过刊目录

  • 2022年, 19卷, 第10期
    刊出日期:2024-06-19
      

  • 全选
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  • CHAI Le, ZHONG Cun-di, GUO Fu-sheng, HUANG Xin-shu, WANG Dao-ying, SHAO Chong-jian, CHEN Liu-qin
    2022, 19(10): 2743-2757.
    Granites of the Mesozoic Era are widespread in South China, and many of them have been shaped into spectacular landscapes with high tourism development values. However, the controlling factors and evolution stages of these granite landscapes were poorly understood. In this study, the Hypsometric Integral curves(HIc), and Hypsometric Integral(HI) values of the Mount Wugong were extracted from digital elevation model data in a geographic information system environment. The relationships between the HIc, HI values, and factors including the tectonism, lithology and climate of the study area were analyzed to determine the evolution of granite landscapes evolution in the main scenic areas of the Mount Wugongshan. The HI values on the northwestern and southeastern slopes of the Mount Wugongshan range from 0.223 to 0.415 and 0.385 to 0.465, respectively; the HIc are mainly concave on the northwestern slopes and irregularly ‘Sshaped' on the southeastern slopes. The main ridge of the granite geomorphic scenic area of the Mount Wugongshan, where the alpine meadow geomorphic landscape is located, is in the youthful stage of geomorphic evolution, the Mt. Jinding-Mt. Wanlong and Mt. Mingyue-Wentang scenic areas are in the old stage, and the Yangshimu scenic area is in the mature stage. Differences in watershed scale may be the main reason for the variabilities in geomorphic evolution in the area, while the regular development of tectonic phenomena is a key factor shaping the spatial variability in the watersheds on both sides of the main ridge.
  • ALTINO?LU Fatma Figen, POLAT Gulten
    2022, 19(10): 2758-2775.
    The parameter b(commonly referred to as the b-value) is one of the most significant seismic parameters to describe the seismicity of an investigated region. In this study, the structural framework of the Sar?g?l-Buldan region located in the intersection area of the western Anatolian graben system in Turkey was investigated by using seismicity and gravity data. As known, western Anatolia is one of the most seismically active regions of the Anatolian plate. Therefore, seismic activity in this region is very high. Analysis of the Bouguer gravity data enabled to define the shallow subsurface structure of the study area. Results from the gravity analysis indicated that the sediment basement depth varied from 0.1 km and 2.1 km. We also detected many NW-SE, E-W, and NESW trending lineaments that may be faults or fractures, and the NW-SE trending the Denizli basin lies to the east of the Ala?ehir basin. We observed that the findings from this analysis seem compatible with the regional geological trend. In addition to this, the seismicity of the region was analyzed by using the frequency-magnitude distribution to find out the seismic hazard risk. The most useful way in the analysis of the seismic hazard studies is to reveal the location of the earthquake boundary, which produces devastating big seismic events because such studies make it possible to forecast the location of possible future earthquakes and improve seismic hazard maps. The b-value for this study region was estimated by using the maximum likelihood method. Variations in the b-value were observed, which range from ≈ 0.2 to 2. A higher b-value was detected in the Buldan horst and surrounding area. In contrast to this, lower bvalues were observed in the northeast part of the interaction region between the Denizli and the Ala?ehir grabens. The positive Bouguer anomaly values as high as +10 m Gal and low b-values in the north-eastern part of the study region were interpreted as indicating a thinner crustal root. In comparison, negative Bouguer anomaly values were observed in the Alasehir and the Denizli grabens. Also, in these grabens, intermediate to high b-values were found. This suggests that there is a relation between gravity anomaly and b-value. This relation is strongly related to the normal faulting mechanism existing in the region.
  • HUANG Yun-xin, LIU Zheng-jia, LIU Yan-sui, LI Yu-rui, LIU Xue-qi
    2022, 19(10): 2776-2790.
    Increasing the quantity and improving the quality of cropland can alleviate the human-land contradiction and promote the sustainable development of agriculture especially in mountainous areas. With the support of the central government's policies, Yan'an, Northern Shaanxi, China implemented a major land consolidation engineering project in the loess hilly-gully region from 2013 to 2018, achieving 33,333.3 ha of new cropland. However, the poor quality of some newly-constructed cropland at the initial stage hindered its efficient utilization. In order to overcome this problem, red clay and Malan loess were compounded in different volume ratios to explore the method to improve the cropland quality. The Root Zone Water Quality Model was used to simulate the effects of different soil treatments on soil water, nitrogen and maize growth. Experimental data were collected from 2018 to 2019 to calibrate and validate the model. The root mean square error(RMSE) of soil water content, nitrate nitrogen concentration, above-ground biomass, leaf area index were in the range of 11.72-14.06 mm, 4.06-11.73 mg kg~(-1), 835.21-1151.28 kg ha~(-1) and 0.24-0.47, respectively, while the agreement index(d) between measured and simulated values ranged from 0.70 to 0.96. It was showed that, compared with land constructed with Malan loess only(T1), the soil structure and hydraulic characteristics of land with a volume ratio of red clay and Malan loess of 2:1(T3) was better. Simulation indicated that, compared with T1, the soil water content and available water content of T3 increased by 14.4% and 19.0%, respectively, while N leaching decreased by 16.9%. The aboveground biomass and maize yield of T3 were 7.9% and 6.7% higher than that of T1, respectively. Furthermore, the water productivity and nitrogen use efficiency of T3 increased by 21.0% and 16.6% compared with that of T1. These results indicated that compounding red clay and Malan loess in an appropriate ratio was an effective method to improve soil quality. This study provides a technical idea and specific technical parameters for the construction or improvement of cropland in loess hilly-gully region, which may also provide reference for similar projects in other places.
  • ZHAI Bo, DANG Xiao-hong, LIU Xiang-jie, WANG Ji
    2022, 19(10): 2791-2805.
    Phytogenic mounds(nebkhas) formed by shrubs are a common phenomenon in arid and semiarid areas. The formation of nebkhas is accompanied by the appearance of the fertile island effect. Quantitative evaluation of the shrub sand compost island effect is a key link in preventing soil erosion and nutrient loss. This study took the typical shrub Tetraena mongolica in desert areas as the research object and quantified the sand-trapping capacity of the shrub. We revealed the influence of sediment texture and volumetric soil water content on fertile islands during the development of T. mongolica nebkhas. The results showed that(1) the single shrub intercepted large amounts of sediments due to the high density of branches of T. mongolica, forming nebkhas that were positively correlated with the shrub size.(2) The overall soil nutrient content below the shrub was greater than the soil nutrient content outside the shrub, forming a typical fertile island effect. The soil organic carbon(SOC), alkaline hydrolytic nitrogen(AHN), available phosphorus(AP), and available K(AK) content all increased gradually with increasing nebkha volume. Compared with the deep soil of nebkhas, the nutrient content of the surface soil was generally higher.(3) There was a positive correlation between the volumetric water content and nutrient content in nebkhas.(4) The semi-ellipsoid shape of T. mongolica enabled it to intercept large amounts of coarse-grained material. Fine sand(100–250 μm) was the main particle size in the sediment aggregates inside the nebkhas. The fine sand content generally increased with increasing shrub size. Redundancy analysis(RDA) revealed that the fine sand content of the nebkha sediments had a strong positive correlation with the soil nutrient content. This paper provides an example for evaluating the fertile island effect during the deposition process of nebkhas in the desert transition zone.
  • Mohamed A.FADL, Hatim M.AL-YASI, Emad A.ALSHERIF
    2022, 19(10): 2806-2822.
    Mountains are biodiversity hotspots, and due to their unique microclimatic circumstances, they host a vast range of endemic species. There are two main hypotheses, the Rapoport and the mid-domain effect hypotheses, which explain how elevation and species richness are linked. The current study was conducted in the Al-Hada escarpment, which is a unique area in the world. It is located on the border of Eurasia and Africa, where there are a lot of plant species from both places. The study aimed to detect the effect of elevation on the floristic composition of the study area. The obtained results showed that the Al-Hada escarpment flora consists of 297 species belonging to 194 genera and fifty-seven distinct families. Only two families, Poaceae and Asteracae, had 22% of the whole recorded species. The obtained results showed that with increasing elevation, the numbers of species, genera, and families increased, in accordance with the Rapoport hypothesis. The numbers of families increased by 62% from the lowest elevation to the highest one, while the numbers of both species and genera increased by more than twofolds. Therophytes exhibited the maximum number, which was 44%, and Chamaephytes came in second with 25%. Phanerophytes and hemicryptophytes made up 13% and 11% of all life forms, respectively, while geophytes made up just 7%. Monoregional elements represented 33.2% of the total recorded species, where Saharo-Sindian species had the most monoregional species, accounting for around 13% of the total species. At the highest elevation, succulents accounted for 7.6% of the research area, whereas Nfixing plants accounted for 6.2%. At the highest elevation, they had the lowest value, and at the middle elevation, they had the highest value. With the rise in elevation, the neotropical, endemic, and Mediterranean elements rose. Succulents and Nfixing species did not show a clear relationship with the elevation but exhibited the lowest value at the highest elevation, and vice versa. Therophytes and geophytes increased while the number of hemicryptophytes decreased with elevation. Surprisingly, phanerophytes did not show any relationship with elevation, while, with the rise in elevation, the pan-tropical, endemic, and Mediterranean elements rose. Neotropical and Saharo-Sindian elements decreased with the rise in elevation. Considering our results, we can conclude that the relationship of taxa diversity with the different altitude of the arid subtropical regions' mountains, whose elevation does not exceed 2000 m (without human disturbance), confirms the Rapoport hypothesis.
  • LIU Zheng, SHENG Fei, LIU Shi-yu, WANG Yan-yan, ZHOU Chang-ming, GU Chao-jun
    2022, 19(10): 2817-2829.
    Baseflow is an essential component of streamflow and plays a crucial role in maintaining the stability of streamflow. However, few quantitative studies have identified the effects of leading factors on baseflow variation at the small watershed scale, especially in subtropical China. In this study, the small watershed(Pengchongjian watershed, 2.90 km2), located in Southern China, was considered to explore the quantitative impact of precipitation, evapotranspiration, temperature, and vegetation restoration on baseflow. The digital filter method was used to separate baseflow by daily streamflow records from 1983 to 2014. The stepwise regression models were developed for selecting significant influencing factors of baseflow at seasonal and annual scales. The direct and indirect effects, as well as their quantitative relationships between baseflow and multiple factors, were clarified by the path analysis. The results showed that filtered average annual baseflow significantly decreased(p < 0.05), ranging from 72.82 to 305.85 mm, and the average yearly baseflow index was 0.22. In addition, various significant influencing factors of baseflow had different direct and indirect effects on baseflow at seasonal and annual scales. The precipitation was the dominant factor with respect to the direct impact, which directs path coefficient was 0.891 in spring, 0.823 in summer, 1.599 in autumn, 1.332 in winter, and 0.917 in an annual scale, respectively. In terms of the indirect effects, evapotranspiration played a leading role during the spring, autumn, winter, and annual scale, whereas the average temperature was the dominant factor during the summer. Overall, results demonstrated that the baseflow variation was mainly attributed to climate change. The present works are beneficial for revealing the internal mechanism of the baseflow variations in the study area, and it can provide a scientific basis for managing water resources in the watershed.
  • ZHANG Bao-jun, XIONG Dong-hong, LIU Lin, TANG Yong-fa
    2022, 19(10): 2830-2845.
    Controlling aeolian desertification is a key ecological target on the Tibetan Plateau, especially within the widespread river valleys. Vegetation recovery can change the near-soil surface characteristics, which thus may influence wind erodibility of soils. However, these potential effects are not sufficiently evaluated for aeolian sandy soils. This study selected the Shannan valley of the Yarlung Zangbo River on the southern Tibetan Plateau as a case to investigate the variations in wind erodibility of aeolian sandy soils impacted by different vegetation restoration, since many ecological measures have been implemented in recent decades in the river valley. Eight vegetated sandy lands with different restoration types and ages and two bare sandy lands(as controls) were chosen as test sites. Four vegetated sandy lands were covered by Artemisia wellbyi, Hedysarum scoparium, Sophora moorcroftiana, and Populus L. with the similar restoration age of 10 years. For Sophora moorcroftiana and Populus L. communities, two restoration ages of 6 and over 30 years were also selected respectively. Wind erodibility was reflected by wind erodible fraction(EF), mean weight diameter of dry aggregates(MWD), capillary water capacity(CWC), soil cohesion(CS), and soil penetration resistance(PR) from different aspects. A comprehensive wind erodibility index(CWEI) was further produced by a weighted summation method to combine those five indices together and comprehensively quantify the effects of vegetation restoration on wind erodibility of aeolian sandy soils. The results showed that revegetation was efficient to reduce wind erodibility of aeolian sandy soils. EF generally decreased, while MWD, CWC, CS, and PR increased after vegetation restoration on the aeolian sandy lands. The CWEI of vegetated sandy lands varied greatly from 0.850 to 0 under different restoration types and ages and decreased by 14.4% to 100% compared to the control. Under the four different restoration types, Populus L. had the relatively minimum CWEI, followed by Artemisia wellbyi, Sophora moorcroftiana and Hedysarum scoparium. With succession from 6 to over 30 years, CWEI gradually declined for both the Populus L. and Sophora moorcroftiana restored sandy lands. The decreases in wind erodibility(reflected by CWEI) on vegetated sandy lands were dominantly controlled by the improvement of soil texture and the increases of organic matter and calcium carbonate contents with vegetation restoration. The combined vegetation measure of Populus L. mixed with shrubs and grasses was suggested as the optimal restoration type for mitigating wind erodibility of aeolian sandy soils in the Shannan valley of the Yarlung Zangbo River.
  • MU Hao-xiang, HAN Fang, ZHANG Bai-ping, LIANG Tian, WANG Zhi-yong, WANG Zhe
    2022, 19(10): 2846-2860.
    Different types of vegetation patches are alternately and randomly distributed in a timberline ecotone where the upper limit is the treeline and the lower limit is the timberline. However, most studies on timberline/treeline altitudinal distributions have simplified timberline or treeline as continuous curves and disregarded the fuzziness of timberline/treeline and the randomness of different vegetation patch distributions in a timberline ecotone. To study the altitudinal distribution characteristics of timberline and treeline from the perspective of uncertainty theory, we constructed the timberline and treeline elevation cloud models in Mt. Namjagbarwa in east Himalayas. Subsequently, we established multiple linear regression models by using nine influencing factors, namely, aspect, slope, topographic relief, dryness index, average temperature in January and July, latitude, summit syndrome(represented by the vertical distance from the peak), and snow effect(represented by the nearest distance from the snow) as independent variables, and the elevations of timberline/treeline as dependent variables. Then we compared the contributions of the nine factors in timberline, treeline, and the core and peripheral areas of timberline and treeline. The results show that 1) the timberline/treeline elevation cloud model can represent the overall characteristics(especially the uncertainty) of the altitudinal distributions of the timberline/treeline well. The uncertainty of treeline's altitudinal distribution is higher than that of timberline(entropy and hyper entropy: 207.59 m and 70.36 m for treeline elevation cloud; entropy and hyper entropy: 191.17 m and 50.13 m for timberline elevation cloud). 2) The influence of climate and topography on timberline and treeline are similar. The average temperature in July has a significant negative correlation with the timberline/treeline elevation in Mt. Namjagbarwa, which is the most critical factor that affects timberline and treeline elevation, explaining the altitudinal distribution of 44.01% timberline and 46.74% treeline. However, the contributions of the nine factors in core and peripheral areas of timberline and treeline area are evidently different.
  • ZHOU Jian, YANG Fei-ling, ZHONG Zi-jie, ZHANG Ji, LENG Xian, YE Jin, WU Rui-dong
    2022, 19(10): 2861-2875.
    Bird diversity is often used as surrogates for other species diversity, but there is a limited understanding of the extent of this surrogate in identifying representative priority conservation areas(PCAs). We used Yunnan Province in China as a case to measure the surrogacy of birds in systematic conservation planning. Here, we collected distribution records of mammals, amphibians, reptiles, and birds from public databases and literature, and applied systematic conservation planning methods to identify PCAs. We targeted four taxonomic groups at conservation targets of 17%, 31%, and 50% of the total study area, and used the Jaccard similarity index to evaluate the surrogate extent of bird PCAs for the other three groups. Then, we overlapped different portfolios of PCAs with six categories of protected areas(PAs) in Yunnan, calculated the protection rates,and evaluated the effect of sustainable-use PAs on improving the protection rate of strict Nature Reserves. The results showed that bird PCAs generally had the highest surrogacy for representing PCAs of the other three taxa. At the 50% conservation target, the Jaccard indices between birds and the other taxa reached about 0.50. Moreover, amphibian PCAs had a good surrogacy for conserving reptiles, with a Jaccard index of 0.30, 0.44 and 0.51 at the 17%, 31% and 50% conservation targets, respectively. The existing PA system had quite low coverages for PCAs of these four taxa, and the average protection rates were 22.97%, 19.78% and 16.52% at the three levels of conservation targets, respectively. The sustainable-use PAs can greatly complement the strict Nature Reserves by achieving average increased PA coverages of 10.00%, 9.20% and 7.90% at the three conservation targets. Our findings provide a basis for surrogate-based conservation planning for areas with insufficient biodiversity information.
  • ZHOU Yang, YI Yu-jun, LIU Hong-xi, TANG Cai-hong, ZHU Yu-long, ZHANG Shang-hong
    2022, 19(10): 2874-2891.
    Rapid change of climate in vertical and considerable geomorphologic features form a typical diversity and distribution of biota in mountain ecosystems, i.e., the subalpine forest zone(SFZ), the valley savanna zone(VSZ), and the transition zone between them. The arid hot valley in the middle and lower reaches of Jinsha River, China represents a well target area to study distribution and the driving factors in these typical mountain ecosystems. Therefore, this study selects four sub-sample areas in the arid-hot valley to explore the distinctive changes of vegetation during 1990 to 2020, and their driving factors in the three different vegetation zones on spatiotemporal scales. On the spatial scale, the Moran's index was applied to identify the transition zone between the SFZ and the VSZ. Results show that the VSZ at low altitudes(less than 600-1000 m from the valley bottom) is mainly affected by geomorphologic features, especially the slope aspect. With increase in altitude, the climate factors(e.g., humidity, temperature, etc.) play a more significant role in the development of the SFZ, while the effect of geomorphologic features gradually weakens. On the time scale, The SFZ at higher altitudes experienced more rapid changes in temperature(temperature increase of 1.41°C over the last 60 years) than the VSZ at lower altitudes(temperature increase of 0.172°C over the past 60 years). It caused the forest cover increase faster than that of savanna grassland. Humidity and heat conditions are altered by topography and climate conditions, which shapes the development and physiology of plants as they adapt to the different climatic zones. Furthermore, according to the driving factors(geomorphologic and climate factors) of vegetation distribution found in this study, it suggests that suitable tree species should be planted in the transition zone to evolve into the forest zone and making the forest zone to recover from high to low altitudes gradually.
  • JIAN Sheng-qi, ZHU Tian-sheng, HU Cai-hong
    2022, 19(10): 2886-2904.
    Due to the influence of human activities such as cultivation and urban construction, the ecosystem of the Yellow River Basin(YRB) is subjected to increased vulnerability and even potential risk of destruction. Ecological restoration has led to an increase in vegetation, but excessive afforestation conversely results in low survival rate of trees, water shortages, and biodiversity loss. It is of great significance for achieving sustainable development of forests to reasonable revegetation in the region. At present, the potential distribution pattern of dominant species and their mixed forms in the basin has not been effectively studied. This study simulated the potential distribution of dominant vegetation in the YRB based on Maximum Entropy(Max Ent) and Genetic Algorithm for Rule-Set Prediction(GARP) and explored the impact of human interference on it by employing land use as the environmental filter to distinguish the regions of human activities. We further predicted the potential distribution of typically mixed forests and discussed their human interference. The main results are as follows:(1) Except for Caragana korshinskii, all models had good above performance(0.7 < the mean AUC < 1). Except for Caragana korshinskii, the area under the curve(AUC) for 90% of the models indicated that Max Ent performed better than GARP, and Max Ent easily lead to over-fitting while GARP predicted a wider range.(2) Except for Nitraria tangutorum, the dominant types of vegetation such as Pinus tabulaeformis, Platycladus orientalis, and Hippophae rhamnoides mainly distributed in southern Gansu, Shaanxi, and south-central Shanxi. Among them, the largest suitable area of Artemisia gmelinii and Stipa bungeana(High suitable area) were approximately 56.7×104 km2(38.8%) and 54.7×104 km2(28.5%) with the area occupied by large-scale cultivation being 17.5×104 km2(39.4%) and 18.9×104 km2(48%), respectively, which indicated human activities caused great damage to the core growth regions of these vegetation.(3) Mean temperature of coldest quarter or month mainly constrained the growth of most vegetation in the YRB in terms of temperature, while precipitation of wettest/driest month is one of the dominant factors. However, some vegetation responded differently to other meteorological factors due to niche differences.(4) Most of the mixed forests were distributed in southern Gansu, Shaanxi, and Shanxi provinces; its middle and high suitable areas were mainly concentrated in Shaanxi and southern and central Shanxi, where the cultivated land had occupied most of them. Therefore, the results showed that the restoration of herbaceous vegetation such as Artemisia gmelinii and Stipa bungeana has a high potential and it is appropriate that the measures for afforestation should be concentrated in the areas like the lower reaches of the Weihe, Jinghe, and Beiluo rivers and Luliang Mountain, where the cultivated land overlaps with the high suitable areas of the corresponding vegetation and the mixed forests with less water consumption and wide distribution, such as Caragana korshinskii-Hippophae rhamnoides, Pinus tabulaeformis-Quercus liaotungensis, and Ostryopsis davidiana-Stipa bungeana-Hippophae rhamnoides. The results of this study can provide effective guidance for mixed forest plantations and vegetation conservation in the YRB.
  • SHI Peng, QIN Yan-li, LI Peng, LI Zhan-bin, CUI Ling-zhou
    2022, 19(10): 2905-2919.
    Linking landscape indexes to ecological processes is the key topic of landscape ecology. However, traditional landscape metrics based on the Patch-Mosaic Model have no ecological significance. In this study, the runoff-sediment landscape index coupling land use, topography, soil, and vegetation factors was constructed to link landscape patterns to runoff and sediment. In the study area, the runoffsediment landscape index at the class scale showed an increasing trend from 0.10 in 1995 to 0.26 in 2015. Cropland had a higher runoff-sediment landscape index compared to grassland or forestland. At the landscape scale, the runoff-sediment landscape index showed a decreasing trend since 1995; furthermore, it decreased by 36.24% in 2015 compared with the index in 1990. The runoff-sediment landscape index had higher correlations with runoff and sediment compared with traditional landscape metrics. Redundancy analysis showed that the runoffsediment landscape index had a higher contribution to runoff and sediment compared to traditional landscape metrics, explaining 90.1% of the variability. The soil erosion risk assessed by the runoff-sediment landscape index showed an increasing trend upstream of the Dali River watershed. More attention should be paid to this area in future vegetation restoration attempts, as exploring the impact of landscape pattern changes on ecological processes, especially hydrological processes, plays an important role in comprehensive watershed management.
  • FENG Zhu-jun, WANG Xiu-li, RAN Yong-hong
    2022, 19(10): 2920-2934.
    Concrete dams are reliable when subjected to static loads such as earth pressure and water pressure. However, the dam failure would be abrupt and catastrophic if it is impacted by boulders. This study simulated the dynamic response of flat dam, concave dam, and convex dam under the impact of boulders by using ANSYS/LS-DYNA finite element software. In the numerical simulation, the strain rate effect under the impact load is considered, and Holmquist-Johnson-Cook(HJC) model-a dynamic damage constitutive model is applied to concrete materials. Results show that the peak impact force of concave dam is minimum. Meanwhile, for different dam types(flat dam, concave dam, and convex dam) and impactor velocities(5, 10, and 15 m/s), the impact force fluctuates with the height of the impact point and it reaches the maximum value when the height of the impact point is 2/3 of the dam height. Numerical simulation mainly considers different masses and velocities and obtains empirical formulae of impact force for three dam types. The established empirical formula for the flat dam is compared with the existing classical formula and several similar experimental tests. It was found that the newly empirical formulae are reasonable and effective, and it provides design suggestions for similar concrete dams.
  • JIAN Tao, KONG Ling-wei, BAI Wei, LIU Bing-heng, SUN Zhi-liang
    2022, 19(10): 2935-2951.
    The loess tableland provides an excellent site for people to live and cultivate. However, flowslides occur frequently on the slope of loess tablelands due to agriculture irrigation, resulting in serious economic losses and casualties. The structure degradation effect of irrigation water seepage on intact loess leads to a weakening of its mechanical properties, which may be responsible for the recurrent occurrence of flowslides in irrigated loess tablelands. In this paper, seepage tests and triaxial tests were carried out to investigate the evolution of the microstructure and undrained shear properties of intact loess during seepage. The results show that water seepage leads to a significant decrease in pore water ion concentration and migration of fine particles with water flow, but no noticeably change in mineral composition. During seepage, the metastable structure of intact loess collapses, the fine particles disperse around the skeleton particle to fill the pores, and the total porosity decreases. The permeability coefficient gradually decreases with seepage time and then tends to a constant. The saturated intact loess shows strongly contractive behavior during undrained shear and has considerable liquefaction potential. After seepage, the intact loess is characterized by more rapid build-up of pore water pressure and more intense strain-softening during shearing and has lower shear strength(including peak strength and steady-state strength). In irrigated loess tablelands, long-term seepage could weaken the shear strength of intact loess and increases its liquefaction potential, which contributes to the initiation of loess flowslide failure and the movement with high-speeds and long run-outs.
  • ZHANG Hao-nan, JIA Cang-qin, WANG Gui-he, SU Fei, SUN Yong-shuai, FAN Chang-yi
    2022, 19(10): 2952-2967.
    Loess disintegration can lead to geotechnical engineering problems, e.g., slope erosion, wetting-induced landslide, and hydroconsolidation. Microbially induced calcite precipitation(MICP) technique is a potential loess reinforcing method. This study investigated the physical-mechanical properties of MICP-treated loess and then explored the mechanism of loess modification by MICP. Here, loess first underwent MICP treatment, i.e., mixing loess with Sporosarcina pasteurii and cementation solution(CS). Then, the effects of the CS concentration(0.2, 0.6, 0.8, and 1 M) on the physical and mechanical properties of the MICP-treated loess were tested. Finally, the static contact angle test, scanning electron microscopy(SEM), and X-ray diffractometry(XRD) were conducted to study the mechanism of MICP treatment on loess. Results showed the following property changes of loess after MICP treatment: the liquid limit decreased by 1.7%, the average particle size increased from 6 to 47 μm, the specific gravity decreased from 2.65 to 2.43, the unconfined compressive strength increased from 37 to 71 k Pa, and the disintegration time increased from 10 to 25 min. Besides, the shear strength also increased, and the shear strength parameters(cohesion c and internal friction angle ?) varied with the CS concentration. The static contact angle tests indicated that the water absorption ability of loess was reduced after MICP treatment. SEM and XRD results verified that the CaCO_3 from MICP was attributed to the above results. The above findings explained the mechanism of MICP treatment of loess: the CaCO_3 coats and cements the particles, and fills the pores of loess, improving the strength and water stability of loess.
  • ZHANG Kai, ZHAO Li-ming, ZHANG Hai-long, GUO Ao-jun, YANG Bo, LI Sheng
    2022, 19(10): 2968-2986.
    The railway subgrades in the sandy areas act as an obstacle interfering wind-blown sand, causing sand erosion and sedimentation, which can disrupt the safe and stable operation of the railway system. Most previous studies mainly focus on the flow field around railway subgrades, however, the real erosion and sedimentation patterns are rarely studied. This study aims to analyze the erosion and sand sedimentation patterns of wind-blown sand over the subgrades with different heights and steel rails using the ratio of the wall shear stress to the critical value of erosion shear stress. Results show that wind erosion near the top of the upwind slope of the embankment and the shoulder on the upwind side are more severe, and the severity increases with an increase in the height of the embankment. With the increase of wind velocity, sand sedimentation both on the windward and leeside of the subgrade decreases and wind erosion by reverse flow occur. This study indicates that railways in sandy areas should be constructed with a moderate subgrade height(4 m).
  • YAN Qi-xiang, ZHANG Tian, ZHANG Chuan, GUO De-ping, QING Song-yong
    2022, 19(10): 2987-2998.
    Due to the existence of a large number of discontinuous fractures and interfaces in tunnel surrounding rocks, the groundwater inflow into tunnel generally presents significant anisotropy. Therefore, it is of great significance to consider the anisotropic permeability when dealing with water gushing-induced engineering accidents in water-rich mountain tunnels with large burial depth. In this study, based on the complex variable method and the seepage flow theory, a theoretical model of water inflow into a deep-buried circular tunnel in a fully saturated, anisotropic and semi-infinite aquifer is developed. The influence of grouted zone, initial support and secondary lining is fully considered. By comparison to the existing analytical methods and numerical results, the reliability of this proposed analytical solution is well validated. It is indicated from the parametric study that the groundwater inflow into tunnel presents an upward trend with an increasing value of the strata permeability in the vertical direction. Moreover, the water inflow rate and the total water head decrease with the growth of the thickness of grouting circle. It is suggested that reasonable grouting thickness and permeability should be controlled to enhance the grouting effect. This study provides a practical method for estimating the water inflow into a deep-buried, grouted and lined mountain tunnel considering the anisotropic strata permeability.
  • LI Cong, ZHANG Rong-tang, ZHU Jie-bing, LU Bo, SHEN Xiao-ke, WANG Xiao-wei, LIU Jie-sheng, WU Liang-liang, ZHANG Xin-zhou
    2022, 19(10): 2999-3012.
    The stability of slope rock masses is influenced by freeze-thaw cycles in cold region, and the mechanism of stability deterioration is not clear. In order to understand the damage and progressive failure characteristics of rock masses under the action of freezing and thawing, a model test was conducted on slope with steep joint in this study. The temperature, frost heaving pressure and deformation of slope rock mass were monitored in real-time during the test and the progressive failure mode was studied. The experimental results show that the temperature variations of cracking and the rock mass of a slope are different. There are obvious latent heat stages in the temperature-change plot in the crack, but not in the slope rock masses. The frost heaving effect in the fracture is closely related to the constraint conditions, which change with the deformation of the fracture. The frost heaving pressure fluctuates periodically during freezing and continues to decrease during thawing. The surface deformation of the rock mass increases during freezing, and the deformation is restored when it thaws. Freeze-thaw cycling results in residual deformation of the rock mass which cannot be fully restored. Analysis shows that the rock mass at the free side of the steep-dip joint rotates slightly under the frost heaving effect, causing fracture propagation. The fracture propagation pattern is a circular arc at the beginning, then extends to the possible sliding direction of the rock mass. Frost heaving force and fracture water pressure are the key factors for the failure of the slope, which can cause the crack to penetrate the rock mass, and a landslide ensues when the overall anti-sliding resistance of the rock mass is overcome.
  • Graham MCDOWELL, Katherine HANLY
    2022, 19(10): 3013-3025.
    Nearly a quarter of Canada's landmass is covered by mountainous terrain, making mountains an important aspect of the physical and human geography of the country. Mountain areas in Canada have motivated a great deal of research activity, yet the state of mountain research in the country has never been systematically characterized, precluding a detailed understanding of what is being studied, when, where, how, and by whom. In response, we conducted a systematic scoping review to rigorously identify, collate, and critically examine existing peer-reviewed articles related to mountains in Canada. 2,888 articles were included in our review, which reveals strong biases towards work in the natural sciences and in the mountain west, with little work to date in the social and health sciences or in other mountainous regions of the country. Our results demonstrate that Canada is among the most productive contributors to mountain research globally, but that topical and geographical biases in existing research effort leave important gaps that must be addressed to successfully navigate challenges and opportunities facing mountain areas in Canada. We provide a roadmap to guide future mountain-focused research activities in the country.
  • LI Ya-juan, OUYANG Chen-xing, ZHOU Sheng-yu, YU Hu, KNIGHT W David
    2022, 19(10): 3026-3037.
    Questions persist on the relationship between tourism dependence and economic growth in ethnic tourism areas. This study addresses such gaps by constructing a threshold regression model based on socio-economic data from 2006 to 2019 for nine sites in Enshi Prefecture of central China. Arc GIS and other open-source data were also used to visualize changing tourism resources in the region. Findings suggest that tourism dependence(the ratio of tourism-based GDP to overall GDP) significantly promotes economic growth in ethnic minority areas. However, the positive influence of tourism dependence on economic growth appears dynamic and non-linear – rising at first before falling when tourism dependence exceeded a threshold of 34%, with effects varying by site and year. Methods and findings make crucial theoretical contributions to understanding tourism dependence and poverty alleviation linkages. This paper also highlights the importance of political support and balanced investment in diverse industries to minimize decreasing returns beyond tourism dependence thresholds in destinations worldwide.