用GSVAT模型研究地表/大气界面传输

用麦男水分和能量平衡资料验证了包括地下水的土壤－植被－大气水热传输模型（ＧＳＶＡＴ）,结果显示,模型能较好地模拟地表／大气水热传输特征,以及土壤水分的动态变化。通过敏感性分析,探讨叶／气界面,土壤／空气界面的节水调控效应,结果发现这两个界面对水汽传输的交互影响显著,若同时增加它们的水汽传输阻力,节水效果尤其明显。     

喀斯特坡地基岩起伏对土壤剖面水分格局的影响

研究了喀斯特地区典型坡地3条人工开挖样沟(投影长21 m、宽1 m)的岩土结构特征、土壤剖面平均含水量和土岩界面含水量沿坡面向下的变化趋势,探讨了喀斯特坡地基岩起伏对土壤水分格局的影响.结果表明: 喀斯特坡地地表地形与基岩地形不一致,基岩深度变异系数最大为82%,基岩起伏较大.基岩起伏程度明显影响到土壤剖面水分分布格局: 基岩起伏较小时,土壤含水量呈上坡位至下坡位逐渐增加的趋势,且土壤剖面平均含水量和土岩界面含水量与基岩深度相关性均不显著;基岩起伏越大,土壤含水量沿坡向下线性增加的趋势越不明显,土壤水分空间连续性越差,基岩凹陷、裂隙处土壤含水量较高,土壤剖面平均含水量和土岩界面含水量与基岩深度呈极显著正相关,但后者对基岩起伏的响应更明显.     

湘南红壤丘陵区不同生态种植模式下土壤磷素流失特征

以湖南省祁阳县红壤坡地大型标准径流场为例,研究了湘南红壤丘陵区8种不同生态种植模式下土壤磷素的地表流失特征.结果表明: 总磷流失量以撂荒处理(T₁)最严重,顺坡种植模式处理(T₂、T₃)其次,5种梯田模式处理(T₄～T₈)均能有效减少土壤磷的流失,磷流失量分别是T₁处理的9.9%、37%、0.7%、2.3%和1.9%.生态种植模式直接影响红壤坡地土壤磷素的地表流失形态,研究区流失的磷素以颗粒磷为主.暴雨(日降雨量＞50 mm)情况下,降雨量对不同生态种植模式下磷流失量影响差异不大,但磷流失量随降雨强度增大而增加.红壤坡地土壤磷素地表流失主要集中在6-9月,降雨量和降雨强度是影响湘南红壤丘陵区土壤磷素地表流失时间分布的直接因素.
     

茶园间植乌桕的气候生态效应

在安徽省黄山地区的红壤上,研究了茶园种植乌桕树对改善小气候环境的效应。夏秋季借助乌桕树稀疏的林冠为茶树遮荫,茶树-乌桕间植茶园的太阳总辐射低于茶树的光饱和点,其散射辐射比普通纯茶园增加,散射辐射与直接辐射的比率高达0.78-0.90,气温及湿度得到调节,宜于茶树正常生长;茶树及乌桕树的根系分别从浅层及深层吸收土壤水分,提高了土壤水的利用率。因此,茶园间植乌桕可减轻夏季热旱危害茶树生长,提高茶叶产量和品质,是江南茶区生产优质绿茶的一种人工生态模式。     

基于稳定同位素的干旱半干旱区SPAC水分运移过程研究进展

土壤-植物-大气连续体(SPAC)是生态水文学的重点研究对象,其水分运移过程对于干旱半干旱区生态植被建设和水资源综合管理具有重要意义。氢氧稳定同位素较高的灵敏性和准确度有助于揭示这一过程。介绍了氢氧稳定同位素在土壤-大气界面、土壤-地下水界面、土壤-植物界面和植物-大气界面水分补给传输过程中的应用,包括土壤水分来源和蒸发;水分补给入渗机制和滞留时间;植物水分来源和水力再分配;蒸散发分割和叶片吸水的相关研究,同时明确了氢氧稳定同位素技术在应用过程中存在的一些不确定性以及未来亟需加强的方面,以期为利用稳定同位素技术对生态水文过程的研究提供参考依据。     

稻草覆盖对红壤丘陵茶园的生态调控效应

在红壤丘陵区幼龄茶园通过连续4年稻草覆盖的大田试验,研究了稻草覆盖对茶园的生态综合调控效应。结果表明,稻草覆盖改良了土壤理化性状,提高了茶树生长时期(3~10月)的土壤水分含量,特别是土壤表层(0~20 cm)的水分含量;缓冲了茶园土壤温度变化;抑制了茶园杂草的生长;增加了蜘蛛等天敌的数量,有效地控制了假眼小绿叶蝉和茶蚜虫等害虫数量,但茶尺蠖显著增加;有利于蚯蚓的生长,改善了茶园生态环境。     

干旱区包气带土壤水分运移能量关系及驱动力研究评述

包气带土壤能量和水分平衡及其驱动因子是维系地下水-土壤-植物-大气连续体(GSPAC)系统中水分运移发生的关键因素。在降水稀少、水资源短缺的干旱地区,开展包气带土壤水分形态、运移过程与能量的耦合规律研究对揭示区域水资源形成和转化机理具有极其重要的现实意义。文章总结了土壤水分运移理论研究进展,探讨了水分参与水文循环过程及干旱环境下土壤水分可能表现形态及其降雨入渗、再分布、渗漏、蒸发、毛管水上升等过程驱动机制,评述了包气带土壤水分与能量过程在不同空间尺度上生态水分效应。在一个非饱和土壤系统中,水分运移受包气带结构,土壤物理特征,植物根系和土壤生化环境的综合控制,物质和能量平衡改变是驱动水分循环的源动力,而土壤环境变化是导致水分运移形态的发生变化根本原因。因此,在气候变化背景下,研究干旱区土壤与大气界面以及包气带与饱和带界面水、汽、热耦合转化形式与能量驱动过程,能够提升我们对包气带土壤水分运移规律机理的深入理解,丰富对区域气候和水文变化认知。为干旱区生态植被恢复建设和水资源精细化管理提供理论向导。     

稳定同位素在干旱区水分传输过程的研究进展

景观内部地下水-土壤-植物-大气界面的水分传输和不同景观界面间的水力联系是干旱区生态水文学研究的理论基础, 对提高认识不同景观格局水文连通性具有重要意义。鉴于干旱区水分循环的复杂性, 稳定同位素(δ2H、δ18O)在干旱区生态系统水分传输研究中广泛应用。综述了稳定同位素在干旱区植物/土壤-大气界面水分转换、植物根系-土壤界面水力联系与根系吸水过程和土壤水-地下水相互作用方面的研究。提出未来研究发展方向: 加强对干旱区非稳态条件蒸散发同位素量化; 优化不同生境植物根系吸水的同位素模型; 基于区域地下水-土壤-植被长时间序列同位素观测, 阐明干旱区不同景观界面间的水力连通性机制。     

南方东部丘陵区季节性干旱成因及其对策研究

本文着重从气候和土壤两方面探讨红壤丘陵区土壤季节性干旱的成因。研究结果表明,红壤特殊的水分物理性质和该区特定的大气－土壤－植物系统水分运动模式的综合作用是红壤季节性干旱的主要成因。认为丘陵红壤的土壤水分管理应从土壤结构改良和协调气候－土壤关系两方面入手,通过合理的耕作技术和建立合理的利用方式体系,改良土壤结构,利用深层土壤水分,从而达到提高土壤水分利用率和抗旱、避旱的目的。复合农林业和免耕覆盖技术对红壤水分具有显著的调节作用。     

基于SPAC系统干旱区水分循环和水分来源研究方法综述

土壤-植物-大气连续体(SPAC)是研究植物水分利用与循环的核心,研究其水分传输过程对于旱区植被恢复具有重要指导意义.本文从土壤水分和植物蒸腾两个方面进行阐述,对土壤水分的研究主要涉及热惯量法、中子仪法和时域反射仪法,植物蒸腾则从枝叶尺度、单木尺度、林分尺度和区域尺度4个层面分类总结;并重点介绍了稳定同位素方法在研究植物不同水分来源中的应用.     

Litterfall and litter accumulation in red alder stands in western Oregon

Summary Litter production in red alder communities 2 to 33 years old was higher than that reported for any plant community of the temperate regions. Litter production is also atypically high in communities of other nitrogen fixers, which suggests that nitrogen fixation may be an important contribution to the high litter production. Litter accumulates rapidly on the ground during the first 5 years after red alder establishment, but equilibrium is reached at the age of 6 years and maintained for several decades. During this time, the decomposition of litter equals the annual litterfall. In 50 years, cumulative litterfall reaches over 300 metric tons per ha, most of which is decomposed and incorporated into mineral soil. Favorable physical, chemical, and nutritional conditions of soil are created by alder for development of the climax vegetation. Paper No.733.     

红壤生态学

红壤是一种重要类型的土壤,面积大、分布广,条件优越,开发利用潜力巨大。当前,红壤退化严重、生态环境问题突出,亟待研究治理。建立红壤生态学,将红壤生态学的理论与技术运用到红壤的生态治理、环境改善及其合理开发利用中,既是现实需要又是形势所迫,势在必行。红壤生态学是由土壤学与生态学交叉、复合而形成的一门新兴、边缘农业应用科学,是土壤生态学的一个分支学科。红壤生态学以红壤为研究对象,探索红壤生态系统中生物与生物、生物与环境、环境因子与环境因子之间的相互关系及其作用机理,深入揭示红壤生态系统的结构、功能、演变规律及调控措施,最终目标是要实现红壤资源的可持续利用和红壤生态系统的可持续发展。红壤生态学着重研究以下7个方面的内容:(1)红壤生态系统的结构;(2)红壤生态系统的功能;(3)红壤生态系统的演变;(4)红壤生态系统的退化;(5)红壤生态系统的平衡;(6)红壤生态系统的调控;(7)红壤资源的开发利用。红壤生态学具有以下几个明显的特征:交叉性与边缘性、复合性与综合性、实践性与应用性、理论性与学术性、多样性与复杂性、层次性与系统性,以及长期性与战略性。今后,红壤生态学将向着规范化、数字化、高效化、国际化方向发展。为促进红壤生态学的又好又快发展,应采取以下战略对策:一是培养专门人才;二是增加物质投入;三是建设研发平台;四是加强交流合作;五是勇于开拓创新。     

我国金花茶组植物的地理分布

世界产金花茶组植物22种,其中我国20种,特有18种,仅产广西。其分布区在北纬21°30′—23°40′,东经106°40′—108°35′,北界基本上与广西北热带半常绿季雨林、湿润雨林地带北界吻合。该组植物分布于石灰(岩)土的13种,红壤的7种。它们出现的地段比较固定,天然林下,沟谷或溪边处,相对高度10—15米;峰丛圆洼地底部和荫蔽的坡面下部。该组植物个体最多的地区(几何中心)一个在防城县,一个在龙州县;种类最多的地区(最大变异中心)一个也在龙州县,9种,一个在扶绥县,7种。该分布区从南到北分化成六个小分区。其垂直分布一般在海拔700米以下。水平分布种的更替表现为:北纬21°31′为小瓣金花茶等五种;北纬22°10′—22°45′为鼻岗金花茶等八种更替;北纬22°50′为顶生金花茶等三种更替;北纬23°40′为平果金花茶更替。金花茶分布幅度最宽,可由北纬21°31′到22°55′。在土山,东西以东经107°30′为界,以东为金花茶等四种,以西为小瓣金花茶等二种。     

桂西北典型喀斯特区生态服务价值的环境响应及其空间尺度特征

Study on ecosystem service values (ESVs) is the bridge of understanding ecosystem and economic decision-making. To investigate the response of ESVs to ambient environment and their spatial scales is an urgent work in the process of ecological restoration and sustainable development in southwest China. Based on the previous research results, the remote images, and weather data of 31 years (1975-2005), the response of ESVs to ambient environment and their spatial scales in a typical karst area of northwest Guangxi, China were evaluated with the method of empirical mode decomposition (EMD) in this paper. The results showed that ESVs had obvious variations with changes in elevation, rocky types and soil types, and had corresponding characteristics of spatial scales. The ESVs in middle and low elevation areas were higher, but they decreased due to human activities such as deforestation. The ESVs in peak-cluster depression areas were lower, and they would increase as influenced by policies such as returning farmland to forestland. The ESVs were influenced by rocky types, showing lower values but an increasing trend in the typical karst regions while higher values but a decreasing trend in non-karst regions. The average ESVs in the west part of the study region, which is not only the main nature reserve for rare wildlife species in Guangxi, but also one of the best preserved natural vegetation regions in China, were more than 15,000 RMB Yuan ha-1,. Comparatively, the ESVs were less than 10,000 Yuan ha-1 in the middle part of the region attributed to low vegetation coverage, serious peak-cluster depression and karst rocky desertification. After about 20 years, that is from 1985 to 2005, the ecosystem conditions had been improved and the ESVs had increased in the middle and eastern part of this study region. On the contrary, in most western part, which was dominated by subtropical evergreen broad-leaved forest, they had been worsened, and the balance values of ESVs were negative. As for the relationships of ESVs with rocky types and soil types, lime soil and red soil were the two main soil types that contributed to ESVs (The total contribution was above 60%, and it is 63.77%,64.37%,64.56%,64.91% respectively in the four years of 1985, 1990, 2000 and 2005.). The variance contribution of intrinsic mode function (IMF) and trend (R) showed that there were obvious special sales for ESVs in this study area, and the main spatial scales were about 2.7 km, 5.5 km, and 11.6 km. The variance contribution ratio was 12.29%, 11.26%, 11.49% respectively, and the trend (R) was high (17.74%). In conclusion, this study indicated that ecosystem conditions in the typical karst area were improved owing to the application of rocky desertification control policies, such as ecological migration and returning farmland to forestland. Besides, the main spatial scales of ESVs in the study area were the interactions of terrain, physiognomy, land use / land cover and human activities.     

红壤丘陵区生态农业模式研究

根据不同坡位上红壤的理化性质分异,建议在红壤丘陵上推行“顶林、谷农、塘渔”生态农业模式。并在塘边建造猪场,以养猪为纽带,实行种养结合,建立饲草－猪－沼、菇－果、粮－果、珍珠的食物链,再定量调控种养结合链环的饲料配置,粪尿投放、制沼育菇和塘淤返田,以提高系统生产力,达到农业可持续发展。     

黄土丘陵区三种典型土壤地类造林技术

中国黄土高原丘陵沟壑区是世界上水土流失最严重的区域之一,由于长期水土流失的侵蚀切割作用,表层土壤流失殆尽,黄绵土母质、红胶泥土以及土壤与岩石过渡类型--风化岩沫土等土壤类型依次裸露了出来,形成了3种典型的土壤地类,增加了造林的难度.由于红胶泥与风化岩沫土土壤瘠薄,当地林业部门认为这两种土壤地类不能造林,因此,传统造林只在黄棉土进行.为此,提出了＂适土适树,因土制宜＂的造林原则和＂穴衬膜栽植技术＂,以扩大适宜造林的土壤类型.穴衬膜栽植技术是指树木栽植时,在挖好的栽树坑底部和四周衬贴一层防渗薄膜（厚度为0.0007 mm可降解塑料薄膜）,树木栽好覆土浇水后,再在地表面覆膜,防止栽树浇水（施肥）的渗漏和蒸发,使树根在较长时间内处于含水量较高、四周封闭的潮湿土壤之中,从而达到提高成活率和促进林木前期生长的目的.1997～2001年,我们在黄土丘陵区陕西省延安市下砭沟小流域采用田间对比试验法进行了5年试验,结果表明,穴衬膜栽植技术促进浅层根系的生长发育,保水作用可持续4个月以上,对各种树木成活率和生长量均有显著促进作用,在黄土丘陵地区这3种土壤地类采用穴衬膜栽植技术可达到良好的造林效果,特别是红胶泥和风化岩沫土地类主要位于沟谷两岸,地下水供给较为充裕,是浅根性植物生长发育的良好土壤类型,科学混交可获得更好效果.     

红壤旱地不同复种方式的生态功能评价

为了充分发挥红壤旱地的生态功能,筛选出适于红壤旱地的优化复种方式,依据3年的田间定位试验资料,从农田生态系统的生产功能、物质循环特征、能量流动特征、价值流动特征以及养地效果等方面对红壤旱地4种复种方式[处理A(CK): 小麦/大豆-芝麻;处理B: 混播绿肥(油菜×紫云英×肥田萝卜)-大豆‖玉米-绿豆‖芝麻;处理C: 黑麦草-花生‖玉米-粟‖荞麦;处理D: 油菜-绿豆‖甘薯,“/”表示套作,“‖”表示间作,“-”表示接茬,“×”表示混作]的功能和效益进行了分析,并采用灰色关联度法从经济效益、生态效益和社会效益3个层次的13个指标对各复种方式进行了综合评价.结果表明: 混播绿肥(油菜×紫云英×肥田萝卜)-大豆‖玉米-绿豆‖芝麻复种模式的经济效益、生态效益和社会效益的关联度值均居第一位,经灰色关联度分析,得出其综合效益关联度值也最高,为0.847,是比较适宜在红壤旱地推广应用的高效复种方式,对今后红壤旱作区种植业结构布局和优化具有积极意义.     

Screening of arbuscular mycorrhizal fungi for the revegetation of eroded red soils in subtropical China

Some acidic red soils in hilly regions of subtropical China were degraded as a result of slope erosion following the removal of natural vegetation, primarily for fuel. Revegetation is important for the recovery of the degraded ecosystem, but plant growth is limited by the low fertility of eroded sites. One factor contributing to the low fertility may be low inoculum density of arbuscular mycorrhizal (AM) fungi. Compared to red soils under natural vegetation or in agricultural production, substrates on eroded sites had significantly lower AM fungal propagule densities. Thus, the management and/or application of AM fungi may increase plant growth and accelerate revegetation. Thirteen species of AM fungi were identified in red soils by spore morphology. Scutellospora heterogama, Glomus manihotis, Gigaspora margarita, Glomus aggregatum and Acaulospora laevis were among the most common according to spore numbers. Pot cultures were used to isolate and propagate 14 isolates of AM fungi indigenous to red soil. The effectiveness of each fungus in promotion of growth of mungbean was evaluated in red soil. For comparison, three isolates from northern China, known to be highly effective in neutral soils, and two isolates from Australia, known to be from acidic soil were used. Effectiveness was positively related to root infection (r ² = 0.601). For two of these isolates, Glomus caledonium (isolated from northern China) and Glomus manihotis (an isolate indigenous to red soil), the applied P concentration giving the highest infection and response to infection was approximately 17.5 mg P kg^–1 soil. In field experiments in which this concentration of P was applied, the five most effective isolates were tested on mungbean. The Glomus caledonium isolate from northern China was the most effective, followed by the indigenous Glomus manihotis isolate. The Glomus caledonium isolate was also shown to be effective on Lespedeza formosa, which is commonly used in revegetation efforts. We conclude that inoculation of plants with selected isolates of AM fungi may aid in revegetation efforts on eroded red soils in subtropical China.     

Echinococcus multilocularis in the red fox Vulpes vulpes from the East Carpathian region of Poland and the Slovak Republic

The occurrence of Echinococcus multilocularis in the Poland-Slovak frontier zone of the East Carpathian region was assessed, for comparison with that in adjacent regions in both countries. A total of 392 red foxes from Poland and 427 red foxes from the Slovak Republic were examined from 2001 to 2004. Significant differences in prevalences were observed in foxes captured from the borderland and adjacent zones in both countries. The mean prevalence of E. multilocularis in the Polish borderland reached 45.7+/-18.6% and in the Slovak border 35.0+/-10.7%. In both countries, the prevalence of E. multilocularis in red foxes from adjacent districts, outside the frontier Carpathian region, was considerably lower (18.9+/-9.2% in Poland and 20.8+/-9.0% in Slovakia). These differences are probably due to geomorphological and ecological factors, which contribute to the survival of the tapeworm eggs and the subsequent spread of infection. The Carpathian regions of northeast Slovakia and southeast Poland are characterized by specific climatic conditions such as low mean annual air temperatures, low temperatures in active soil surfaces, high soil humidities and a high mean annual rainfall.