Physiological Basis of Irrigation Scheduling for Seed Production in Egyptian Clover Syn. Berseem (Trifolium alexandrinum L.) Crop

A field experiment was conducted to find out the critical physiological stages of irrigation schedules inducing better growth, physiological efficiency and seed yield potential of berseem ( Trifolium alexandrinum L., Var. S-99-1). For this purpose eight irrigation treatments were made comprised of four treatments of three irrigation (W₁, W₂, W₃ and W₄), three treatments of four irrigation (W₅, W₇ and W₈) and one treatment of five irrigation (W₆) at various physiological stages i. e. regeneration, flower initiation, full bloom, seed initiation and advance seed development stage.
Thus based on the experimental results the physiological role of watering in berseem seed production could be discussed as:
With-holding of irrigation either at regeneration or at full bloom stage developed potential water stress in plants as indicated by high proline content of irrigation treatments — W₄, W₁ and W₇; and further brought out disturbance on the formation of carotene, synthesis of water soluble sugar and translocation of sugar towards reproductive organs during grain development stage. These stresses adversely affected the plant growth and flowering behaviour. The irrigation at seed initiation stage increased the seed yield. Continuous irrigation did not appear to be useful. Thus it can be concluded that irrigation at three critical physiological stages i. e. regeneration, full bloom and seed initiation was found to be essential for obtaining potential seed yield of berseem.     

加热光纤法同步测定土壤水热参数误差分析

土壤水热参数是研究土壤水热传输的基本物理参数。当前热脉冲探针法（HPP）可同步测定土壤水热参数,但该方法仅限于在点尺度下测定。与其具有相同理论基础的加热光纤法（SPHP-DTS）,可将测定尺度增大至田间千米尺度,但其测定精度尚未得到有效验证。为了探知SPHP-DTS法的误差,本研究进行了SPHP-DTS法与HPP法测定土壤水热参数的对比试验。结果表明,以HPP为标准,加热光纤法测定热导率的精度RMSE为0.13 W?m-1?℃-1。SPHP-DTS法测定的热导率显著高于HPP法,主要原因在于加热光纤时产生的温度效应。通过热导率法测定土壤含水率时,在热导率测定误差的影响下,SPHP-DTS法的测定精度明显低于HPP法。SPHP-DTS法测定土壤水热参数的其他误差来源包括光纤与土壤之间多个界面的接触热阻、光纤的温度敏感性、噪音干扰以及温度梯度驱动下的水分迁移。本研究可为SPHP-DTS法提升土壤水热参数测定精度提供理论参考。     

生物结皮生长发育对黄绵土抗侵蚀性能的影响

[目的] 黄土高原退耕还林(草)工程驱动的生物结皮发育可显著抑制土壤侵蚀,为探明土壤抗侵蚀性能随生物结皮生长发育的变化特征及其响应机制。[方法] 设置藻结皮、藓结皮和自然演替结皮3个处理,培育176天,系统研究生物结皮不同发育阶段及其类型差异对黄绵土抗侵蚀性能的影响。[结果] (1)生物结皮盖度、厚度、生物量、叶绿素和粗糙度随生长时间均显著增加,培育初期藓结皮较高,培育末期自然演替结皮反而最高。(2)随生物结皮发育,土壤黏结力呈幂函数增强,较初期增加39.8%~60.3%;质量损失率呈指数函数减小,较初期降低45.6%~57.3%;饱和导水率变化趋势较为复杂,但培育末期均最低(0.08~0.12 mm/min)。(3)土壤黏结力随生物结皮盖度、厚度、叶绿素、生物量和表面粗糙度的增加呈幂函数增长,质量损失率随生物结皮盖度、厚度、叶绿素、生物量和表面粗糙度的增加呈指数函数下降。(4)土壤抗侵蚀综合指数(C_ser)可表示为盖度(Cov)、厚度(T)和生物量(B)的幂函数(C_ser=0.279 Cov^0.194 T^0.188 B^0.119, R²=0.73, p＜0.05)。[结论] 黄土高原生物结皮发育可显著提高黄绵土抗侵蚀性能,藓结皮效果最强。     

高寒草甸退化对土壤电导率变化影响的研究

土壤电导率是表征土壤水溶性盐的一个重要指标,可反映土壤盐渍化程度.为了研究高寒草甸退化对土壤电导率的影响,以三江源区未退化高寒草甸和退化高寒草甸为研究对象,系统分析了退化高寒草甸的植被特征和土壤特征与土壤电导率的相互关系.结果表明:高寒草甸退化会对土壤电导率产生显著负影响,且土壤电导率与评价高寒草甸的退化指标植被盖度、...     

Integrating multiple electromagnetic data to map spatiotemporal variability of soil salinity in Kairouan region,Central Tunisia

Soil salinization is a major problem affecting soils and threatening agricultural sustainability in arid and semi-arid regions,which makes it necessary to establish an efficient strategy to manage soil salinity and confront economic challenges that arise from it.Saline soil recovery involving drainage of shallow saline groundwater and the removal of soil salts by natural rainfall or by irrigation are good strategies for the reclamation of salty soil.To develop suitable management strategies for salty soil reclamation,it is essential to improve soil salinity assessment pro cess/mechanism and to adopt new approaches and techniques.T his study mapped a recovered area of 7200 m2 to assess and verify variations in soil salinity in space and time in K airouan region in Central Tunisia,taking into account the thickness of soil materials.Two electromagnetic conductivity meters(EM38 and EM31)were used to measure the electrical conductivity of saturated soil-paste extract(ECe)and apparent electrical conductivity(E Ca).Multiple linear regression was established between ECe and ECa,and it was revealed that ECa-EM38 is optimal for E Ce prediction in the surface soils.Salinity maps demonstrated that the spatial structure of soil salinity in the region of interest was relatively unchanged but varied temporally.Variation in salinity at the soil surface was greater than that at a depth.These findings can not only be used to track soil salinity variations and their significance in the field but also help to identify the spatial and temporal features of soil salinity,thus improving the efficiency of soil management.     

外源脱落酸对抗寒性狗牙根抗氧化酶活性的影响

以寒敏感的普通狗牙根、海岸狗牙根和抗寒的新农1号狗牙根、喀什狗牙根为供试材料,研究外源脱落酸（0 mg•L^-1、5 mg•L^-1、15 mg•L^-1、25 mg•L^-1）在4 ℃低温处理下（处理时间24 h、72 h）对叶片相对电导率（EC）、丙二醛（MDA）含量、超氧化物歧化酶（SOD）活性、过氧化氢酶（CAT）活性、过氧化物酶（POD）活性的影响。结果表明：与CK2（喷水、常温培养）相比,4 ℃低温处理24 h、72 h,无论是否喷施外源脱落酸,狗牙根均表现为[WTBX]EC[WTBZ]增大,MDA含量增加;但与CK1（喷水、4 ℃低温处理）相比,喷施外源脱落酸可以诱导狗牙根细胞EC、MDA含量降低,促进SOD活性、POD活性、CAT活性的进一步增加,保护膜系统的完整性,增强其对低温的适应。综合分析认为,抗寒狗牙根的适宜外源脱落酸喷施浓度为15 mg•L-1,寒敏感狗牙根为5 mg•L^-1更有利于其对低温的适应。随着低温处理时间的延长,抗寒狗牙根SOD活性增加率、MDA含量降低率明显高于寒敏感狗牙根,说明SOD酶活性不同可能是狗牙根抗寒性差异的原因之一。     

德系安哥拉兔的生长特性

德系安哥拉兔不仅以产毛量高、毛质好而著称,而且有生长迅速、体成熟早、体型大的特点。六月龄时已达成年体重的87.37％。母兔的初配可在此时进行,公兔可延迟一个月配种。四月龄与六月龄体重和成年体重的相关系数分别为0.505与0.508,这为德系安哥拉兔体重的早期选择提供了有利时机。     

数显式豆浆总固形物含量检测仪设计与试验

为了给豆浆总固形物含量的检测提供一种简单、便捷的仪器,首先研究了豆浆的总固形物含量(2.13~6.50 g/(100 m L))和温度(20~70℃)对其电导率的影响规律。结果说明,豆浆的电导率随总固形物含量和温度的增大而增大,可用二元二次模型表达豆浆的电导率与总固形物含量、温度的关系,该模型的决定系数为0.994。进而设计了以STC12C5A16S2单片机为控制器、以DJS-1型电导电极为电导率传感器、以DS18B20为温度传感器、以锂电池供电的便携式豆浆总固形物含量检测仪硬件系统。用C51语言设计了检测仪的软件,实现了数据的采集、处理和显示。对该检测仪的检验结果说明,当总固形物质量浓度在2.00~8.00 g/(100 m L)范围内时,该检测仪的总固形物含量测量误差为-0.52~0.37 g/(100 m L),平均绝对误差为0.17 g/(100 m L),响应时间小于5 s。     

应用电导仪测定番茄灰霉病菌对多菌灵抗药性的初步研究

1.0 mg/L和5.0 mg/L多菌灵盐酸盐溶液处理灰霉病菌多菌灵敏感菌株和抗性菌丝体,用电导仪测定溶液电导率的动态变化,结果表明:在敏感菌株存在时,多菌灵盐酸盐溶液2 h后的电导率显著降低,而抗性菌株存在的溶液中电导率则未见下降。     

Comparison and sensitivity of measurement techniques for spatial distribution of soil salinity

In Khorezm, a district of Uzbekistan situated in the Aral Sea Basin, soil salinization is an important driver of soil degradation in irrigated agriculture. The main objective of this study was to identify techniques that enable rapid estimation of soil salinity. Therefore, bulk electrical conductivity of the soil (EC_a-meas) was measured with three different devices (2P, 4P, and CM-138) and electrical conductivity of the soil paste (EC_p-meas) was measured with the so-called 2XP device. These measurements were compared with independent estimates of EC_a-calc and EC_p-calc based on laboratory measurements of the saturated extract, EC_e, of soil samples from the same sites. Soil salinity could be assessed satisfactorily with all four devices. EC_p-meas could be well reproduced by the 2XP device (R ² = 0.76), whereas EC_a-meas estimates using 2P, 4P, and CM-138 in the field were less accurate (R ² < 0.50). The sensitivity of all devices to the main ions Cl⁻ and Ca^{2 +} suggests that the measuring principles are similar for all instruments. The devices can therefore be used interchangeably. Field assessment of soil salinity was considerably enhanced by the use of CM-138, because large areas can be quickly assessed, which may be desirable in spite of the lower accuracy.