北方旱地土壤氮素平衡

北方大部分地区的旱地土壤中,农业氮素一般表现亏损,平衡强度约87%;园田土壤氮素略有盈余,平衡强度约123%.~(15)示踪研究表明,旱地土壤主要作物氮素利用率平均为27.04%,土壤残留24.79%,亏缺损失48.17%.园田主要蔬菜氮素和用率平均为29.11%,土壤残留22.67%,亏缺损失48.23%,其间差异很小.北方旱地施用铵态氮化肥主要损失是氨的挥发.影响氨挥发的因素有风速、温度、土壤水分、土壤质地、化肥品种.氮肥深施是防止氨挥发的有效方法.     

农田土壤含水率与坚实度快速信息采集系统

介绍了一种农田土壤含水率与坚实度快速信息采集系统.本系统包括土壤介电传感器、圆锥指数传感器及深度传感器,可以快速、同步、实时地获得0～500mm范围内土壤剖面含水率与圆锥指数信息.同时,本系统还结合了GPS和GIS技术,实现了土壤参数的空间分析,可以更方便地把系统应用于农田信息管理.本系统为实现土壤水分和坚实度的同步测量搭建了一个智能化的试验平台,并且在与德国波恩大学农业工程研究所的合作中成功地应用于田间测量.     

肥料结构对红壤氮素淋失的影响及防治措施

肥料结构是影响氮素淋失的重要因素。氮肥进入土壤后,其损失途径主要是氨挥发和反硝化的气态损失。但是,氮肥通过渗漏淋失对地下水(饮用水源)的污染,也不容忽视。为此,综述了近年来3种肥料结构(即单施无机氮肥、无机肥混施、无机肥与有机肥混施)对红壤区稻田土壤氮素淋失的影响的研究进展,并且提出了如何防止氮素淋失的对策     

污水灌溉条件下作物对土壤重金属吸收特征比较

通过采样和化学测试，对污水灌溉条件下，小麦、水稻、蚕豆和油菜果实中Cu、Zn、Pb、Cr和Cd的含量及土壤中重金属本底浓度进行测定和分析。结果表明，污水灌溉对4种作物吸收土壤重金属的能力影响不显著，而不同作物种类对这种吸收能力的影响表现出显著的差异。     

Irrigation scheduling in a mature peach orchard using tensiometers and dendrometers

Three trickle irrigation schedules, two of which were scheduled according to soil water potential ( soil) (tensiometer method) and daily stem contraction (DSC) (dendrometer method) respectively and the other one was a schedule of restricted water supply, were applied to a mature peach orchard.The annual water application based on soil was greater than that based on DSC. However, tree growth, fruit size and leaf water potential (leaf) on the trees in the dendrometer scheduling plot did not differ from those in the tensiometer scheduling plot while the premature fruit drop and fruit bud initiation were greatly different. The restricted water supply treatment limited significantly both tree and fruit growth. In addition, the lower leaf was observed on the trees in this plot.Further study shows that use of the dendrometer method for scheduling irrigation satisfies the water needs of the plant and that the tensiometer method is less accurate.Abbreviations leaf leaf water potential - soil soil water potential - DSC daily stem contraction - LVDT linear variable displacement transducer - PET potential evapotranspiration     

Farmers' irrigation practices in a high rainfall area

Recent droughts in the humid southeastern United States have focused attention on the need for and use of supplemental irrigation. Total annual rainfall amounts are sufficient for most crops in the region. However, erratic distribution of rainfall and the low water-holding capacities of most soils in the region cause frequent drought stresses in many crops. An on-farm study was conducted in southeastern Alabama to evaluate the effects of farmers' irrigation scheduling decisions on soil moisture variations in peanut fields irrigated with center-pivot irrigation systems. The study showed that the way irrigation was practiced in this high rainfall area often caused soil moisture deficit (SMD) level higher than the desired SMD limit during over 20% of the 140-day growing season. This is partially due to farmers' tendency to delay irrigation in anticipation of rainfall which may or may not occur, as rainfall during the growing season is often erratic and local. In contrast SMD in non-irrigated fields was higher than the SMD limit for half of the growing season.Abbreviations SMD soil moisture deficit - ET evapotranspiration - R_eff effective rainfall - WHC water holding capacity     

土壤水分特征曲线几种标定的对比分析

土壤水分特征曲线的标定是土壤水的能量和数量关系在不同尺度间转换的方法,也是植被生态需水机理研究的重要组成部分。通过对传统的迭代法、一次法和建立的2种混合遗传算法进行比较,标定的结果表明,多项式遗传算法能综合考虑2种方差的影响,并能给出一致性的标定结果,这种经验式混合遗传算法对传统的标定算法进行了改进。     

地下滴灌棉花栽培试验与技术研究

根据新疆兵团农五师九十团8hm^2地下滴灌棉花栽培、灌溉和施肥等方面的试验研究，地下滴灌与地面滴灌比较，无论投入产出和作物的长势，地下滴灌都比地面滴灌优越。地下滴灌比地面滴灌工程设备、材料费低0．15297万元／hm^2，降低年运行费用841．8元／hm^2。     

应用TDR对土壤含水率及土壤冻结融解深的计测

运用 TDR(Time Domain Reflectometry)计测土壤含水量 ,80年代以来就受到了瞩目 ,到今天为止TDR方法在土壤盐分浓度 ,浸润面深度 ,冻结融解面深度等许多领域得到广泛应用。为了确认在运用 TDR方法进行土壤含水率测定时介电常数 ε与含水率 θ之间的关系曲线的滞后现象的有无 ,以及确认运用 TDR方法计测土壤冻结融解面深度的有效性 ,进行了一系列的实验。实验证明 ,在运用 TDR方法进行土壤含水率测定时介电常数ε与含水率θ之间的标定曲线中没有出现滞后现象 ,运用 TDR方法计测土壤冻结融解面深度不论在室内实验还是在田间实验中都很有效 ,并取得了较高的精度。     

新疆阿瓦提灌区土壤盐渍化状况的

采用主成分分析方法对阿瓦提灌区土壤盐渍化状况进行了研究，结果表明，该地属于中重度硫酸盐盐渍地，0～30cm耕作层含盐量在0.5%-4%之间，在灌区内部土壤盐分存在多次积盐和脱盐过程，耕作层第一、二主成分显著，累计贡献率高达90%，第一主成分综合反映灌区内土壤盐渍化程度，第二、第三主成分联合反映了土壤的碱性特征。