扬州沿运灌区暗管排水土工布外包滤料的水力性能试验研究

农田暗管排水系统建设是提高农业机械化作业效率的有效措施之一.土工布作为排水暗管外包滤料时,需要具有良好的透水性能和抗淤堵能力.文中以扬州段沿运灌区为例,针对当地土壤中粉粒含量较高,土工布外包滤料筛选困难等实际问题,参考相关技术准则,选用2种开孔率和厚度不同的土工布进行了水力渗透试验,并与传统的河砂反滤材料进行了对比,筛选出适合当地土壤的土工布外包材料.研究结果显示,所选用的2种土工布透水性能存在较大差异,其中厚度较大(0.41 mm)、孔径较小(180 μm)的土工布A的透水性能较好,渗透系数为初始值的54.1%,高于河砂滤层的46.1%,而厚度为0.35 mm、孔径为227 μm的土工布B渗透系数仅为初始值的30.2%.相比于土工布B,土工布A具有更好的抗淤堵能力,长期使用后淤堵率比土工布B低16%.通过对土工布表面形成的、透水性较低的滤饼分析发现,土工布B不但自身发生了较大程度淤堵,其表面形成的滤饼较为密实,是影响其渗透性能的直接原因.     

Research and developments in selecting subsurface drainage materials

Subsurface drainage requires appropriate materials to ensure a proper functioning of the drainage system. The materials normally applied for subsurface drainage are drain pipes and envelopes. Besides a review of the materials used for drain pipes, their hydraulic characteristics — discharge capacity and entrance resistance — have been treated. Much attention is paid to subsurface drainage envelope materials because of practical problems and a serious gap in knowledge, in spite of considerable research efforts. After treating the aim of drainage envelopes, a review of the used materials is given. Practical experience with gravel envelopes, still often used in irrigated areas, shows serious shortcomings. Since organic envelopes are vulnerable to deterioration, the only possible alternative are synthetic envelopes. Their property to retain soil particles is characterized by the so-called filter criteria. Laboratory research and field experiments to evaluate the blocking and clogging aspects of synthetic envelopes are discussed and selection criteria given.     

Strategies for reducing subsurface drainage in irrigated agriculture through improved irrigation

The traditional approach ofinstalling subsurface drainage systems tosolve shallow ground water problems is notfeasible along the west side of the SanJoaquin Valley of California because of thelack of drain water disposal methods thatare economical, technically feasible, andenvironmentally friendly. Thus, optionssuch as drainage reduction through improvedirrigation and drain water reuse are beingexamined as methods for coping with thesubsurface drainage problem. This paperdiscusses options for reducing subsurfacedrainage through improved irrigationpractices. Options are discussed forimproving irrigation system design such asupgrading existing irrigation methods andconverting to systems with higher potentialirrigation efficiencies. Methods forimproving water management are alsopresented. Case studies on upgradingexisting systems or converting to otherirrigation methods are presented along with study results of the effect of variouspolicies on reducing subsurface drainage.     

Time-dependent drainage from root zone and drainage coefficient under different irrigation management levels for subsurface drainage design in Egypt

Drainage water from the lower boundary of the root zone is an important factor in the irrigated agricultural lands for prediction of the water table behavior and understanding and modeling of water and chemical movement in the soil profile. The drainage coefficient is an important parameter for the design of subsurface drainage. On a 33,138 ha of the Nile Delta in Egypt, this study is conducted using 90 irrigation periods over a 3-year crop rotation to estimate the time-dependent drainage from the root zone and the design subsurface drainage coefficient with different cropping seasons and irrigation management levels.The results showed that the cropping seasons and the irrigation management levels as indicated by different irrigation efficiency are significantly affected the drainage rate from the root zone and the design value of subsurface drainage coefficient. Drainage rates from the root zone of 1.72 mm/d and 0.82 mm/d were estimated for summer and winter seasons, respectively. These rates significantly decreased in a range of 46% to 92% during summer season and 60% to 98% during winter season when the irrigation efficiency is increased in a range of 5% to 15%. The subsurface drainage coefficient was estimated to be 1.09 mm/d whereas the design drain pipe capacity was estimated to be 2.2 mm/d, based on the peak discharge of the most critical crop (maize), rather than 4.0 mm/d which is currently used. A significant decrease of the drainage coefficient and the drain pipe capacity ranges from 18% to 45% was found with the increase of irrigation efficiency in a range of 5% to 15%. The leaching requirement for each crop was also estimated.     

膜下滴灌暗管排水规律及土壤脱盐效果试验研究

为了探索膜下滴灌盐碱地在灌溉过程中暗管排水规律及土壤脱盐效率,设计了一种暗管排水模型试验装置系统来探究灌溉过程中暗管排水规律和排盐效果.试验通过控制灌水时间、灌水量、观测并记录暗管出水时间、排水流量、排水矿化度、土壤盐分剖面等指标,分析灌溉排水过程中暗管排水流速和排水矿化度特征以及各土层土壤脱盐效率.结果表明:经过3次灌水淋洗试验后,暗管排水流速最终趋于1.5~3.5 L/h稳定范围,排水矿化度稳定在20~40 g/L内;0~40 cm土层脱盐率高达85%,0~80 cm土层土壤脱盐率为80.5%,两暗管中间位置处脱盐率最小分别为57.96%,56.73%,69.29%,暗管上方脱盐率最大分别为71.73%,73.34%,84.26%,暗管排盐量占0~80 cm土层总盐分含量的28.9%,其余盐分被淋洗到了80 cm土层以下.     

外包滤料对暗管排水与土壤脱盐效果的影响

为了探究不同外包滤料条件下的暗管排水性能和土壤脱盐效果,基于室内试验研究成果,在田间设置4种暗管排水系统(各系统中暗管埋深均为80 cm,间距均为20 m),所用外包滤料分别为68 g/m²土工布(L)、砂滤料(S)、68 g/m²土工布+砂滤料(LS)和无外包滤料(W),以当地常规明沟排水(CK)作为对照,通过田间试验分析了春灌过程中各暗管系统的排水性能指标及土壤脱盐效率.结果表明:相比处理W,处理L,S和LS平均排水速率提升了7.44%,12.55%和15.75%,平均流量衰减度降低4.07%;处理S和LS累积排水量提高了5.11%和8.31%(P<0.05).各暗管处理春灌后平均土壤脱盐率均达47%以上,较CK提升显著,其中处理LS效果最优,为50.94%.综上,应优先选择处理LS作为河套灌区暗管排水系统外包滤料布设方案.该研究结果可为河套灌区暗管排盐技术的推广应用提供理论支撑和科学指导.     

Discharge rates,salinities, and the performance of subsurface collector drains in Egypt

To evaluate the hydraulic performance of subsurface collector drains and to study the relationships between discharge rates, crop patterns, and the salinity of drainage water, subsurface drains were monitored in different parts of the Nile Delta and Valley.Actual discharges were much smaller than design discharges. Also, overpressure in the pipes occurred frequently, indicating too small a capacity in the design. From research in one pilot area, it was concluded that if construction methods and materials are not improved, the roughness factor in the design should be increased by 100% to allow sufficient capacity.The cultivation of rice increases discharges. Salinity of drainage water is higher in winter than in summer, and higher in the north of the Delta than in the south.     

Analysis of groundwater behaviour in a farmer controlled subsurface tile drainage system in Mardan, Pakistan

Extensive subsurface drainage system was installed in districtMardan in the North West Frontier Provinceof Pakistan in 1987 to control increasingwater logging and salinity problems due tocanal irrigation. Several recentlycompleted fields studies have indicatedthat subsurface drainage system hasenormously lowered watertable in certainareas due to extensive drainage network. Therefore, a study of controlled subsurfacedrainage technique was initiated in MardanScarp area to observe the temporal andspatial variations in water table depths ofthis specific case under various modes ofcanal irrigation and monsoon rains. Twoartificially drained areas, consisting of40 ha and 160 ha respectively, werecontrolled and selected for extensivemonitoring. A total of 98 observationswells (7.6 cm dia. and 4.1 m depth) wereinstalled in between lateral drains toobserve water table fluctuation. Theresults of this study are very interesting.Each of the two areas monitored in thestudy behaved differently. It was observedthat in one of the areas design water tabledepth at 1.1 m was maintained with properfunctioning of the controlled techniqueapplied to the subsurface drainage system. The results from this area showed that 25to 55% of the time throughout the yearachieved this objective whereas in thesecond area desired water table could notbe maintained and water table depth in thisarea remained between 2.0 to 2.7 m causingunnecessary water stress to plants. Alsoit was observed that watertable in theformer area is mostly controlled by thefunctional behavior of the irrigationcanal. In addition, the proper functioningof controlled techniques in subsurfacedrainage system supplemented veryefficiently to retain the groundwater levelto the optimal limits in dry season and tothe design ones in the others for timelyneeds of the crops. Also rainfalls havesignificant impact on the spatial andtemporal behaviors of water table depths inboth the areas during the monsoon season.     

地下滴灌中毛管水力计算的数学模型与试验

为了研究地下滴灌毛管水力特性与水力计算方法,用较短毛管并通过毛管末端泄流的方式,在室内利用地下滴灌毛管水力要素试验测试系统,分别测试了2种滴灌管在轻黏土中毛管上每个滴头的流量和毛管首末两端的压力水头．结果表明：在灌水持续2min之后,地下滴灌毛管上各滴头流量均趋于恒定值;在稳定的压力水头差下,滴头流量沿程依次减少．根据毛管沿程压力变化规律,结合考虑土壤质地、土壤体积质量和初始含水率的地下滴灌滴头流量计算公式,提出了毛管水力计算数学模型．利用该模型计算的滴头流量值与其实测值之间的相对误差在1．0％左右;并计算出考虑毛管局部水头损失的加大系数约为1．20．将该模型推广应用于一般情况下的地下滴灌毛管水力计算,可求解均匀坡、均质土、均匀管径与滴头等间距时的地下滴灌毛管水力特征值．     

Optimal sampling density of hydraulic conductivity for subsurface drainage in the Nile delta

The density of hydraulic conductivity measurements is of primary importance for the design of large-scale subsurface drainage projects. This study was conducted to investigate the effect of sampling density on hydraulic conductivity estimation, and to determine the optimal sampling density using results of 3488 hydraulic conductivity tests from a 33 500 ha subsurface drainage project in the Nile Delta of Egypt. Kriging was used to obtain hydraulic conductivity point and block estimates based on the original 300 m sampling grid and on reduced sampling grids with spacings of 600, 900, and 1200 m. Kriged estimates from the complete grid were compared to those from reduced grids. The correlation coefficient between kriged estimates of block hydraulic conductivity based of the 300 m versus the 600 m measurement grid was larger than 0.90, which indicates that the optimal sampling grid spacing is in the order of 600 m. Slopes of the estimation standard deviation versus sampling density showed that the optimal sampling grid spacing was between 400 and 600 m, and could be determined from sampling grids with a spacing of 900 m or less. It appears that, for the Nile Delta, the optimal sampling density of hydraulic conductivity can be determined from a preliminary survey with a grid spacing of 900 m.     

Adaptability constraints of a technically and economically feasible subsurface drainage system in the low-lying acid sulphate soils of Kerala,India

This paper discusses the introduction of subsurface drainage as a tool to improve rice production in low land areas of acid sulphate soils. Pipe drains with 15 and 30 m spacing were installed in farmers fields in coastal lowlands of Kerala, India, at Kuttanad. Soil conditions improved within 2 years after the introduction of the subsurface drainage and significantly improved the crop yield. Data collected over a period of 14 years, showed a yield increase of 1.1 t/ha (43%) compared to non-drained areas. An economic analysis indicated that subsurface drainage is feasible with a benefit–cost ratio of 2.45, an internal rate of return of 47% and a net present value of Rs 5.17 million. The poor financial status of the farmers, however, is the main constraint for the large-scale adoption of the comparatively capital-intensive subsurface drainage systems in the acid sulphate soils of Kerala.     

Field-saturated hydraulic conductivity of soils from laboratory constant-head well tests

Field-saturated and unsaturated finite element analyses (FEA) of constant-head well percolation tests at three well pressure heads in two large tanks with three soils of widely differing field-saturated hydraulic conductivities (K_fs) were carried out. The results of these analyses were compared with those from the Glover classical approach. The A values in the Glover-type formula (A = K_fs/Q_s where A was a model parameter and Q_s was the FEA steady-state infiltration rate into the soil) were shown to be independent of soil type for a particular pressure head and soil condition. Constant-head well percolation tests were carried out in two laboratory sand tanks with the same dimensional arrangement used in the finite element analyses. Field saturation was maintained by spray irrigation, and in the unsaturated condition there was no spray irrigation. Following saturation and stabilisation of the well pressure heads, drainage ports were opened instantaneously and the rate of inflow into the well was recorded. The infiltration rates, Q_s, into the sand under the two soil conditions were multiplied by the appropriate A values from the FEA for each specific pressure head to derive K_fs. A values were significantly different under field-saturated and unsaturated conditions. K_fs of the sand was also measured independently in a constant-head permeameter. Values of K_fs from the FEA and the Glover approach were in close agreement with one another, and with that measured in the constant-head permeameter. Agreement was within 13% at the higher pressure heads. The procedure appears promising for field use.     

暗管排水条件下微咸水灌溉对土壤盐分动态及夏玉米生长的影响

进行暗管排水条件下微咸水灌溉田间试验,设置3种暗管埋深,分别为80 cm(D1)、120 cm(D2)以及无暗管排水(D0),3种微咸水浓度,其电导率分别为0.78 dS/m(S1),3.75 dS/m(S2)和6.25 dS/m(S3),共9个处理,每个处理3组重复.试验结果表明:暗管排水措施可以有效排除微咸水灌溉过程中土壤中累积的盐分;在玉米全生育期内,暗管埋深D1条件下,3种浓度微咸水S1,S2和S3灌溉时根系土壤电导率分别下降了39.00%,31.56%和29.43%,暗管埋深D2条件下,根系土壤电导率则分别下降了31.91%,18.08%和7.44%;夏玉米干物质累积量、穗棒累积量和穗棒质量分配率及最终产量均随着微咸水浓度的升高而降低;在相同微咸水浓度下,不同暗管埋设条件下的夏玉米最终产量从大到小依次为D1,D2,D0;3种暗管埋设条件下的作物需水量从大到小依次为D0,D2,D1的规律;暗管埋深80 cm的处理(D1)下夏玉米水分利用效率最高,而未埋设暗管的处理(D0)水分利用效率最低;当暗管埋设条件一定时,夏玉米水分利用效率随微咸水浓度的升高呈逐渐降低的趋势.     

农田不同排水措施地下排水效果模拟试验研究

在地下水位较高、地表易于形成积水的中国南方地区,通过农田排水措施可以及时排除多余地表积水,快速降低地下水位,以达到排涝降渍、协同调控的目的.文中基于室内砂槽试验,揭示暗管排水、明沟排水、不同反滤体高度的反滤体排水及改进暗管排水等措施的地下排水规律及效果.结果表明:将暗管周围土体置换为高渗透性土体介质的改进暗管排水可明显提高排水流量,当土体置换高度达2 cm时(对应于田间条件40 cm),其排水流量均高于相同埋深条件下的其他排水措施,达暗管排水的1.59~1.66倍;改进暗排在地表积水消失时仍保持较大的排水流量,可达相同埋深暗管流量的2倍以上,在积水层消失后,能迅速降低农田土壤水的渍害胁迫,将地下水位降低至暗管埋设高度;各种排水措施,在地表积水即将消失时,出现了流量与水头变化幅度较大的现象.相对于各种地下排水措施,改进暗管排水在除涝降渍中存在明显优势.研究结果可为涝渍灾害易发地区高效除涝降渍减灾工程设计和建设提供参考.     

Predicting effects of drainage water management in Iowa's subsurface drained landscapes

Long-term hydrologic simulations are presented predicting the effects of drainage water management on subsurface drainage, surface runoff and crop production in Iowa's subsurface drained landscapes. The deterministic hydrologic model, DRAINMOD was used to simulate Webster (fine-loamy, mixed, superactive, mesic) soil in a Continuous Corn rotation (WEBS_CC) with different drain depths from 0.75 to 1.20 m and drain spacing from 10 to 50 m in a combination of free and controlled drainage over a weather record of 60 (1945-2004) years. Shallow drainage is defined as drains installed at a drain depth of 0.75 m, and controlled drainage with a drain depth of 1.20 m restricts flow at the drain outlet to maintain a water table at 0.60 m below surface level during the winter (November-March) and summer (June-August) months. These drainage design and management modifications were evaluated against conventional drainage system installed at a drain depth of 1.20 m with free drainage at the drain outlet. The simulation results indicate the potential of a tradeoff between subsurface drainage and surface runoff as a pathway to remove excess water from the system. While a reduction of subsurface drainage may occur through the use of shallow and controlled drainage, these practices may increase surface runoff in Iowa's subsurface drained landscapes. The simulations also indicate that shallow and controlled drainage might increase the excess water stress on crop production, and thereby result in slightly lower relative yields. Field experiments are needed to examine the pathways of water movement, total water balance, and crop production under shallow and controlled drainage in Iowa's subsurface drained landscapes.     

Field determination of soil hydraulic properties for simulation of the optimum watertable regime

A field experiment to evaluate accurate cost and time efficient methodologies for determining soil hydraulic properties was done at the NIAB Research Station at Faisalabad, Pakistan. The experiment was performed on a freely draining loamy soil. This soil type is representative of 75% of the topsoil in a tile drainage area known as the Fourth Drainage Project. Redistribution of water was monitored at five locations, for seven depths, following a steady state infiltration for prolonged time. The data were analyzed with Darcian flow analysis, three simplified methods, and two parameter optimization programs to calculate unsaturated hydraulic conductivity. The Darcian flow analysis was used as a reference against which the simplified methods were compared. Two simplified methods produced satisfactory results with less effort. The drawback is that the simplified methods alone do not provide enough information for use in simulation models. The advantage of the two optimization programs — SFIT and RETC — is that they are based on a continuous function which describes complete h() and K() curves. This is a requirement for computer simulation of salt and water movement in the unsaturated soil. The results of the optimizations were evaluated by their correspondence to field measurements and to laboratory measurements and by their ability to simulate soil water flow. Both programs fit the observed field data well, but only the SFIT optimized parameters were suitable for soil water flow simulations.Abbreviations IWASRI International Waterlogging and Salinity Research Institute - NRAP Netherlands Research Assistance Project - NIAB Nuclear Institute for Agriculture and Biology - SSP Soil Survey of Pakistan Revised paper from Field determination of soil hydraulic properties presented in ICID, CIID IDW5, Lahore, Pakistan (1–55 — 1–64).     

利用盘式负压仪测定土壤导水率的计算方法对比

土壤导水率作为重要的水力特征参数之一,准确测量和计算不仅有助于促进土壤非饱和带的水分运动过程理论研究,同时可为合理确定农田灌排技术参数提供科学依据.为了比较分析在盘式入渗仪下不同导水率计算方法的适用性,针对2种土地类型(菜地、茶园)进行了4个负压水头(-9,-6,-3,0 cm)、2个盘径(10,20 cm)的入渗试验,并通过不同计算方法计算导水率.结果表明:盘径对导水率影响不具有统计学意义,且不同计算方法结果趋于一致,因此在野外缺水条件下,可考虑选用小圆盘进行试验;对于不同的土地类型,建议选择不同的方法测量,作为耕作地的菜地,计算导水率时建议使用稳态流方法,而茶园导水率的测定则推荐使用瞬态流方法;在相同负压下,不同土地利用方式对导水率的影响具有统计学意义,且对于不同的计算方法,2种土地类型在4个负压下表现的导水率变化规律一致.     

植被群落演替对土壤饱和导水率的影响

土壤饱和导水率是表征土壤入渗能力的重要参数,对不同土地利用类型反应敏感。为了揭示植被演替对土壤剖面上饱和导水率的影响规律,采用恒定水头法测定了天童林区155 a植物群落演替序列60 cm深土壤剖面上的饱和导水率。结果表明,不同演替阶段饱和导水率均随土壤深度增加迅速降低,在0～20 cm土层内,各演替阶段饱和导水率均存在极显著差异,0～60 cm土层内饱和导水率的平均值从裸地、石栎+檵木灌丛、马尾松林、木荷+马尾松林、木荷林到栲树林升高极为显著,植物群落演替到灌丛阶段,平均饱和导水率已与裸地存在显著差异,演     

泰安棕壤土不同土地利用类型饱和导水率比较

为了分析土地利用类型对土壤饱和导水率的影响,利用单环入渗概化解法对泰安棕壤土草地、麦地、果树行间裸地3种土地利用类型饱和导水率进行研究.结果表明:草地、麦地、果树行间裸地的饱和导水率、入渗速率以及累计入渗量呈现依次降低的变化趋势.随着时间的增加,累计入渗量不断增加,试验时间120 min内,草地累计入渗量最大,数值为78.564 cm;麦地入渗量次之,数值为67.609 cm;果树行间裸地入渗量最小,数值为30.082 cm.利用实测累计入渗量与观测时间的拟合关系,得到3种土地利用类型累计入渗量的表达式,对累计入渗量进行估算,草地、麦地、果树行间裸地累计入渗量计算值与实测值相对误差分别在6,8,7 min后波动在5%以内,在15,52,56 min后波动在1%以内,同时推求了草地、麦地和果树行间裸地3种不同土地利用类型下的土壤饱和导水率K_s分别为0.073 1,0.032 9,0.015 8,以期为不同土地利用类型对原状土饱和导水率的影响研究提供参考.     

Diagnosis of mineral clogging hazards in subsurface drainage systems

The paper presents a global review of drain clogging hazard criteria. Some of them are simple granulometric formulae, some include an evaluation of soil structural stability, and some others are based on laboratory tests which reproduce water-flow through a soil core. A recent development is then described. Terzaghi's theory of critical hydraulic gradient explains structural break-up of soil samples by water-flow towards drain pipes. Based on this theoretical approach, a laboratory test has been designed to determine experimental values of the hydraulic gradient causing soil breaking. This test is used to compare the stability of different soil materials and to diagnose mineral clogging hazards.Due to the existence of numerous granulometric criteria there is evidence that no global criterion can be found. If a proper granulometric criterion is suited to a given climatological and pedological context, the hydraulic laboratory test is probably the most cost-effective method to diagnose mineral clogging hazard, especially when no field references are available.