区域节水灌溉的节水潜力简易计算方法探讨

节水灌溉是用尽可能少的灌溉水投入,取得尽可能多的农作物产出的一种灌溉模式.节水灌溉的节水潜力是在保持农作物产量不降低的前提下,通过采用工程、技术和措施使从水源取用的灌溉水通过输水、配水和灌水供给作物利用的过程中,可能减少的损失水量.在制定区域节水灌溉规划时,需要对发展节水灌溉后产生的节水潜力进行分析计算,以此作为规划决策的依据.对于节水灌溉的节水潜力分析计算方法国内已进行过诸多研究,但要精确计算则很困难.为此,借用《全国灌溉用水定额编制》的研究成果,采用作物灌溉用水"参照定额"、作物灌溉用水定额调节系数和作物用水定额计算式提出了一种区域节水灌溉的节水潜力简易计算方法,并以全国2010年节水灌溉发展规划的节水潜力作为算例,分析计算了规划目标年发展节水灌溉工程的节水潜力.     

调亏灌溉对蚕豆需水规律及水分利用效率的影响

在甘肃秦王川灌区通过大田试验研究了苗期调亏灌溉对蚕豆需水规律和水分生产效率的影响.结果表明:调亏处理蚕豆在苗期、拔节期及花荚期需水量减少,叶面积、蒸腾速率和光合速率下降,在鼓粒成熟期则相对增加,作物的总需水量减少.叶面积、蒸腾速率和棵间蒸发减少是调亏灌溉需水量降低的主要原因.调亏灌溉能够延缓鼓粒期叶片衰老,提高光合速率,使光合同化物向籽粒分配的比例增加,提高水分生产效率.     

Movements by wild brown trout in a boreal river: response to habitat and flow contrasts

Abstract  Radio transmitters were implanted in wild brown trout, Salmo trutta L., in the River Måna at low summer water flows ( n  = 18), higher flow in summer ( n  =   20), and variable, peaking flows in autumn ( n  =   20), and tracked two to four times day and night for 4–5 weeks. Individuals were caught and released in a 4-km uniformly channelised section, and in a 4-km natural diverse river section. Substantial individual variation in home range and total movement (924–85 818 m² and 295–7014 m) suggested flexibility to adapt to local environmental conditions. Fish were stationary most of the time (median movement 0 m), but some individuals undertook few and apparently sporadic longer movements, sometimes involving shifts in home range. No consistent diurnal pattern in movements was found. Trout in the uniform habitat section appeared to have larger home ranges and moved more than trout in the natural section. Differences were, however, not statistically significant in most comparisons, due to large individual variation. Similarly, larger home ranges and movements between trials related to higher flow were found, but differences were generally not significant. No consistent effects of sudden, extreme peaking flows on area use or movements by the brown trout were observed.     

Spatiotemporal changes in terrestrial water storage in the Beijing-Tianjin Sandstorm Source Region from GRACE satellites

The Sandstorm Source Control Project in and around the Beijing-Tianjin region was one of the most important ecological projects in China. Terrestrial water storage (TWS) has important impacts on the ecological construction, agriculture, industry, and resident’s lives. Based on the Gravity Recovery and Climate Experiment (GRACE) data, meteorological and Moderate Resolution Imaging Spectroradiometer (MODIS) data, etc., this paper analyzed spatiotemporal characteristics of TWS, groundwater storage, and precipitation, and explored the influencing factors of regional TWS combined with land use and land cover (LULC), social and economic data. The most important results were as follows: (1) From 2003 to 2016, TWS in the Beijing-Tianjin Sandstorm Source Region showed a decreasing trend with a rate of 3.14 mm yr⁻¹. (2) The TWS decline was caused mainly by groundwater overexploitation, but not precipitation variation. (3) Spatiotemporal variations of TWS were related to LULC. The area with the most serious decrease of TWS was mainly located in the southwestern part of the region, where farmland percentage and population density were greater. (4) Reducing the percent of farmland and tree planting, and adding the shrub and grass planting, could be a viable choice for the Beijing-Tianjin Sandstorm Source Control Project. These results provide a scientific basis for regional water resource and ecological management.     

Effect of soil pore size distribution on plant-available water and least limiting water range as soil physical quality indicators

Soil pore size distribution(SPSD) is one of the most important soil physical properties. This research investigated the relationships of location and shape parameters of the SPSD curves with plant-available water(PAW) and least limiting water range(LLWR) of the light-textured soils at the Torogh Agricultural Research Station in north-eastern Iran. Soil moisture release curve(SMRC), PAW and LLWR in matric heads of 100 and 330 h Pa for the field capacity and location and shape parameters of the SPSD curves of 30 soils with different texture and organic carbon contents were determined, and the variable relationships were statistically analyzed. The results showed that the median equivalent pore diameter(de), mean de, standard deviation(SD*), and skewness of the SPSD curves were significantly correlated with PAW(PAW330) and LLWR(LLWR330) measured in a matric head of 330 h Pa. Decrease in deand increase in the diversity of soil pore size(SD*) increased PAW330 and LLWR330. The SD* values of all the soil samples were lower than the optimal ranges suggested in literature. Neither PAW nor LLWR values were significantly different in the soils with the optimal modal deand those with non-optimal modal de. Optimal values of median and mean equivalent pore diameters and kurtosis of SPSD curves led to a significant improvement of PAW330 and LLWR330 as soil physical quality indicators. It was recommended to revise the optimal ranges for SD* and modal defor future studies.     

秸秆或粉煤灰添加对砂姜黑土持水性及小麦抗干旱胁迫的影响

针对黄淮海平原典型中低产土壤砂姜黑土黏粒含量较高,土壤有效水分库容较低,严重限制作物生产的现状,该文采用盆栽试验,研究了不同外源改性物料的添加对土壤持水性能及小麦生理的影响,以期获得农田水分管理过程中的关键参数。盆栽试验设置常规氮磷钾(control,CK),常规氮磷钾配施下的添加秸秆(straw returning,SR)、秸秆碳(straw carbon,SC)和粉煤灰(fly ash,FA)处理,维持土壤相对含水率在80%,培育小麦至抽穗期,开展为期10 d的干旱胁迫试验。结果显示SR和SC处理提高了土壤持水能力,且处理间的差异较小;FA处理因其表面富含大量疏水性结晶矿物,土壤相对含水率下降较快,迟效水含量显著低于其余处理,但土壤速效水含量显著提高。不同改性措施均有提高小麦叶片相对含水率,减轻干旱胁迫的趋势,但在极端干旱胁迫下,FA处理叶片相对含水率不仅明显低于其余处理,且作物体内积累大量丙二醛、过氧化氢等有害物质。田间管理中砂姜黑土相对含水率应维持在38%(SR)、36.5%(SC)和24.5%(FA)以上,当土壤相对含水率低于30.78%(SC)、28.43%(SR)和22.5%(FA)时将会对作物生理产生不可逆的伤害。鉴于秸秆优良的保水性能,粉煤灰“富水,不保水”的特性,秸秆与粉煤灰的配合施用将利于砂姜黑土的改良。相关机制值得进一步研究。     

间歇式双循环工厂化养殖系统构建及其养殖效果

为改善工厂化循环水养殖系统水质净化效果,提高养殖密度和成活率,构建了间歇式双循环工厂化养殖系统。通过间歇运行生物膜反应器增加水力停留时间,充分降解含氮污染物;连续运行弧形筛及时去除固体颗粒物。考察了该系统的启动过程及石斑鱼高密度养殖效果。启动初期,将硝化型生物絮团与海绵填料混合培养,生物膜22 d即可挂膜成功。以30.03 kg/m~3为初始养殖密度开展石斑鱼养殖试验,经66 d养殖,石斑鱼平均质量从(273.00±12.22)增至(552.52±107.04) g,最终养殖密度达到60.78 kg/m~3,成活率为100%。养殖过程中,生物膜逐渐适应养殖环境,氨氮、亚硝酸盐氮去除率从13.33%、14.84%增至93.73%、93.50%。此外,在弧形筛进水槽增加曝气形成曝气式弧形筛,可进一步除去细小颗粒物,有效控制养殖水体浊度。     

基于综合判别法的广东省水土流失状况遥感分析

以2009和2010年10 m分辨率的ALOS多光谱遥感影像为数据源,采用计算机自动分析与人机交互判别相结合的方法,对广东省水土流失状况进行了遥感分析。结果表明:广东省土地利用以林草地、水田、建筑用地、水域和旱地为主,植被覆盖状况良好,珠三角和粤西地区地形平缓,粤北山区地形起伏较大;全省水土流失总面积20945.87 km 2,其中自然侵蚀面积14781.06 km 2,人为侵蚀面积6164.81 km 2;全省水土流失以轻度和中度侵蚀为主,主要分布在河源、梅州和云浮等地,其中生产建设活动导致的人为侵蚀集中分布在惠州、清远和广州等地。