盐度对中华绒螯蟹繁殖特性及胚胎质量的影响

为探究盐度对中华绒螯蟹亲体繁殖特性及所产胚胎质量的影响,开展了不同盐度(3、6、9、12、15、18、21)下亲体的生殖产卵实验,分析了各盐度下亲体的产卵量、生殖指数和生殖力等繁殖特性及所产胚胎的卵径、重量、生化成分和脂肪酸组成。结果显示：(1)中华绒螯蟹产卵的最低盐度为6,在盐度6～21的范围内,中华绒螯蟹亲本的产卵量、生殖指数和生殖力均表现为先升高后下降的趋势,其中盐度18时,亲本的产卵量、生殖指数和生殖力均最高,且与其他各组都有显著差异。(2)盐度6时胚胎直径最大,平均为(391.13±12.27)μm,显著高于其他各组。盐度12时单个胚胎湿重和干重均最高,分别为(50.64±2.80)μg和(14.85±0.31)μg,且与其他各组均有显著差异。(3)随盐度的增加,中华绒螯蟹胚胎的粗蛋白、总脂肪和水分含量都呈现先升高后降低的变化趋势。其中盐度15时,胚胎中粗蛋白、总脂肪和灰分含量均达到最高,平均分别为(20.64%±3.42%)、(8.65%±1.44%)和(1.30%±0.22%)。各盐度下胚胎水分含量无显著差异。胚胎中胆固醇和磷脂含量均随盐度的增加呈现出先上升后下降的变化趋...     

A calibration method of detecting soil water content based on the information-sharing in wireless sensor network

In agricultural production, there is contradiction between the cost and accuracy of detection during the course of acquiring soil water content (θ) online. This conflict is one of the core issues of automatic water-saving irrigation technology in agriculture. At the same time, capacitive soil moisture sensor (CSMS) has received considerable attention, for it can acquire θ with low cost and high precision, and meet the application requirements of wireless sensor network (WSN). But CSMS is vulnerable to the soil temperature (T_s) and salinity (S_s) in the measurement process. Therefore, this study took EC-5 sensor for example to establish water detection calibration models of soil temperature and salinity for single sensor, using Least Squares Support Vector Machines on MatLAB (LS-SVMlab) as the tool. On this basis, we explored the spatial variability of T_s and S_s, and then a method, which could be used to calibrate the output signals of sensors in multi-point network, was proposed based on the information-sharing (T_s or S_s) technology of WSN. Through laboratory experiment, we effectively reduced the impact of soil temperature and salinity on the single sensor. In example analysis, we investigated the detection precision and costs under different information-sharing radiuses (r). And the results indicated that the method we proposed based on the information-sharing technology of WSN could successfully calibrate the influence of soil temperature and salinity on sensors in multi-point network, and it was an efficacious approach to determine the balance between the calibration accuracy of moisture sensor and the investment of agricultural production. For example, while the calibration precision of soil temperature and salinity is respectively 1%, the costs can be reduced by 30%.     

Comparison of nuclear and capacitance‐based soil water measuring techniques in salt‐affected soils

A field calibration experiment was carried out on salt‐affected clayey soil in Syria, to compare the sensitivity to soil electrical conductivity (ECe), and bulk density (ρ_b) of two instruments for estimating soil moisture: the neutron probe (NP) and the Diviner 2000 capacitance probe (CP). The results showed that the values of the correlation coefficient of the calibration were decreased when the ECe and ρ_b values increased; this decrease was more pronounced for the Diviner 2000, indicating that it was more sensitive to ρ_b and ECe than the NP. When only scaled frequency was used in the fitted equation, the Diviner 2000 in wet soil underestimated soil water content significantly at all depths, but especially in the top layer, by up to 0.09 cm³/cm³ compared with gravimetric determinations. However, in dry soil, the Diviner 2000 overestimated the volumetric water content by up to 0.05 cm³/cm³ in the top 15 cm, and by 0.03 cm³/cm³ at 30‐45 cm depth. The performance of the neutron probe was better overall; using a factory calibration curve no significant differences were observed between NP estimates and the gravimetric values. Including both ρ_b and ECe in the calibration equations improved the fits, although the regression coefficient (R²) for the Diviner 2000 remained low.     

Irrigated land retirement

Land retirement is ceasing irrigation withthe goal of reducing load, in general, ofdissolved constituents and, in particular,of trace elements, present in subsurfacedrainage generated from irrigated lands. Retirement is achieved through a process ofgoal setting, strategy development anddetermining effects, developing landselection criteria, implementation, andmonitoring. In this study, effects of landretirement are evaluated using hydrologic,soil and economic models as well as resultsfrom a field demonstration study. From themodeling and field monitoring, a process isdeveloped to meet the goals of a landretirement program in the San JoaquinValley of California.Potential negative effects listed for landretirement included loss of agriculturalproductivity, perhaps permanently, and lossof revenue to surrounding communities. Uncertainties included those associatedwith reuse of retired lands as wildlifehabitat, with retired-land maintenanceincluding dust control, with potentialpreservation of retired lands in reservefor future re-introduction to irrigated ordry-land agriculture, and withinstitutional changes concerning repaymentof federal and state water contracts. Benefits would accrue from economic returnto the landowner from the sale of property,the sale or lease of irrigation watersupply, the reduced cost of handlingdrainage, and allocation of freed-up waterto beneficial uses, and the reduced risk ofselenium exposure to fish and wildlife.A recommended sequential approach to selectand manage retired land is to identifyprimary objectives; formulate and implementarea-specific land retirement scenarios;measure biologic, hydrologic, soils andeconomic consequences in the short term andthe long term and manage and monitorretired lands based on dynamic biologic,hydrologic and soil conditions.     

咸水灌溉下土壤水盐变化的试验研究

2002年在内蒙古河套灌区红卫节水示范园进行了咸水灌溉试验,分析试验结果得出:咸水灌溉下的土壤经过秋浇后含盐量可以降到咸水灌溉前水平。以荷兰Wageningen农业大学等单位开发的土壤水分大气作物系统模拟软件SWAP为工具,应用示范园的土壤、水、盐分试验资料对模型的参数进行了率定和验证,模型模拟结果和田间试验结果符合较好。     

新疆盐碱地长期利用盐水灌溉土壤盐分变化

在地下水位3～5m、壤质土壤条件下,利用盐碱地时用2～5g/L盐化水灌溉,土壤1m剖面均为脱盐状况。灌溉盐化水15年后,1m土壤残留阴离子浓度较小,多点平均为3.709毫克当量/100克土。其中HCO-3相对较多,1m多点平均为0.404毫克当量/100克土。K++Na+浓度很大,1m多点平均为2.492毫克当量/100克土。这时,土壤1m全盐多点平均为0.248%,在灌溉水矿化度不直接危害作物生长时,不影响耕作和作物正常生长。由此可见,盐化水在盐碱地上无排灌溉,是可行的。     

Managing secondary dryland salinity: Options and challenges

Salt occurs naturally at high levels in the subsoils of most Australian agricultural land. As a result of clearing native vegetation, groundwater tables have risen, mobilising the stored salt and causing adverse impacts on farmland, infrastructure, water resources, and biodiversity. The main action required to prevent groundwater tables from rising is establishment of perennial plants, either herbaceous (pastures or crops) or woody (trees and shrubs). Recent technical and economic research has emphasised how difficult it will be to establish sufficient perennials to get control of groundwater tables. Where watertables are already shallow, the options for farmers are salt-tolerant plants (e.g. saltbush for grazing) or engineering (e.g. deep open drains). The existing options for farm-level salinity management are reviewed, with mixed but somewhat disappointing findings regarding their suitability for addressing salinity. However, there are also a number of good prospects for development of new and better options for plant-based management of salinity, and these are described.     

Farm salinity appraisal with water reuse

The need for a better understanding of the interaction between irrigation practices and the elevation and quality of the water table is of paramount importance for developing irrigation management strategies to ameliorate the regional problems of elevated saline water tables in the San Joaquin Valley, California. An area of approximately 3000 ha which includes portions of the Diener Ranch and the adjacent University of California, Westside Research and Extension Center, located south of Five Points in the Westlands Water District on the west side of the San Joaquin Valley was chosen for extensive field measurements. Field work consisted of four main activities namely, field instrumentation, collection of records of field activities, periodic data collection, and analyses of field data. Field measurements of water table carried out during 1994 indicated that the water table elevation was sensitive to the irrigation practices. There was a general increase in the area with a water table close to the surface during the irrigation season, and a return to water table elevations similar to the starting conditions at the end of the season. During the study period, the surface water quality deteriorated more in areas irrigated with reuse water and persisted through the end of the season. Depth averaged electrical conductivity for the study area over 6.5 m decreased between December 1993 and December 1994. Vertical hydraulic gradients in the saturated zone, were found to be an order of magnitude larger than horizontal gradients. The direction of vertical gradients changed, with downward gradients following pre-irrigations and upward gradients later in the season, when crop water requirements increased. Based on the results of the field study, it can be concluded that the irrigation management practices have a direct effect on local water table response as well as on water quality. Therefore, irrigation practices that promote less deep percolation losses may be helpful in controlling the water table rise.     

棉田膜内与膜间土壤溶液含盐量的变化

用定期取表层土样测定其电导率和在不同深度埋设盐分传感器探头的方法 ,在作物生长季节内 ,监测了棉田膜内和膜间不同深度的土壤溶液含盐量变化。结果为 :1棉田膜内与膜间表层土壤和 1 0 cm、30 cm深土壤溶液含盐量变化较大 ,且规律相同。未灌水时上升 ,灌水后迅速下降。膜间未灌水期间的含盐量上升幅度大于膜内 ,灌水对膜内和膜间表土洗盐、1 0 cm、30 cm深土壤溶液含盐量的降低作用没有差别。降雨可引起膜内和膜间 1 0 cm深土壤溶液电导率的变化 ,这个影响也是膜间大于膜内。 2 60 cm深的土壤溶液不存在明显的盐分累积现象 ,灌水可使这里的土壤溶液含盐量缓慢降低 ,膜间的降低过程快于膜内     

干旱区土地盐渍化时空动态变化及影响因子分析

土壤是人类社会及一切社会活动的基本条件,而土壤盐渍化是土壤退化和土壤荒漠化的重要类型之一,是当今干旱区发展中面临的重要问题之一,也是影响干旱半干旱区农业生产的第一障碍性问题。土壤盐渍化时空动态变化研究是发展土壤监测研究及估算方法的重要基础工作。因此盐渍化治理工作的好坏也成了人们关注的问题。文章以新疆塔里木盆地北缘渭干河-库车河三角洲绿洲为研究区,采用1989年9月25日及2001年8月1日的遥感影像,通过计算盐分指数,得到盐分指数图像,进一步将盐分指数图像参与其它波段进行分类,通过统计分析,研究了渭干河-库车河三角洲盐渍地动态变化状况和变化趋势,并对变化影响因素进行了分析。结果表明：非盐渍地有所减少,轻、微盐渍地有所扩大,年均扩大率3.37%,中度盐渍地和重度盐渍地都相应减少,而中度盐渍地减少较多,年均减少率分别为1.96%和1.09%;盐渍地时空变化是同时受自然和人文因素影响的复杂过程,其中人为因素的影响最大。虽然盐渍化治理工作取得了一定的成就,但干旱区盐渍化防治工作需要进一步努力和加强。