In situ radiometric mapping of soil erosion and field-moist bulk density on cultivated fields

Abstract. Recent developments in in situγ ray spectrometry offer a new approach to measuring the activity of radionuclides such as ¹³⁷Cs and ⁴⁰K in soils, and thus estimating erosion or deposition rates and field moist bulk density (ρ_m). Such estimates would be rapid and involve minimal site disturbance, especially important where archaeological remains are present. This paper presents the results of a pilot investigation of an eroded field in Scotland in which a portable hyper pure germanium (HPGe) detector was used to measure γ ray spectra in situ. The gamma (γ) photon flux observed at the soil surface is a function of the ¹³⁷Cs inventory, its depth distribution characteristics and ρ_m. A coefficient, Q_Cs, derived from the forward scattering of ¹³⁷Cs γ ray photons within the soil profile relative to the ¹³⁷Cs full energy peak (662 keV), was used to correct the in situ calibration for changes in the ¹³⁷Cs vertical distribution in the ploughed field, a function of tillage, soil accumulation and ρ_m. Based on only 8 measurements, the agreement between in situγ ray spectrometry and soil sample measurements of ¹³⁷Cs inventories improved from a non significant r²=0.05 to a significant r²=0.62 (P<0.05). Erosion and deposition rates calculated from the corrected in situ¹³⁷Cs measurements had a similarly good agreement with those calculated from soil cores. Mean soil bulk density was also calculated using a separate coefficient, Q_K, derived from the forward scattering γ photons from ⁴⁰K within the soil relative to the ⁴⁰K full energy peak (1460 keV). Again there was good agreement with soil core measurements (r²=0.64; P<0.05). The precision of the in situ¹³⁷Cs measurement was limited by the precision with which Q_Cs can be estimated, a function of the low ¹³⁷Cs deposition levels associated with the weapons testing fallout and relatively low detector efficiency (35%). In contrast, the precision of the in situ ρ_m determination was only limited by the spatial variability associated with soil sampling.     

氧漂期间桦木硫酸盐纸浆表面性质变化的探讨

尝试性地应用ESCA对桦木硫酸盐浆氧漂期间表面性质的变化进行了初步分析。结果表明:桦木硫酸盐浆氧漂期间氧碳比逐渐增加,碳价态发生了显著的变化。这对于指导纸浆氧漂工艺条件的合理制定,预测或控制纸浆的宏观质量有非常重要作用。ESCA可为研究纸浆漂白提供新的有效手段。     

植物叶面铺展剂的复配规律Ⅰ.SDS和TX100混合水溶液体相及表面层相互作用行为

2种典型固体表面铺展剂SDS和TX100混合水溶液,无论在其表面层或在混合胶团中两组分之间均存在一定程度的相互作用,使得以廉价的SDS为主的溶液中加入少许TX100组成的复配体系表面活性提高,在植物叶面上的润湿性能改善,并从理论上计算了其相互作用参数,初步解释了实验现象,上述结果不仅对指导优良植物叶面铺展剂配方具有指导意义,也预示了潜在的实用价值.     

多花黑麦草播期试验(1987～1988年)

本试验研究了7个不同播期对多花黑麦草出苗、生产性能的影响.结果表明:在江西清江种草养畜试验站从8月中旬至11月中旬均可播种多花黑麦草,尤以9月中旬至10月中旬更为适宜.     

毛条灌木草场建立方法的研究

通过对毛条灌木林进行平茬，在人工灌溉条件下观测平茬毛条生物产量的变化，认为毛条平茬后具有很强的萌蘖能力，可产生原生枝条数4．1倍的萌生枝条；每年灌溉1次，灌水量1050m^3／hm^2，既可维持平茬毛条林的正常生长；在4株／m^2的密度条件下，平茬毛条的年产草量(干质量)可达538g／m^2，植被盖度可达78％以上，达到了经济效益和生态效益的共同提高；根据平茬毛条的生长变化规律，可初步确定冬春季节和夏季干旱时期为毛条灌木草场适宜的放牧时间。     

平潭县燕下埔沙荒风口综合治理试验初报

对燕下埔沙荒风口地段的综合治理试验结果表明：风口造林要取得成功，除了要采取必要的生物措施，更为重要的是应设置具有一定疏透度的风障以降低风沙危害，提高造林成活率。     

松嫩平原羊草草地水淹干扰恢复过程的群落动态

根据随机取样的测定数据，经过幂函数和多元回归分析及相关检验，揭示了草地水淹干扰对羊草 寸草苔、羊草 杂类草群范数量性状的变化规律。水淹干扰对草地植被的物种组成及其比例有明显的影响。水淹后基本恢复到正常草地的种类数量和生产量配置大约需要6—7年。随着生境水分减少和土壤变干，羊草种群的数量和生物量均以幂函数形式增加，而寸草苔和杂类草的数量和生物量则呈先增后降的变化过程。     

油罐阻油切水阀启动过程的研究

本文对油罐本安型阻油切水阀研制过程中的几个技术关键之一￣二次启动进行了较详细的力学分析，研究了阻油切水阀的启动过程，分析了启动过程中液体在静止和流动两种情况下对浮球工作的影响，提出了启动机构方案。