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.     

奶牛胎儿的父亲对母亲产奶量的影响

用中国黑白花奶牛研究了胎儿的父亲及犊牛初生重对母亲当胎及下一个泌乳期产奶量的影响,结果指出胎儿的父亲对母亲当胎及下一个泌乳期90天和305天的产奶量,都有极显著的影响,各占产奶总变异量的9.4％,15.3％及3.77％(P<0.01)。犊牛初生重对母亲产奶量的影响也显著(P<0.05)。当根据公牛的产奶预期差(PDM)将胎儿的父亲分为两组后,发现差异显著(P<0.05),胎儿父亲的PDM高,胎儿母亲的产奶量也高,因此胎儿母亲产奶量不仅受胎儿重量的影响,也受父亲PDM的影响。     

可控止回阀水力特性的测试研究

本文运用水流相似原理，对可控止回阀的流阻系数曲线和动水力矩，进行了系统的水力模型试验研究，为该阀的节能效益和技术开发的可行性，提供了必要的科学依据，其流阻系数值为０．１９，优于液控蝶阀。     

灌水量对不同类型晚稻生育及产量影响的初步研究

采取盆栽遮雨人工定量灌水的方法,探讨了常规晚稻和杂交晚稻前后两大生育时期不同灌水量对生育和产量的影响.结果表明:两类型晚稻品种前后两个生育时期节水灌溉都能达到高产之目的,但不同类型和不同生育时期的最佳灌水量和节水效果不同.     

51个木麻黄地理种源对星天牛抗虫序列的调查研究

本文报道51个木麻黄(Casuarina spp.)地理种源对星天牛(Anoplophora chinensis(Forster))抗性调查和分析的结果。调查获得数据应用IBM—PC计算机进行逐步聚类分析,将51个木麻黄地理种源划分为高感、中抗、高抗和绝抗4个类群,并进行方差分析,结果表明4个类群木麻黄对星天牛的抗性达极显著差异,因此在星天牛发生严重地区可以选择既抗虫、又抗风,生长较好的C_(33)、C_(39)、C_(44)等种源造林。     

土壤生物量-碳和-氮与土壤有机碳、氮及施肥的关系

应用氯仿熏蒸培养法测定不同肥力水平的土壤生物量-C 和-N。结果表明:士壤生物量-C 与土壤有机碳的相关性达到极显著水准;用6mol/L HCl 水解的总氮量与土壤全氮也有很好的相关性,但与生物量-N 则不然;生物量-N 与酸解的氨基酸态氮及未知态氮都有显著相关性。施肥显著提高土壤生物量-C 和-N,有机无机肥料配合施用的大于单施化肥的。     

保定市工业废水农灌的研究

本文论述了保定市工业废水经农灌土地处理,对土壤、地下水和农作物品质的影响。结果表明:以造纸、食品、轻纺和化工为主的工业废水在重金属常年不超出农灌标准下,宜于在非盐化土壤灌溉;废水中硫化物超标,通过土壤生物区系,能降低毒性;废水中常规有机物,农灌后利大于害;只要在土壤容量允许内,可具有二级污水处理工艺不能完成的效果。     

应用积分GM(1,1)模型进行杉木炭疽病预测预报的研究

以积分生成代替传统的累加生成方法 ,并用双向差分建立积分GM (1,1)灰色预测模型进行杉木炭疽病预测预报的研究 ,结果表明积分GM (1,1)模型能较好地预测杉木炭疽病在三明市的发生     

柳沟灌区的盐碱土改良

农七师车排子垦区柳沟灌区,原有柳沟一、二、三场,面积59万余亩。由于盐碱危害,生产状况和经济状况日益恶化,难以自立。在60年代初,与原25团合并,成为现今的125团的三个营,近年来进行大规模的盐碱土改良工作,取得了显著的效果。基本情况改良效果的观测主要在二营(原柳沟三场)进行,二营面积10.67万亩,可耕地8.85万亩,位于灌区南部、天山北麓,奎屯河与四棵树之间。区内由南向北倾斜,地势低平,坡降1-3‰,土壤多为粉粒中壤和重壤,1-2米以下,广泛分布着红棕色粘土层,因而地下水迳流呈封闭状态,极其不畅,主要靠地面蒸发和植物蒸腾维持平衡。地下水埋深1-1.5米;低洼区接近地面。矿化度20-30克/升,最高达88.45克/升。高矿化与高水位成为土壤盐渍化迅速发展的根本原因。