North China Before the Ming dynasty, dense forests still existed in the
Great Wall region. By the Ming, forests on the
Loess Plateau were heavily damaged. In the early Ming, forests in Luya Mountain and Yunzhong Mountain in northwestern
Shanxi, and Heng Mountain in northern Shaanxi, remained intact. Some damaged forest areas in the Guanzhong
Qinling and
Xiao Mountains also partially recovered. After
Yongle established the capital in
Beijing, the
Taihang Mountains became a major source of timber for the city, greatly accelerating deforestation. As the imperial palace and urban development required wood, the government conducted large-scale logging and charcoal production. After prolonged uncontrolled official and private exploitation, the forests in the Great Wall region suffered devastating destruction. After the mid-Ming, large areas of forest disappeared. By around the 17th century, fuel and construction timber were generally in short supply. Rapid population growth led to continuous reclamation of new farmland and increased demand for daily timber, causing a sudden change. Forest areas shrank quickly. Forests in the Heng Mountains and
Lüliang Mountains were successively exhausted. At this point, the massive building materials needed for the capital could no longer be obtained from the middle reaches of the Yellow River and had to be sourced from
Sichuan and the Two Lakes region. Due to thorough destruction, the forests' self-renewal capacity was almost lost. The middle reaches of the Yellow River presented a continuous sight of bare mountains. Although the Ming had policies prohibiting logging, their main purpose was to protect the
feng shui of imperial tombs or to meet military and political needs. The scope was very limited and showed no genuine ecological awareness. In North China, the opening of the Grand Canal slowed the discharge of all rivers, large and small. Sediment continued to accumulate, causing periodic flooding and waterlogging. Because the river water contained salt, waterlogged land easily underwent
soil salinization, becoming uncultivable. The worst areas turned into swamps, which then bred
locusts. The Beijing-Hangzhou Grand Canal further impeded the already slow-flowing Yellow River and forced the
Huai River to backflow into its upper reaches. Sediment from the Grand Canal and Yellow River frequently blocked the mouth of the Huai River, causing floods to spread into the plain. Frequent flooding covered farmland with sand and gravel, sometimes up to 7–8 meters thick. Some formerly prosperous counties with fragrant rice and abundant fish saw large areas of land salinized, turning into barren red earth where even weeds would not grow. Weeds that grew after floods became breeding grounds for locusts. Due to insufficient irrigation, agriculture was limited to drought-resistant crops such as winter wheat, sorghum, and soybeans.. In 1578–1579, Ming official
Pan Jixun managed the lower Yellow River by building earthen and stone dikes, dredging the riverbed, and unifying the Yellow River's course. He proposed the method of "constricting the water to attack the sand," using higher and narrower dikes to accelerate flow. Water was constricted within "lǚ dī" near the banks. His river management increased sediment at the sea mouth, lowered the downstream gradient, and diverted clear water into the Yellow River to scour silt from the riverbed. In 1579, Pan Jixun built the across the Huai River, storing clear water from the Huai and two other rivers in
Hongze Lake. Continuously raising the Gaojia Weir on the eastern shore of Hongze Lake ensured the lake's water level remained higher than the Yellow River, allowing grain-transport boats to pass.
Southwest Urban residents' demand for timber prompted mountain residents to specialize in logging and timber transport. The Yunnan-Guizhou region, previously economically undeveloped with sparse settled agricultural population and inhabited mainly by non-Han indigenous peoples, developed under Ming rule into a region increasingly dominated by Han migrants and commercialized. The southwest had rich and diverse ecosystems. In southernmost
Yunnan's
Xishuangbanna, rolling mountains and dense rivers existed. The
Khmu people lived deep in jungles and bamboo forests, practicing
slash-and-burn agriculture (continuing into the 20th century) and domesticating elephants. The southwest originally had a healthy ecosystem with tigers and elephants frequently appearing and vast forests.
Thai-speaking peoples cleared some river valleys into farmland, while other ethnic groups practiced slash-and-burn. Due to high mountains and deep valleys that were difficult for humans to access, human impact was minimal. From around 1400, large numbers of Han people arrived in Yunnan and Guizhou. The Ming-established
weisuo and military farms spread across the southwest, with 250,000 Han soldiers beginning to farm in river valleys. Indigenous groups' wooden tools could only reclaim lighter alluvial soils in valleys and were unsuitable for the heavy soils of forested areas; they also lacked oxen for plowing. The Ming equipped Han migrants with iron
plows and tens of thousands of oxen, enabling them to reclaim forest soils. In the 15th and 16th centuries, millions of *mu* of farmland were opened in Yunnan and Guizhou. During court wars against indigenous peoples, Han armies set fire to mountains, destroying animal habitats. The ultimate solution to rebellions was to transform different ecological environments into farmland. In
Guizhou, some local
tusi also led people to shift from slash-and-burn to plow-based production..
Northwest The
Ordos Desert in the
Yellow River Hetao region had varied ecosystems—some purely desert, others grasslands suitable for nomadic life. Here, water from the
Yellow River could be diverted for irrigation, allowing Han people to settle and farm. In the late Ming, a total of of canals had been dug in the Hetao region, irrigating thousands of *mu* of land. The Ming built the
Great Wall in the Ordos to separate the grassland from agrarian society. It ordered stationed troops to burn 50–100 *li*-wide strips of wasteland north of the Great Wall (at least in strategic locations) each year, depriving
Mongol cavalry horses of fodder, destroying pastures so Mongol herders could not enter, but sowing the seeds of
desertification. Converting forest and grass vegetation to farmland also tended toward desertification as soil organic matter decreased.
Jiangnan and Central China During the Wanli era (1573–1620), several reclamation fields of over one thousand hectares each had been opened along the
Yangtze and its tributaries in
Anhui. In central China,
Hongwu Emperor established military farm
weisuo in
Hubei, repaired old
dikes, and built new water conservancy facilities, recruiting migrants to reclaim land. These policies continued into the 16th century. People built dikes on the southern bank of the
Han River, preventing water from overflowing. The riverbed rose higher and the current became faster, greatly increasing flood risk downstream. As a result, downstream residents began building dikes to protect their homes and then reclaimed more swamps and lakes. By the late Ming, the hydrological conditions of the entire Han River basin had been thoroughly transformed by humans. In the 15th and 16th centuries, large numbers of people migrated to
Hunan, introducing advanced rice cultivation techniques from the lower Yangtze. They built dikes around swamps and tidal flats to form
polders for flood control and irrigation, transforming the area into rice fields. Some early polders were very large, reaching thousands or tens of thousands of *mu*.
Xu Guangqi already recognized human causes of flooding. He criticized powerful local families for encroaching on swamps, lakes, and riverbank
alluvial plains, filling water bodies to create fields, which increased flood risk and harmed entire settlements.
Southern mountainous areas Before the Ming, there were only a few settlements in hilly and mountainous areas. Most
terraced fields followed riverbanks near cities. In most regions, reclamation of hills and mountains began in the late Ming. After mountain forests were privatized, some private forests in the south survived. After timber was cut and sold, mountain owners would replant to regenerate them. During the Ming and Qing, private forestry was common, especially in southern
Anhui and
Fujian. Mountain tribes south of the
Yangtze specialized in cultivating
Chinese fir and producing timber. At this time, public forest resources were becoming exhausted, while private plantations grew trees for sale, yielding good profits. Mountain owners did not necessarily manage the forests themselves but could lease them to others. In general, private plantations were well protected with high survival rates for replanting, in stark contrast to the destruction of public forests.. After the mid-16th century, planting Chinese fir became prevalent in southeastern mountainous areas.
Broadleaf forests turned into
coniferous forests such as fir. Small animal populations in the mountain forests decreased, tigers faced food shortages and increasingly attacked livestock in the plains, while
Asian black bears and
wolves that once lived in broadleaf forests gradually became extinct.. On the other hand, the Ming issued orders to protect monastery forests to maintain the natural environment around temples. from the
Americas In the
Yangtze basin and
Lingnan, lowland farmland became increasingly insufficient. New migrants, seeking arable land, had to penetrate deep into the mountains and learn various skills from locals. In the first half of the 16th century, New World crops from the Americas—maize, potato, sweet potato, peanut, and tobacco—spread to China, exerting a huge ecological impact. Han people migrating into the mountainous border regions of
Jiangxi,
Fujian, and
Guangdong formed the origin of the
Hakka people. The Hakkas merged and assimilated with the local indigenous
She people. Around 1500, the mountainous border of the three provinces became Hakka territory. Their dialects and customs differed markedly from those of lowland Han. The Hakkas cleared mountain forests and widely planted maize and sweet potatoes, selling mountain products outward. Hemp,
ramie, indigo, tea, sugarcane, and tobacco were the most common cash crops planted by Hakkas. From the mid-16th century onward, Hakkas began migrating to mountainous areas across southern and southeastern China, selling products to riverside towns. They also rented large mountainous lands from Han landlords and recruited poor She people to clear forests using
slash-and-burn methods. In the 16th and 17th centuries, large numbers of Hakka and
She men migrated northward into the mountains of
Jiangxi, Anhui, and Zhejiang, becoming mobile populations known to the government as "shed people" (*pengmin, 棚民). They built temporary sheds, developed mountain land, and moved on after exhausting the soil. In the mountainous areas of the
Gan River basin in Jiangxi, most land had previously been densely forested and untouched by Han logging until the arrival of the shed people. Many shed people in Jiangxi mountains were miners, loggers, and papermakers. Their food mainly came from slash-and-burn on forest edges, gradually damaging the Jiangxi mountain environment.
Hainan Island Hainan Island had numerous
coral reefs and
oyster breeding areas in the north. The island was covered with various
tropical forests containing over 3,500 plant species. Indigenous
Li people practiced
slash-and-burn to grow mountain yams and upland rice, supplemented by forest
hunting and gathering. Due to their small population, their impact on the ecosystem was limited. During the Ming, the amount of cultivated land on Hainan doubled, from about 2 million *mu* around 1400 to 3.8 million *mu* in 1615, most of it farmed by Han people. Hainan had been transformed to become suitable for Han habitation. The government encouraged Han people to burn forests in river valleys and mountains. Continuous burning created opportunities for tropical
cogongrass to grow. ==Qing dynasty==