城市拆迁空地对城市绿化率的影响

近年来,我国城市建设发展迅速,产生了大量的拆迁空地,就拆迁空地对城市绿化率的影响进行了定量的研究,并提出相应的对策。     

Compatible measurements of volumetric soil water content using a neutron probe and Diviner 2000 after field calibration

Field calibrations for a neutron probe and a capacitance sensor (Diviner 2000) for measuring the soil water content of a shrinking–swelling clay soil were substantially different from commonly used default values. Using our field calibrations, the two instruments estimated similar changes in the cumulative water content of a soil profile (0–1 m depth) over one growing season.     

退耕还林间作万寿菊的高产栽培技术

本文介绍了万寿菊的形态特征及生物学特性,根据形态特征及生物学特性,探索了万寿菊的育苗技术和栽培技术以及田间管理的方法。     

建设新农村的重要举措:加强村级班子建设,努力推进依法治村

认真解决好依法治村问题,是建设新农村的重要举措。本文试从加强村级班子建设的角度,探讨新农村建设,推进依法治村的一些问题。     

新疆水土保持情况调查

新疆水土保持情况调查郭廷辅，佟伟力（水利部水土保持司，北京１００７６１）我们于１９９４年８月１１日至２６日对新疆伊犁、和田、喀什、吐鲁番、昌吉、乌鲁木齐等６个地区（州、市）的１１个县（市）、两个流域的水土流失情况和开展治理工作做了典型调查。同时，也对...     

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.     

猴头菌新菌株宁猴6号的选育初报

采用多孢分离技术产生多个新组合 ,经驯化筛选获得猴头新菌株宁猴 6号 ,宁猴 6号为适合用针叶林木屑物料栽培的新菌株。生物学特性表明 :猴头菌宁猴 6号菌丝生长适温 2 5～ 2 8℃ ,子实体生长适温 15～2 0℃ ,菌丝生长期短 ,36～ 4 0d长满瓶底 ,栽培袋在常温下培养 4 3～ 5 0d菌丝满袋。室内栽培生物学效率达5 6 .0 0 % ,室外栽培生物学效率达 6 1.4 0 % ,子实体中型匀称近球型 ,柄短或无柄 ,刺长 0 .9～ 2 .2cm。宁猴 6号不仅适于阔叶木屑栽培 ,最突出的是适应针叶林木屑栽培     

试论含氯化肥的合理施用

根据氯对作物和土壤的影响,表明南方可以在各种作物的耐氯极限内施用含氯化肥,并需配合施用石灰和含钙磷肥;而北方旱区,特别是西北地区合理施用含氯化肥应根据每茬作物吸收带走的氯量,确定一个轮作周期内施用含氯化肥的量,保持土壤氯素的平衡,不致使土壤盐渍化。氯化铵可以就近施用,缺钾作物也能以含氯钾肥予以补充。此即本文所述氮素平衡施肥原理。     

水牛牛巴贝斯虫体外培养的研究：Ⅱ.冷冻血清的应用和筛选

应用冷冻血清对１株采自自然感染的水牛牛巴贝斯虫进行了长达７２ｄ的体外连续培养，共继代２０次，培养７２ｈ红细胞染虫率最高达１４．１％，平均为８％～１０％。培养２０ｄ和３０ｄ的牛巴贝斯虫经液氮保存复苏后，接种于去脾水牛犊均引发了严重的牛巴贝斯虫病，从而说明已建立了水牛牛巴贝斯虫的体外连续培养，且经培养后的牛巴贝斯虫致病力没有改变。本试验利用６头份的冷冻健康水牛血清同时进行培养，结果发现，并非所有的健康水牛血清均适合于体外培养牛巴贝斯虫。这一发现对建立水牛牛巴贝斯虫的体外培养和研究水牛牛巴贝斯虫病均具有重要意义     

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。