以空间变化代替时间变化,对崇明岛稻田和旱地6个不同围垦年代土壤的磷酸脂肪酸(PLFA)指纹图谱研究表明,湿地滩涂围垦16a后土壤微生物总PLFA、细菌PLFA、革兰氏阳性菌(G+)PLFA和革兰氏阴性菌(G-)PLFA含量显著降低。随着围垦时间的逐步增加,PLFA含量逐步上升。经过长时间的农业种植,G+PLFA在围垦120a和300a稻田和旱地土壤中没有显著性差异;而总PLFA、细菌和G-PLFA在围垦75、120a和300a的土壤中含量趋于稳定且没有显著性差异。围垦16a和40a稻田土壤中总PLFA和G+PLFA显著高于旱地土壤;围垦40a稻田土壤中细菌和G-PLFA显著高于旱地土壤。不同围垦年代土壤总PLFA、细菌PLFA与土壤总氮、粘土含量成显著的正相关关系。河口湿地围垦后微生物数量的变化与土壤营养含量存在强烈相关关系,提示土壤围垦及演替过程中微生物与土壤肥力之间的紧密关系,对探讨土壤演替过程中微生物群落的变化具有重要意义。     

北京东郊作物土壤系统中重金属的迁移、分布、积累

 本文研究了北京东郊污灌区重金属在作物—土壤中的迁移、分布、积累规律,证实本区蔬菜中汞含量比粮食作物约大3—15倍,比水果约大6—200倍。麦粒、糙米中的Cu、Hg、Cd、Pb、Ni的含量与土壤含量相关性不显著。架豆中重金属含量与土壤中重金属含量的相关性,只有Zn,Pb达显著水平。白菜土有机质含量与重金属含量相关性达显著水平,而白菜的重金属含量与土壤的重金属含量相关性却不显著。说明除了土壤中重金属的总量外,有效态含量的多少,是影响本区作物吸收积累重金属的主要因素。 本区施污泥的土壤和生长的作物Cd／Zn大部小于1%、盆栽试验证明：施用本区污泥污水对水稻生长发育的影响比施污泥灌清水的影响大些,因此,施用含重金属污泥时,最好不要超过5000斤／亩。大田和室内模拟试验证明：重金属从土壤中迁移到植物,由植物带走输出的量极少,其中以带走输出的Hg、Cd,As相对较多,带走输出的Pb、Cr相对的少些。     

轮作制度对水稻生长季节稻田氧化亚氮排放的影响

通过盆栽试验(3次重复),研究了3种主要轮作制度对稻田水稻生长季节N₂O排放的影响。结果表明,在水稻-小麦轮作中,水稻生长季节稻田N₂O-N的排放量为4．2kg·hm^-2,显著大于双季稻-小麦轮作中早稻的排放量2．2kg·hm^-2;但两者的季节平均排放通量无明显差异,分别为117和118μg·m^-2·h^-1。同时,两者都显著大于双季稻-小麦中的晚稻和持续淹水体系中的水稻生长季节稻田N20的平均排放通量,分别为67．0和42．1μg·m^-2·h^-1,在前作为旱作小麦的2种水稻生长季节中,大于91％的稻田N2O排放量都集中在水稻生长前半期;在前作为水稻的晚稻生长季节中,稻田N₂O排放量的91％集中在中期烤田及收获前水分落干阶段,轮作制度和前作水分状况极大地影响稻田N2O的排放。     

Soil mercury accumulation and transference to different crop grains

Mercury contamination in agro-ecosystems is one of the most important environmental issues. Farmland soil mercury accumulation and transference to crops in Changshu City, eastern China, were investigated to identify mercury migration capacity from soil to crops. The mean content of mercury for soil samples slightly increased year after year. The mercury accumulation capacity of rice grown (bioaccumulation factor (BAF) 0.028) in submerged soils under reductive conditions was stronger than that of wheat (BAF 0.0073) in dried soils under oxidative conditions. There were clear relationships between soil mercury with organic matter (OM), cation exchange capacity (CEC), and CaCO₃ of soil samples, while apparent negative relationships between Hg in rice grain with OM, CEC, and CaCO₃ of soil existed. No clear association for Hg between crops and soil was found, indicating that mercury in crop grains is mostly affected by other factors besides soil mercury. Also, soil properties and farming patterns affected mercury transference from soil to crop grains and mercury enrichment capacity in crop grains. The results suggested that appropriate selection of crop species and water management are two major possible ways to reduce total mercury accumulation in crop grains grown in mercury-contaminated regions.     

Relationships Between Metal Concentrations in Human Hair and in Soil,Road Dust,and Rice

The relationships between metal contents in soil, road dust, and rice, and in human hair from a rural area of China were observed for Cr, Cu, Mn, Ni, Pb, and Zn. The results showed that the mean concentrations of Mn in human hair were higher than the highest reference value. The concentrations of Cr, Cu, Ni, and Zn in soil and road dust were usually higher than their background values. The enrichment factors indicated that the determined metals in soil and road dust were usually derived from natural sources. Chromium, Pb, and Zn in soils and road dusts from several sites were slightly influenced by anthropogenic sources. The regression analyses showed that positive relationships usually exist between the concentrations of the determined metals in rice and in human hair as well as in soil and in human hair. However, relationships between metal concentrations in road dust and in human hair were less obvious. The study demonstrated that human hair was an applicable biomonitor of metal concentrations in rice, soil, and road dust from a rural area in China. Metal concentrations in local human hair could be used to predict contamination levels of metals in rice and soil.     

Phosphorus cycling in rainfed lowland rice ecosystems on sandy soils

Phosphorus cycling in rainfed lowland rice ecosystems is poorly understood. Soil drying and grazing of rice straw during the long dry season, the growth of volunteer pastures during the early wet season, and intermittent loss of soil-water saturation while the rice crop is growing are important distinguishing characteristics of the rainfed lowlands in relation to P cycling. We studied P cycling in an acid sandy rainfed lowland soil that covers about 30% of the rice growing area of Cambodia. Soils with similar properties in comparable rainfed sub- ecosystems occur in Laos and northeast Thailand. We developed a general schema of P pools and fluxes in the crop and soil for rice-based cropping systems in the rainfed lowlands of Cambodia. The schema was derived from a number of field experiments carried out over five consecutive cropping seasons to quantify the residual value of P fertiliser, P mass balances, soil P fractions, the effect on subsequent rice crops of crop residues and volunteer pastures incorporated into the soils, and the dynamics of P turnover in the soil. With a single rice crop yielding 2.5–3 t ha⁻¹, application of 8–10 kg P ha⁻¹ maintained yields and a small positive P balance in the soil. However, the soil P balance was sensitive to the proportion of rice straw returned to the soil. Volunteer pastures growing during the early wet season accumulated significant amounts of P, and increased their P uptake when soils were previously fertilised with P. These pastures recycled 3–10 kg P ha⁻¹ for the succeeding rice crops. While inorganic soil P pools extractable with ion exchange resins and 0.1 M NaOH appeared to be the main source of P absorbed by rice, microbial and organically-bound P pools responded dynamically to variation in soil water regimes of the main wet, dry and early wet seasons. The schema needs to be developed further to incorporate site-specific conditions and management factors that directly or indirectly affect P cycling, especially loss of soil-water saturation during the rice cropping cycle. The paper discusses the application of results for acid sandy soils to other significant rice soils in the rainfed lowlands of southeast Asia.     

贵州万山汞矿区污染土壤中汞的形态分布特征

利用优化Tessier连续化学浸提法对贵州万山汞矿区污染土壤中汞的形态分布进行研究.结果表明,稻田土壤中汞主要以残渣态形式存在(79.65%),其次为有机结合态(19.97%)、氧化态(0.31%)、特殊吸附态(0.04%)和溶解态与可交换态(0.03%);除特殊吸附态外,其他各形态汞含量均随距污染源距离增加而降低,特殊吸附态汞在分析土壤中含量变化不明显;生物可利用性(溶解态与可交换态和特殊吸附态)汞占总汞比例较低,但在污染土壤中其含量明显高于未受污染地区.     

温度和CO2浓度升高下转Bt水稻种植对土壤活性碳氮和线虫群落的短期影响

全球气候变化下转Bt水稻种植对土壤生态系统的影响仍是未知领域。利用野外开顶式气室(OTC)模拟气候变化,探讨了温度和CO2浓度([CO2])升高后种植转Bt(华恢1号)水稻对土壤活性碳氮和线虫群落的影响。结果表明:(1)温度和[CO2]升高条件下种植转Bt水稻显著影响土壤可溶性碳(DOC)、可溶性氮(DON)和硝态氮(NO-3-N)含量,同时DOC和DON受到升温和[CO2]升高与转Bt水稻的交互影响;在正常温度和[CO2]下,转Bt水稻显著降低了土壤微生物量碳氮含量(MBC、MBN),但在温度和[CO2]升高后转Bt水稻种植使土壤MBC和MBN含量显著高于亲本水稻。(2)在温度和[CO2]升高条件下,转Bt水稻土壤线虫总数呈高于亲本水稻的趋势,植食性线虫的比例随[CO2]和温度升高呈增大的趋势。此外,升温和转Bt水稻种植提高了土壤线虫群落的能流通道指数,而[CO2]升高和转Bt水稻种植则提高了土壤线虫群落的富集指数。总之,在模拟全球气候变化下,种植转Bt水稻在短期内对土壤活性碳氮和线虫群落均产生影响,但短期研究并未发现转Bt水稻种植对土壤生态系统的不利影响。     

腐殖质、硫、氯化钠对水稻积累汞的影响试验研究

汞是环境中主要重金属污染物之一。国内外在研究汞在水生环境的迁移转化规律及其基质方面进行了大量的工作,但汞在陆生环境中的迁移转化,尤其是土壤—植物系统中影响汞吸收的机制方面研究得较少。近年来,国外对影响土壤吸收汞的机制的研究工作,认为土壤酸碱度、氧化还原电位是影响土壤、生物吸收重金属的主要因素,环境中无机配位体和有机     

Iron toxicity to rice in an acid sulfate soil as influenced by water regimes

Summary The effects of two water regimes: Continuous flooding and flooding with soil drying on iron toxicity to rice in an acid sulfate soil was studied by continuously growing 7 crops of IR-32 rice in pots under the two water treatments. There was no plant growth upto the second crop under both water treatments due to iron toxicity. But there was good growth of rice under the continuous water regime from third cropping onwards, however, there was no growth of rice in the flooding with soil drying treatment even upto the seventh crop due to iron toxicity.The results of the study bring out that keeping an acid sulfate soil flooded for a few weeks and then planting rice when iron in soil solution has dropped below toxicity level may be a possible management practice for lowland rice culture on such soils. Drying and reflooding an acid sulfate soil on the other hand aggravates soil acidity and keeps iron in solution in high amounts to be toxic to rice plant.     

新疆棉田土壤质量综合评价方法

以新疆主要棉区为研究对象,测定了哈密、博乐、昌吉、奎屯、石河子、阿克苏及喀什棉田土壤耕层的pH、盐分、有机质、全氮、速效磷、速效钾及Cr、Cu、Zn、As、Pb 共计11个指标,综合分析土壤理化性质和重金属含量,采用土壤质量综合指数(SQI)对新疆主要棉区棉田土壤质量进行综合评价.结果表明: 新疆棉区棉田土壤呈碱性,pH均值为7.87,盐分含量均值为3.44 g·kg^-1,为轻度盐化土壤,有机质和全氮含量均偏低,速效磷、速效钾含量较为丰富,与第二次全国土壤普查数据相比,土壤pH、盐分含量、有机质和全氮均呈下降趋势,土壤速效磷明显增长,部分地区土壤速效钾呈现出不同程度的升高趋势;Cr、Cu、Zn、As、Pb 5种重金属含量分别为45.88、40.66、68.30、12.88、16.68 mg·kg^-1,均未超过国家二级标准,但与新疆土壤元素背景值相比,Cu、Zn、As均有累积现象.当重金属内梅罗综合污染指数(PN)小于0.5时,土壤理化性质越好,土壤综合质量越好.土壤有机质、全氮、Cu、Zn和As是影响新疆棉区棉田土壤质量的重要因素.新疆棉区棉田土壤质量总体属于中等水平,昌吉、奎屯质量最高,SQI为0.52,阿克苏质量最低,SQI为0.31,不同棉区土壤质量呈现为:北疆>东疆>南疆.     

The potential of cropping systems and soil amendments for carbon sequestration in soils under long-term experiments in subtropical India

An understanding of the dynamics of carbon (C) stock in soils, as impacted by management strategies, is necessary to identify the pathways of C sequestration in soils and for maintaining soil organic C (SOC) at a level critical for upkeeping soil health and also for restraining global warming. This is more important in tropical and subtropical region where soils are inherently low in organic C content and the production system is fragile. We evaluated the long‐term role of crop residue C inputs to soil in SOC sequestration and also the critical value of C inputs for maintenance of SOC across five different rice‐based cropping systems and four soil management practices including a fallow (no cultivation since initiation of the experiments) using five long‐term (7–36 years) fertility experiments in subtropical India. Cropping per se always caused a net depletion of SOC. Such depletion was inversely proportional to the amount of crop residue C incorporated into the soils (r=−0.92, P=0.001). Balanced fertilization with NPK, however, caused an enrichment (9.3–51.8% over the control) of SOC, its extent being influenced by the cropping systems. Long‐term application of organic amendments (5–10 Mg ha⁻¹ yr⁻¹) through farmyard manure (FYM) or compost could increase SOC hardly by 10.7% constituting only 18% of the applied C, the rest getting lost through oxidation. The total quantity of soil C sequestered varied from −11.5 to 14.5 Mg C ha⁻¹ and was linearly related (r²=0.40, P=0.005) with cumulative crop residue C inputs to the soils. On an average, the rate of its conversion to SOC came out to be 6.4%. This was more in presence of added organics (6.9%) than in its absence (4.2%). For sustenance of SOC level (zero change due to cropping) we found that a minimum quantity of 2.9 Mg C is required to be added per hectare per annum as inputs. The cropping systems and the management practices that could provide C input higher than the above critical level are likely to sustain the SOC level and maintain good soil health in the subtropical regions of the Indian subcontinent.     

不同稻作制对红壤性水稻土中锰剖面分布的影响

为了探讨红壤性水稻土锰的迁移和转化行为,通过长达16a的定位试验研究了不同稻作制、有机肥以及地下水位对土壤剖面中全锰、活性锰和交换态锰分布的影响。试验结果表明,长期淹水种稻引起0-20cm土壤层次全锰、活性锰和交换态锰含量的显著下降,而在20－40cm和40－75cm土层相对累积。不同稻作制比较,0－20cm土层中全锰、活性锰和交换态锰含量以稻稻泡显著高于稻稻绿和稻稻油处理,而20－40cm和40－75cm土层3种锰形态的含量各稻作制之间无显著差异,表明实行水旱轮作的稻稻绿与稻稻油两种稻作制耕层土壤锰的淋溶损失比持续淹水的稻稻泡制更为严重。相对而言,不同有机肥施用水平和地下水位对土壤剖面中锰分布的影响要小于稻作制,总的趋势为：土壤剖面中锰的空间分异程度以高量有机肥＞常量有机肥＞单施化肥;低水位＞高水位。从土壤中锰的空间分布规律可以看出,水旱轮作（尤其是在低水位和有机无机配合的条件下）比长期淹水更有利于土壤锰氧化还原引起的深层淋溶与淀积,加速了典型水稻土剖面的形成。     

Changes in soil carbon sequestration and soil respiration following afforestation on paddy fields in north subtropical China

Aims Although many studies have reported net gains of soil organic carbon (SOC) after afforestation on croplands, this is uncertain for Chinese paddy rice croplands. Here, we aimed to evaluate the effects of afforestation of paddy rice croplands on SOC sequestration and soil respiration (R s). Such knowledge would improve our understanding of the effectiveness of various land use options on greenhouse gas mitigation in China.Methods The investigation was conducted on the Chongming Island, north subtropical China. Field sites were reclaimed from coastal salt marshes in the 1960s, and soils were homogeneous with simple land use histories. SOC stocks and R s levels were monitored over one year in a paddy rice cropland, an evergreen and a deciduous broad-leaved plantation established on previous paddy fields and a reference fallow land site never cultivated. Laboratory incubation of soil under fast-changing temperatures was used to compare the temperature sensitivity (Q 10) of SOC decomposition across land uses.Important findings After 15–20 years of afforestation on paddy fields, SOC concentration only slightly increased at the depth of 0–5cm but decreased in deeper layers, which resulted in a net loss of SOC stock in the top 40cm. Seasonal increase of SOC was observed during the rice-growing period in croplands but not in afforested soils, suggesting a stronger SOC sequestration by paddy rice cropping. However, SOC sequestered under cropping was more labile, as indicated by its higher contents of dissolved organic carbon and microbial biomass. Also, paddy soils had higher annual R s than afforested soils; R s abruptly increased after paddy fields were drained and plowed and remained distinctively high throughout the dry farming period. Laboratory incubation revealed that paddy soils had a much higher Q 10 of SOC decomposition than afforested soils. Given that temperature was the primary controller of R s in this region, it was concluded that despite the stronger SOC sequestration by paddy rice cropping, its SOC was less stable than in afforested systems and might be more easily released into the atmosphere under global warming.     

Alleviating soil sickness caused by aerobic monocropping: responses of aerobic rice to soil oven-heating

“Aerobic rice” system is the cultivation of nutrient-responsive cultivars in nonflooded and nonsaturated soil under supplemental irrigation. It is intended for lowland areas with water shortage and for favorable upland areas with access to supplementary irrigation. Yield decline caused by soil sickness has been reported with continuous monocropping of aerobic rice grown under nonflooded conditions. The objective of this study was to determine the growth response of rice plant to oven heating of soil with a monocropping history of aerobic rice. A series of pot experiments was conducted with soils from fields where rice has been grown continuously under aerobic or anaerobic (flooded) conditions. Soil was oven heated at different temperatures and for various durations. Plants of Apo, an upland variety that does relatively well under the aerobic conditions of lowland, were grown aerobically without fertilizer inputs in all six experiments. Plants were sampled during vegetative stage to determine stem number, plant height, leaf area, and total biomass. Heating of soil increased plant growth greatly in soils with an aerobic history but a relatively small increase was observed in soils with a flooded history as these plants nearly reached optimum growth. A growth increase with continuous aerobic soil was already observed with heating at 90°C for 12 h and at 120°C for as short as 3 h. Maximum plant growth response was observed with heating at 120°C for 12 h. Leaf area was most sensitive to soil heating, followed by total biomass and stem number. We conclude that soil heating provides a simple and quick test to determine whether a soil has any sign of sickness that is caused by continuous cropping of aerobic rice.     

新疆焉耆盆地辣椒地土壤重金属污染及生态风险预警

从新疆加工辣椒主产地(焉耆盆地)采集105个辣椒地典型土壤样品,测定其中As、Cd、Cr、Cu、Mn、Ni、Pb和Zn等8种重金属元素的含量。采用污染负荷指数(Pollution load index,PLI)、潜在生态风险指数(Potential ecological risk index,RI)和生态风险预警指数(Ecological risk warning index,I_(ER))对辣椒地土壤重金属污染及生态风险进行评价。结果表明:(1)焉耆盆地辣椒地土壤Cd、Cr、Ni、Pb和Zn含量的平均值分别超出新疆灌耕土背景值的1.65、1.40、1.32、3.21、6.42倍。辣椒地土壤Pb和Zn呈现重度污染,Cd、Cr和Ni轻度污染,As、Mn和Cu无污染。(2)土壤PLI平均值为1.40,呈现轻度污染。各重金属元素单项生态风险指数从大到小依次为:Cd、Ni、As、Cu、Pb、Cr、Zn。土壤RI平均值为18.40,属于轻微生态风险态势,IER平均值为-4.78,属于无警态势;博湖县辣椒地污染水平、潜在生态风险程度与生态风险预警等级最高,焉耆县污染水平、潜在生态风险程度与生态风险预警等级最低。(3)辣椒地土壤As、Cd、Pb与Zn主要受到人类活动的影响,Cr、Cu、Mn和Ni主要受到土壤地球化学作用的控制。Cd是焉耆盆地辣椒地生态风险等级最高的重金属元素,研究区农业生产过程中要防范Cd的污染风险。     

Loss of Nitrogen,Phosphorus, and Potassium Through Crop Harvests in Agroecosystems of Qianjiang,Hubei Province,PR China

The level of chemical fertilization in China is considerably higher than that normally applied in Western countries. For example, in the last decade the use of N-P-K chemical fertilizers increased, within the province of our study, from about 300 kg/ha in 1980 to about 850 kg/ha in 1990. Data on total amounts on nitrogen, phosphorus, and potassium that are removed with the harvest are necessary in determining and optimizing the amount of chemical fertilizers to be applied to different crops and in different cropping patterns. In this article we report the results of analyses of N, P, and K content of soils and different parts of different plants (soybean, cotton, rice, peanut, radish, Chinese cabbage, sesame, pepper, eggplant, and ambary) typically grown in rural areas of Southern China and provide an estimate of the balance of these nutrients under the five cropping systems that are dominant in the studied area.     

海南稻田土壤硒与重金属的含量、分布及其安全性

采集了海南省18个市(县)代表性的稻田土壤耕作层(0—20cm)样品280个,研究了硒(Se)和5种有毒重金属元素(Hg、Cd、Cr、Pb和As)的含量、分布及其相关关系,并对Se和重金属的安全性进行评价,可为合理区划清洁且富Se稻田提供理论依据。结果表明:海南稻田土壤中Hg、Cd、Cr、Pb和As平均含量均低于国家土壤环境质量一级标准值和全国土壤背景值,以绿色食品产地环境技术条件限量标准为标准,用单项污染指数法和内梅罗综合污染指数法评价海南稻田土壤重金属的污染状况,结果都是清洁的。但以海南省土壤背景值做参比值,Hakanson潜在生态危害指数达到211.54,属于强生态危害,从潜在生态危害系数来看,Hg(102.61)和Cd(98.89)达到强生态危害,分别比海南省土壤背景值增加1.56和2.3倍,今后应注意控制Hg和Cd污染源。稻田土壤Se含量从痕量到1.532mg/kg之间,平均值为0.211mg/kg,占47.5%的稻田土壤Se含量处于中等及以上水平(>0.175mg/kg)。Se含量高的稻田土壤主要集中在东北部的海口及其周边的澄迈、定安、文昌和琼海,还有东南部的万宁和保亭。由于重金属平均含量还比较低,可暂时忽略重金属污染,故可在上述Se含量高的稻田土壤上种植富Se水稻。稻田土壤Se含量与Hg、Cd和As含量呈极显著或显著正相关,因此今后应加强研究稻田土壤Se与Hg、Cd和As的有效性及其相互作用,以便生产出绿色的富Se优质大米。     

Long fallow periods: The key to sustenance of soil fertility?

Changes in N, P, K, Ca and Mg in soil and rice plants were investigated during a cropping season following a long fallow period in a system of traditional cultivation practised for several centuries, under a village tank irrigation system. Soil, N, P, K, Ca and Mg were not found to be deficient for rice production throughout the season. Flooding did not produce toxic levels of Fe and Na and soil pH remained at 6.4 during the season. The average grain yield (3.5 t/ha) without any addition of chemical fertilizer was almost the same as that from fields under major irrigation systems where fertilizer application (less than the recommended level) was common. The sustainability of soil fertility under the traditional system of rice cultivation appears to be dependent upon long fallow periods. The natural build-up of soil fertility during a three-year fallow was evidently adequate to support a good growth of the crop which produced a yield comparable to that obtained in chemically fertilized, more intensively cropped rice fields under major irrigation systems.