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1.

Purpose

Previous studies in the Mezquital Valley evidenced that irrigation with untreated sewage effluent supplies two- to tenfold larger nitrogen doses to crops than common fertilizer recommendations. However, nitrate concentrations in the groundwater are only slightly above threshold concentrations for drinking water. To understand the N dynamics in this agroecosystem, we quantified nitrogen inputs, outputs, and transformations within the rooting zone and in the vadose zone down to the aquifer (i.e., in the critical zone).

Materials and methods

Single irrigation events were monitored in three different fields cropped with either annual rye grass (Lolium rigidum) or oats (Avena sativa L.) harvested for fodder. For each irrigation event, the total amount of water entering and leaving the field was quantified with a flowmeter. Soil pore water was collected with either microsuction cups or observation wells and groundwater was sampled at two wells. All water samples were analyzed for total nitrogen (Nt), ammonium nitrogen (NH4 +–N), nitrate nitrogen (NO3 ?–N), chloride (Cl?1), and pH. Organic N was calculated as the difference between total N and inorganic N. The water tension and the soil water content were monitored before, during, and after the irrigation with tensiometers and TDR probes, respectively, installed at different depths and at three sites within each field. Batch experiments were conducted to assess the NH4 + adsorption capacity of the soils.

Results and discussion

The irrigations added 537 to 727 kg ha?1 N in form of organic N (40 %) and NH4 +–N (60 %) to the fields. Crops absorbed 65 % of the N and 31 to 66 kg NO3 ?–N ha?1 leached out beyond the rooting zone (>40 to 130 cm). Batch experiments evidenced an ammonium adsorption capacity of 43 and 53 % of the input ammonium mass. Nitrification dominated over denitrification as the water infiltrated through the soil, evidenced by changes in nitrate concentrations and pH values in the soil pore water. The behavior of the total N/Cl ratio with depth indicated possible N losses due to NH3 volatilization at the field surface, a temporal withdrawal of N from the soil solution due to NH4 +–N adsorption in the rooting zone, as well as probable denitrification losses in the vadose zone.

Conclusions

Although the studied agroecosystem muses the large N inputs relative efficiently, between 7 and 10 % of the added N with each irrigation leaches beyond the crop root zone as nitrate. This is triggered by overflow irrigation, since up to 8,699,000 L of water with N concentrations of up to 50 mg total N L?1 infiltrate rapidly through macropores beyond the rooting zone. Additionally, ammonia volatilization and denitrification seem to be occurring. The latter could provide a self-cleaning potential to the system, if it reaches N2 and needs further verification. Nevertheless, N inputs to the system should match crop uptake to avoid groundwater and atmospheric pollution.
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2.
华北平原农田生态系统服务评价及灌溉效益分析   总被引：3，自引：1，他引：2  
农田生态系统为人类提供农产品等服务的同时,对生态环境也产生负面影响。本文基于千年生态系统评估(MA)框架,以华北平原典型高产农田区域——河北省石家庄市栾城区为研究对象,应用能值理论分析农田生态系统投入,从供给、调节和支持3方面分析农田生态系统正、负服务产出;应用分摊系数法求解农田灌溉净效益,计算能值指标并评价农田生态系统可持续发展状况。结果表明:研究期间栾城农田生态系统能值年均总投入(1.00×1012 sej·m~(-2))中,不可更新工业辅助能(6.81×1011 sej·m~(-2))与不可更新环境资源(灌溉用地下水,2.57×1011 sej·m~(-2))投入之和占总能值投入的90%以上,说明农田生态系统消耗了大量不可更新资源;农田提供的正服务(1.82×1012 sej·m~(-2))主要是农产品供给(1.07×1012 sej·m~(-2)),负服务(5.87×1011 sej·m~(-2))以温室气体排放(5.31×1011 sej·m~(-2))为主;考虑农田生态系统环境负效益,计算栾城农田灌溉效益分摊系数为0.32,灌溉净效益为3.94×1011 sej·m~(-2),灌溉效益偏低;栾城区能值可持续发展指标取值为0.10~0.18,属于典型的消费型农田生态系统,迫切需要探索出一条低能耗,高产出的真正意义上的高质量农田发展之路,实现农田生态系统健康可持续发展。  相似文献   

3.
In this research, radiation use efficiency (RUE) of winter wheat was determined under different irrigation regimes and nitrogen application rates in experimental field at southwest Iran (semi-arid region) in 2009–2010 and 2010–2011. The experiment was laid out as a split plot design, with irrigation treatments as main plots and N fertilization as sub-plots with three replications. Irrigation treatments were 1.2 (I4), 1.0 (I3), 0.8 (I2), and 0.5 (I1) times of the full irrigation requirements and N treatments were 0 (N1), 46 (N2), 92 (N3), and 136 (N4) kg ha?1. Air temperature had significant effects on RUE that was adjusted by multiplication of hourly temperature factor to the hourly values of solar radiation (RUE a ). The values of RUE a were significantly different from the values of RUE in both growing seasons. The values of RUE a ranged from 1.44 to 1.83 g MJ?1 and 1.45 to 1.81 g MJ?1 in 2009–2010 and 2010–2011, respectively. In both growing seasons, minimum and maximum values of RUE were at I1N1 and I4N4 treatments, respectively. The methods of daily maximum and minimum air temperature were modified for considering the effects of air temperature on RUE at locations where hourly air temperature and radiation were not available.  相似文献   

4.
针对蔬菜灌溉水肥渗漏问题,采用田间试验和室内分析相结合,研究了番茄膜下沟灌灌水量与土壤硝态氮的根层外渗漏关系,分析了灌水量与不同根层土壤硝态氮的淋溶和保蓄特征,结果表明:灌溉不施肥条件下灌水量与土壤硝态氮淋溶量和淋溶率、灌溉施肥条件下灌水量与土壤施入硝态氮的保蓄率和渗漏率均呈直线关系;灌溉均会引起浅根层(0—20 cm)硝态氮淋溶,灌溉施肥条件下7.5～15 mm灌水量范围硝态氮积累有一个峰值,而22.5～45 mm范围则有两个峰值;灌水量在7.5～15mm之间,灌溉不施肥条件下根层土壤硝态氮淋溶率为0,灌溉施肥条件下土壤硝态氮渗漏率为0～5.19%;灌水量在22.5～45 mm之间,灌溉不施肥土壤硝态氮淋溶率为5.38%～19.08%,灌溉施肥条件下根层土壤硝态氮渗漏率为21.91%～61.96%。日光温室番茄膜下沟灌能减少肥料淋溶与渗漏的节水灌水量为15 mm。  相似文献   

5.
To evaluate the effect of groundwater irrigation on the polycyclic aromatic hydrocarbons(PAHs) pollution abatement and soil microbial characteristics,a case study was performed in the Shenfu irrigation area of Shenyang,Northeast China,where the irrigation with petroleum wastewater had lasted for more than fifty years,and then groundwater irrigation instead of wastewater irrigation was applied due to the gradually serious PAHs pollution in soil.Soil chemical properties,including PAHs and nutrients contents,and soil microbial characteristics,including microbial biomass carbon,substrateinduced respiration,microbial quotient(qM),metabolic quotient(qCO2),dehydrogenase(DH),polyphenol oxidase(PO),urease(UR) and cellulase(CE) in surface and subsurface were determined.Total organic C,total N,total P,and available K were significantly different between the sites studied.The PAHs concentrations ranged from 610.9 to 6362.8 μg kg-1 in the surface layers(0-20 cm) and from 404.6 to 4318.5 μg kg-1 in the subsurface layers(20-40 cm).From the principal component analysis,the first principal component was primarily weighed by total PAHs,total organic C,total N,total P and available K,and it was the main factor that influencing the soil microbial characteristics.Among the tested microbial characteristics,DH,PO,UR,CE,qM and qCO2 were more sensitive to the PAHs stress than the others,thus they could serve as useful ecological assessment indicators for soil PAHs pollution.  相似文献   

6.
控制性根系分区交替灌溉对冬小麦水分与养分利用的影响   总被引：25，自引：6，他引：19  
以移栽小麦为试验材料,采用盆栽的方法研究了3种不同灌水方式：全面积均匀灌水(对照)、控制1/2区域交替灌水(CRDI)和控制固定1/2区域灌水对冬小麦水分与养分利用的影响。研究结果表明：在同一灌水方式中土壤含水率下限小的冬小麦根冠比大,且根系总的干重也大;CRDI对根系生长有显著促进作用,使根均匀分布在土壤中,且根长密度较对照大;对于CRDI,当控制土壤含水率下限由65％θF变化为55％θF时,耗水量下降了35％,节水效果明显;土壤含水率较高,有利于冬小麦根系对土壤中离子态养分的吸收;土壤含水率下限相同时,3种不同的灌水方式中,土壤中H2PO-4和NH+4-N离子浓度均呈现出递减的趋势,而NO-3-N离子浓度却呈现出明显的递增趋势,在同一土壤含水率下,CRDI对养分离子的吸收优于其它两种灌水方式。  相似文献   

7.
Extensive use of chemical fertilizers in agriculture can induce high concentration of ammonium nitrogen(NH4+-N) in soil. Desorption and leaching of NH4+-N has led to pollution of natural waters. The adsorption of NH4+-N in soil plays an important role in the fate of the NH4+-N. Understanding the adsorption characteristics of NH4+-N is necessary to ascertain and predict its fate in the soil-water environment, and pedotransfer functions(PTFs) could be a convenient method for quantification of the adsorption parameters. Ammonium nitrogen adsorption capacity, isotherms, and their influencing factors were investigated for various soils in an irrigation district of the North China Plain. Fourteen agricultural soils with three types of texture(silt, silty loam, and sandy loam) were collected from topsoil to perform batch experiments. Silt and silty loam soils had higher NH4+-N adsorption capacity than sandy loam soils.Clay and silt contents significantly affected the adsorption capacity of NH4+-N in the different soils. The adsorption isotherms of NH4+-N in the 14 soils fit well using the Freundlich, Langmuir, and Temkin models. The models’ adsorption parameters were significantly related to soil properties including clay,silt, and organic carbon contents and Fe2+ and Fe3+ ion concentrations in the groundwater. The PTFs that relate soil and groundwater properties to soil NH4+-N adsorption isotherms were derived using multiple regressions where the coefficients were predicted using the Bayesian method. The PTFs of the three adsorption isotherm models were successfully verified and could be useful tools to help predict NH4+-N adsorption at a regional scale in irrigation districts.  相似文献   

8.
本文通过对华北平原典型再生水灌溉区(河北省石家庄洨河流域)的包气带土壤、地表水和地下水进行采样分析,对硝酸盐在多种环境介质中的来源与环境行为进行了研究,识别了再生水灌溉区地下水硝酸盐污染来源,明确了不同灌溉条件对包气带土壤中硝酸盐迁移的影响。在受到城市再生水严重影响的洨河流域,地下水中的硝酸盐浓度分布范围在4.0 mg·L?1到156.6 mg·L?1之间,已经形成了距离河道2 km、深度70 m的硝酸盐高值区域,经过计算硝酸盐的垂向扩散速率为每年1～2 m。硝酸盐与氯离子的相关性表明,城市再生水是再生水灌溉区包气带、地表水和地下水中硝酸盐的主要来源。利用Geoprobe获取利用不同灌溉水农田土壤剖面样品,研究再生水对厚包气带NO3?-N垂向分布影响,再生水灌溉区和地下水灌溉区中包气带土壤的NO3?-N的平均含量为137.0 mg·kg-1和107.7 mg·kg-1,最高含量523.2 mg·L?1和725.9 mg·L?1,分别出现1.20 m和0.85 m深度,分布规律有着明显的差别。包气带土壤硝酸盐与氯离子的相关性分析表明,再生水灌溉区土壤硝酸盐主要来源于城市再生水,而地下水灌溉区可能来源于农田氮肥。地下水年龄和硝酸盐之间关系表明,地下水中1975年以前补给的硝酸盐浓度低于1975年以后补给,地下水硝酸盐污染与包气带氮入渗的历史过程密切相关。在华北平原特殊的地质水文背景下,农田面源污染对地下水的影响有限,但再生水灌溉区地下水硝酸盐污染的风险较高。  相似文献   

9.
This paper focuses on N balance in a paddy field planted with whole crop rice (Oryza sativa cv. Kusahonami). The experiment was conducted with two treatments during two rice-growing seasons: one was fertilized with N (160 kg N ha–1; 16N plot) and the other unfertilized (0N plot); both plots were fertilized with P and K. The N input from precipitation was 15 and 12 kg N ha–1 in 2002 and 2003, respectively. The N input from irrigation water reached as much as 123 and 69 kg N ha–1 in 2002 and 2003, respectively. This was because irrigation water contained higher NO3– concentrations ranging from 4 to 8 mg N l–1. The N uptake by rice plants was the major output: 118 and 240 kg N ha–1 in the 0N and 16N plots in 2002 and 103 and 238 kg N ha–1 in 2003, respectively. N losses by leaching were 4.8–5.3 and 6.5–7.3 kg N ha–1 in 2002 and in 2003, respectively. Laboratory experiments were carried out to estimate the amounts of N2 fixation and denitrification. Amount of N2 fixation was 43 and 0 kg N ha–1 in the 0N and 16N plots, respectively. Denitrification potential was quite high in both the plots, and 90% of the N input through irrigation water was lost through denitrification. Collectively, the total N inputs were relatively large due to irrigation water contaminated with NO3–, but N outflow loading, expressed as leaching–(irrigation water + precipitation + fertilizer), showed large negative values, suggesting that the whole crop rice field might serve as a constructed wetland for decreasing N.  相似文献   

10.
As nitrogen (N) fertilizer-use efficiency rarely exceeds 50% in most agricultural systems, the potential leaching of N to the groundwater, particularly under irrigated conditions, has economic, health, and environmental implications. Research in the Akarsu irrigation district in the Lower Seyhan Plain in southern Turkey sought to determine spatial and temporal variability of groundwater (GW) nitrate (NO3) concentrations in 2007–2008. Shallow groundwater observation wells 3 m deep were installed at different locations to represent the whole irrigation district. Groundwater samples were collected (February, April, July, October) and analyzed for ammonium (NH4) and NO3 concentrations. Because NH4 values were negligible, only NO3 data were processed to determine spatial and temporal variability and then used to develop regional NO3 maps using geographic information systems. Groundwater NO3 concentrations ranged between 0.17 and 55.96 mg L–1 during the 2 years, only exceeding the critical 50 mg L–1 concentration in 1% of the area sampled. The areal mean of NO3 concentration was greatest in February, indicating a potential N leaching of unused N from the early season with intensive rainfall, especially in wheat-growing areas. Groundwater NO3 concentrations decreased after February; however, during the peak irrigation season in July, NO3 was relatively low because of crop uptake during spring and summer. In about half the area, groundwater NO3 concentrations ranged between 20 and 50 mg L–1 and were thus marginal relative to the critical pollution level. As N fertilizer use will continue to increase, especially with the expanded irrigation that is now occurring in the Mediterranean region, regular monitoring of groundwater NO3 is advisable under such conditions.  相似文献   

11.
华北山前平原农田土壤硝态氮淋失与调控研究   总被引：11，自引：5，他引：6  
本文依托中国科学院栾城农业生态系统试验站小麦-玉米一年两熟长期定位试验, 应用土钻取土和土壤溶液取样器取水的方法, 研究了不同农田管理措施下土壤硝态氮的累积变化, 计算了不同氮肥处理通过根系吸收层的硝态氮淋失通量。结果表明, 小麦-玉米生长季土壤硝态氮累积量和淋失量随着施氮量的增加显著增加, 相同氮肥水平下增施磷、钾肥增加了作物的收获氮量, 施磷肥增加的作物收获氮量最高可达123kg·hm-2·a-1, 施钾肥增加的作物收获氮量最高为31 kg·hm-2·a-1。不同灌溉水平下0~400 cm 土体累积硝态氮随着灌溉量的增加而降低, 控制灌溉(小麦季不灌水, 玉米季灌溉1 水)、非充分灌溉(小麦季灌溉2~3 水, 玉米季按需灌溉)、充分灌溉(小麦季灌溉4~5 水, 玉米季按需灌溉)各处理剖面累积硝态氮量分别为1 698 kg·hm-2、1148 kg·hm-2 和961 kg·hm-2。与非充分灌溉和充分灌溉处理相比, 控制灌溉在100~200 cm 土层硝态氮累积量显著高于其他层次, 2003~2005 年间控制灌溉剖面增加的硝态氮量占施肥总量的23%; 非充分灌溉处理剖面增加的硝态氮量占施肥总量的22%; 充分灌溉处理剖面增加的硝态氮量占施肥总量的47%。免耕措施降低了作物产量, 影响土壤水的运移, 增加了硝态氮的淋失风险。根据作物所需降低氮素投入(N 200 kg·hm-2·a-1), 增施磷、钾肥, 控制灌溉量是减少华北山前平原地区硝态氮淋失, 保护地下水的有效措施。  相似文献   

12.
不同灌溉处理下冬小麦水平衡与灌溉增产效率研究   总被引：6，自引：1，他引：5  
水资源是华北平原冬小麦、夏玉米种植区最重要的生产制约因素, 农业水资源高效利用具有重大的社会需要。通过设置冬小麦不同灌溉处理, 分析了各处理的水分平衡、产量和灌溉增产效率。结果显示: 1)不同灌溉处理具有不同的水分平衡过程, 雨养农田、充分灌溉处理、返青水胁迫处理、拔节抽穗水胁迫处理和灌浆水胁迫处理的蒸散量分别为251±58 mm、482±48 mm、352±44 mm、388±22 mm 和324±53 mm; 2)灌溉量对于小麦产量的增加具有明显的正效应, 拔节-抽穗水胁迫对作物产量有较大影响, 灌浆水胁迫和返青水胁迫均没有对小麦产量造成明显影响; 雨养农业的经济产量为2 950±635 kg·hm-2, 充分灌溉下的经济产量约为5 994±994 kg·hm-2; 冬小麦返青期、拔节抽穗期、灌浆期施加适度的水分胁迫, 产量分别为5 163±885kg·hm-2、5 047±1 180 kg·hm-2、5 249±975 kg·hm-2, 与充分灌溉相比, 没有明显的产量下降; 3)小麦的灌溉增产效率存在明显的年际差异, 在丰水年或特丰水年, 灌溉增产效率为1.9 kg·m-3, 在枯水年为0.4 kg·m-3, 平水年为1.6 kg·m-3。  相似文献   

13.
Intermittent irrigation is an important option for mitigating CH4 emissions from paddy fields. In order to better understand its controlling processes in CH4 emission, CH4 fluxes, CH4 production and oxidation potentials in paddy soils, and 13C-isotopic signatures of CH4 were observed in field and incubation experiments. The relative contribution of acetate to total CH4 production (fac) and fraction of CH4 oxidized (fox) in the field was also calculated using the isotopic data. At the beginning of the rice season, the theoretical ratio of acetate fermentation: H2/CO2 reduction = 2:1 was reached, however, in the late season H2/CO2-dependent methanogenesis became dominant. Compared to continuous flooding, intermittent irrigation significantly reduced CH4 production potential and slightly decreased fac-value, indicating methanogens, particularly acetate-utilizing methanogens, were inhibited. CH4 oxidation was very important, especially in paddy fields under intermittent irrigation where 19–83% of the produced CH4 was oxidized. Intermittent irrigation enhanced CH4 oxidation potential slightly and raised fox-value significantly relative to continuous flooding. Intermittent irrigation significantly decreased CH4 flux creating a more positive δ13C-value of emitted CH4 by 12–22‰. A significant negative correlation was found between CH4 fluxes and values of δ13CH4 suggesting that the less the CH4 oxidation, the higher the CH4 emission, and the lower the δ13C-value of emitted CH4. Collectively, the findings show that intermittent irrigation reduced the seasonal CH4 production potential by 45% but increased the fraction of CH4 oxidized by 45–63%, thus decreasing the seasonal CH4 emission from the paddy fields by 71%, relative to continuous flooding.  相似文献   

14.
Irrigation management has an important influence on emissions of nitrous oxide (N2O) and nitric oxide (NO) from irrigated agricultural soils. In order to develop strategies to reduce the emission of these gases, a field experiment was carried out to compare the influence of different irrigation systems: furrow (FI) and drip-irrigation (DI), on N2O and NO emissions from a soil during the melon crop season. Two fertilizer treatments were evaluated for each irrigation regime: ammonium sulphate (AS) as a mineral N fertilizer, at a rate of 175 kg N ha?1; and a control without any N fertilizer (Control). On plots where the AS treatment was applied, drip irrigation reduced total N2O and NO emissions (by 70% and 33% respectively) with respect to values for furrow irrigation. This was probably due to the lower amount of water applied and the different soil wetting pattern associated with DI. Dry areas of the drip-irrigated plots emitted a similar amount of N2O to the wet areas (0.45 kg N2O-N ha?1) in the Control and greater quantities in the AS treatment (0.92 kg N2O-N ha?1 for dry and 0.70 kg N2O-N ha?1 for wet areas). We suggest that the N oxide pulses observed throughout the irrigation period on DI plots could have been the result of frequent increases in the soil wetting volume after the addition of water. Denitrification losses (from depths of 0–10 cm) were estimated at 11.44 kg N2O- N ha?1 for the AS treatment under FI and at 4.96 kg N2O-N ha?1 for DI. Under DI, nitrification was an important source of N2O, whereas denitrification was the most important source under FI. The addition of NH4+ and the use of DI enhanced the N2O/N2 ratio of gases produced through denitrification. The quantity of dissolved organic C (DOC) in the soil generally decreased with addition of NH4+.This work showed that, in comparison with furrow irrigation, drip irrigation is a method that can be used to save water and mitigate emissions of the atmospheric pollutants NO and N2O.  相似文献   

15.
基于2000年和2005年的遥感影像,利用RS,GIS及景观生态学方法,对台兰河绿洲灌区2000-2005年的土地利用进行监测,并分析了不同时期台兰河绿洲灌区水资源开发利用程度.对研究区土地利用与水资源动态变化关系进行了分析.结果表明,2000-2005年耕地面积和水域面积年均增加分别为3 603.8 hm2和151.4 hm2;绿洲林地和草地大面积减少,减少量分别为2 247.07 hm2和14 325.9 hm2,相应地绿地面积减少了165 72.97 hm2;草地和林地等生态用地的减少是灌区耕地增加的主要来源,转移比例分别为13.97%和5.93%.地表来水量不断减少的情况下,灌区地下水开采量从1989年的5.91×106m3增加到2003年的1.39×107m3,灌溉面积和机井数量不断增大,地下水开采强度日益增加,地下水水位呈日益下降的趋势.农业用水所占比例过大,生态用水逐渐缩减.  相似文献   

16.
Vertical water fluxes at the water table and in the subsoil need to be quantified because of their significance for the supply of water to crops and the control of soil salinization in areas with shallow groundwater. A soil–water–atmosphere–plant (SWAP) model was calibrated using measured values of soil water content and the water fluxes at the water table. The measurements were taken in a field experiment where the depth to groundwater and the volume of irrigation water applied were controlled. The calibrated SWAP model was then used to simulate the soil water content and fluxes at the water table and in the subsoil under different irrigation and groundwater conditions. The predicted values provided a quantitative insight into specific terms in the water balance equation together with soil water fluxes in the subsoil that cannot be measured directly by field instruments. Crops utilized significant amounts of water from deeper soil layers and directly from groundwater, when the volume of irrigation decreased and the depth to the water table was <3.0 m. Depth to the water table significantly influenced water fluxes occurring in the soil profile over the period when evaporation dominated the hydrological cycle. Shallow groundwater is a very significant water resource for meeting the water requirement of crops. In practice, the frequency and quantity of irrigation need to be varied according to groundwater conditions.  相似文献   

17.
Shortage of water in arid and semi-arid regions increases the need of applying efficient drip irrigation system. A two-year field study in the semi-arid region of Upper Egypt was carried in randomized complete block design with four replicates. Wheat plants were irrigated by 100 or 75% of water requirements (I100 = 5,370 and I75 = 4,027 m3 ha?1). Irrigation of wheat by I100 increased growth and uptake of nitrogen, phosphorus, and potassium compared to low irrigation level. I100 caused 14 and 5% increase in straw and biological yield, respectively, compared to I75. Grain yield and water use efficiency (WUE) were higher by 20 and 59% in the case of I75 compared to I100. The use of deficit irrigation in drip-irrigated wheat under arid conditions is an effective tool to maximize efficiency of water use; moreover, 4,027 m3 ha?1 is the optimum irrigation rate for maximum WUE and grain yield.  相似文献   

18.
Abstract

In the course of a series of studies conducted to investigate the long-term behavior of 129I (which has a half-life of 16 million years) in the environment, seasonal variation in the concentration of stable iodine (127I) in precipitation and soil water to a depth of 2.5 m in a forest plot, an upland field and a paddy field in the upland area of Tsukuba, Japan, were determined. Iodine concentration in precipitation tended to increase during the summer (high air temperature) season and low-rainfall period, and a positive high correlation was observed between annual rainfall and the annual amount of iodine supplied by precipitation. No seasonal variations in iodine concentration in soil water were observed at any depth in the forest plot and upland field unlike at shallow depths (0.2 and 0.5 m) in the paddy field. In the paddy field, from the beginning of summer irrigation, under flooding conditions, iodine concentration in soil water at shallow depths (0.2 and 0.5 m) continuously increased, and immediately before mid-summer (intermittent) drainage and drainage, the maximum iodine concentration (approximately 50 µg L?1) and lowest Eh values (approximately ?150 to ?200 mV) were recorded. These high iodine concentration levels and low Eh values were ascribed to high air temperature (approximately > 25°C on average every 10 days) and the continuation of the groundwater level above the ground surface. As for the temporary winter irrigation period (mean daily air temperature 2?4°C), the iodine concentration was low (1.7–3.7 µg L?1) at all depths, as was the case in the non-irrigation period. After mid-summer drainage, and drainage, the iodine concentration in soil water at depths of 0.2 and 0.5 m decreased drastically as the groundwater level decreased. The mean annual amount of iodine accumulated in the surface soil horizons (0–0.67 m) in the forest plot was estimated to be approximately 2.9 mg m?2 (7.5 µg kg?1 dry soil), which coincided with the mean annual amount of iodine supplied to the earth surface by precipitation. A mildly oxidative subsurface 2Bw horizon (0.60–0.89 m) in the paddy field was estimated to illuviate approximately 3.1 mg m?2 (20 µg kg?1 dry soil) of iodine annually by retaining iodine in the soil water percolated to this horizon.  相似文献   

19.
Nitrogen fertilization management under water limited conditions needs to be refined to save environmental ecosystems and increase economic returns. Two-year field studies in a split-plot design were conducted to investigate the response of maize to different nitrogen rates (N100 = 100, N130 = 130, and N160 = 160?kg N ha?1) under two irrigation levels (100 or 75% of water requirements). Under deficit irrigation, water and N were used more efficiently than normal water supply. N-fertilization of drip irrigated maize grown under deficit irrigation with N160 increased the uptake of N, P and K by 35, 29 and 70% compared with N100. Fertilization of maize grown under deficit irrigation with N160 increased the grain, straw and biological yield and water use efficiency by 50, 14, 22 and 33% compared with N100. Based on the obtained results, 160?kg of N ha?1 is the optimum rate of N for maize irrigated by 75% of water requirements.  相似文献   

20.
Studies were conducted on the effects of waters of different quality on the chemical characteristics of 74 surface and subsurface soils of the Nagaur district, Rajasthan. The electrical conductivity (EC) of the saturation extract of these sandy and loamy sand soils were found to be less than that of the irrigation water. Correlations were observed between EC and the constituent ions (Na+, Ca2+ and Mg2+ of the irrigation water and of the saturation extract of the soil samples. The pH values of the irrigation water and soil suspensions also showed a positive correlation. The carbonate and bicarbonate ion concentrations in both the irrigation water and the saturation extract of the soils correlated with their respective pH values. EC of both the irrigation water and the saturation extract from surface and subsurface soil layers correlated with total cations. Correlations between the chemical characteristics of the irrigation water and the saturation extract of the soils are of limited value for prediction purposes, due to other factors operating under field conditions.  相似文献   

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