南方山丘水库种草养鱼防淤减积综合利用的研究

在长沙县百倍冲水库进行多年的试验研究结果表明,开发利用库内长期荒芜的大片消落区种植黑麦草;荒山堤坝上种植扁穗牛鞭草、岸杂一号狗牙根、皇草、幼林间种植鸡脚草、拉丁鲁白三叶等饲草配套养鱼和防止水土流失、防淤减积试验获得成功。库内鲜鱼产量由种草前常年1000kg提高到7000～8000kg,泥砂淤积量每年减少0.516×104m3,经济生态效益显著。     

Soil and water loss in the Lancang River-Mekong River watershed (in Yunnan section, China) and its control measures

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污染生态学的新发展—污染进化生态学

污染胁迫的最显著效应是消除敏感物种或个体，导致植物居群进化。突变是进化的原料，选择是进化的手段，隔离是进化的条件，控制抗性性状的基因因物种及污染物的种类不同而异，但也会出现植物同时具有对某两种或几种污染物的抗性，即所谓协同抗性；污染除使植物衰退外，还可能导致一些遗传信息丧失，使抗性种群内物种单一，降低其适合度，对其它环境胁迫因素的抵抗力下降，即所谓适应代价。     

热镀锌板表面钝化时的磷化工艺

热镀锌板表面钝化（铬酸盐钝化），主要是为了防止在使用过程中其表面被氧化。由于表面的钝化膜的存在。使得磷化工艺无法进行，从而影响涂装后涂层的附着力（铬酸盐钝化膜不如磷化膜附着性好）和耐蚀性能（铬离子不耐氯离子的腐蚀）。为了提高热镀锌板表面钝化后其表面的涂装性能，开发出一种适合上述条件的磷化工艺。     

全国土壤侵蚀量估算及其在吸附态氮磷流失量匡算中的应用

应用土壤流失方程(USLE),根据我国土壤水力侵蚀分类分级标准,建立了大尺度区域土壤侵蚀量的估算模型;基于GIS技术平台,利用土壤普查数据,构建了全国表层土壤氮磷含量数据库,完成了2000年全国境内水土流失影响下吸附态氮磷的流失量估算.经数据合理性分析验证后得出以下结论:(1)全国因水土流失引发的吸附态氮素和磷素的流失总量分别达到104.22×104t和34.65×104t;(2)长江、珠江和黄河三大流域的吸附态氮、磷流失量之和分别占全国总量的83%和89%,单位面积(1km2)吸附态氮、磷的流失量分别介于6.0×10-4～0.53t和2.1×10-4～0.13t之间;(3)吸附态氮的重点流失区主要分布在长江中上游水土易蚀区、黄河中游沟壑区、西辽河上游区、珠江流域红水河、西江等上游区以及怒江、澜沧江下游区.     

COALBED METHANE PRODUCT WATER CHEMISTRY IN THREE WYOMING WATERSHEDS1

ABSTRACT: The Powder River Basin in Wyoming has become one of the most active areas of coalbed methane (CBM) development in the western United States. Extraction of methane from coalbeds requires pumping of aquifer water, which is called product water. Two to ten extraction wells are manifolded into one discharge point and product water is released into nearby unlined holding ponds. The objective of this study was to evaluate the chemistry, salinity, and sodicity of CBM product water at discharge points and associated holding ponds as a function of watershed. The product water samples from the discharge points and associated holding ponds were collected from the Cheyenne River (CHR), Belle Fourche River (BFR), and Little Powder River (LPR) watersheds during the summers of 1999 and 2000. These samples were analyzed for pH, electrical conductivity (EC), total dissolved solids (TDS), alkalinity, sodium (Na), calcium (Ca), magnesium (Mg), potassium (K), sulfate (SO₄^2‐), and chloride (C^1‐). From the chemical data, practical sodium adsorption ratio (SARp) and true sodium adsorption ratio (SARt) were calculated for the CBM discharge water and pond water. The pH, EC, TDS, alkalinity, Na, Ca, Mg, K, SARp, and SARt of CBM discharge water increased significantly moving north from the CHR watershed to the LPR watershed. CBM discharge water in associated holding ponds showed significant increases in EC, TDS, alkalinity, Na, K, SARp, and SARt moving north from the CHR to the LPR watershed. Within watersheds, the only significant change was an increase in pH from 7.21 to 8.26 between discharge points and holding ponds in the LPR watershed. However, the LPR and BFR exhibited larger changes in mean chemistry values in pH, salinity (EC, TDS), and sodicity (SAR) between CBM product water discharges and associated holding ponds than the CHR watershed. For instance, the mean EC and TDS of CBM product water in LPR increased from 1.93 to 2.09 dS/m, and froml,232 to 1,336 mg/L, respectively, between discharge and pond waters. The CHR exhibited no change in EC, TDS, Na, or SAR between discharge water and pond water. Also, while not statistically significant, mean alkalinity of CBM product water in BFR and LPR watersheds decreased from 9.81 to 8.01 meq/L and from 19.87 to 18.14 meq/L, respectively, between discharge and pond waters. The results of this study suggest that release of CBM product water onto the rangelands of BFR and LPR watersheds may precipitate calcium carbonate (CaCO₃) in soils, which in turn may decrease infiltration and increase runoff and erosion. Thus, use of CBM product water for irrigation in LPR and BFR watersheds may require careful planning based on water pH, EC, alkalinity, Na, and SAR, as well as local soil physical and chemical properties.     

真丝绸阻燃整理

综述了真丝绸燃烧性能及其阻燃整理的发展历史，总结了真丝绸的各种阻燃方法及具体工艺并对各种方法阻燃性能的优劣作了评价，归纳了真丝绸阻燃所用阻燃剂的种类及各类阻燃剂的作用机理，并指出目前真丝绸阻燃主要存在的问题以及今后的发展方向。     

NATURAL EROSION RATES AND THEIR PREDICTION IN THE IDAHO BATHOLITH1

ABSTRACT: Natural rates of surface erosion on forested granitic soils in central Idaho were measured in 40 m² bordered erosion plots over a period of four years. In addition, we measured a variety of site variables, soil properties, and summer rainstorm intensities in order to relate erosion rates to site attributes. Median winter erosion rates are approximately twice summer period rates, however mean summer rates are nearly twice winter rates because of infrequent high erosion caused by summer rainstorms. Regression equation models and regression tree models were constructed to explore relationships between erosion and factors that control erosion rates. Ground cover is the single factor that has the greatest influence on erosion rates during both summer and winter periods. Rainstorm intensity (erosivity index) strongly influences summer erosion rates, even on soils with high ground cover percentages. Few summer storms were of sufficient duration and intensity to cause rilling on the plots, and the data set was too small to elucidate differences in rill vs. interrill erosion. The regression tree models are relatively less biased than the regression equations developed, and explained 70 and 84 percent of the variability in summer and winter erosion rates, respectively.